Utah State Engineer Technical Publication No. 15

WATER FROM BEDROCK IN THE COLORADO PLATEAU OF UTAH

by R. D. Feltis Geologist

U. S. Geological Survey

Prepared by the U. S. Geological Survey in cooperation with THE UTAH OIL AND GAS CONSERVATION COMMISS10N

1966

CONTENTS - (Continued) Page Water from bedrock in the Canyon Lands section-Continued Entrada Sandstone _. . .. _. . .. _._ .._ _.. .. '2:7 Bluff Sandstone .. __ ._ __.. __ ._ .. __ . .. _._ _ _ _.... '2:7 Morrison Formation .... ._ .. _. __ ._.. __ __ .. _. .__ ..__.._.._..... '2:7 Dakota Sandstone .. ______.. __ _ _..... 28 Burro Canyon Formation __ __ .. . _ _.._ __ _ _.. _..... 28 Mancos Shale .__ _._.______._ _ __ _..... 28 Ferron Sandstone Member of Mancos Shale _ _. __ .._ _.. __ .__ __ _ 29 Tununk Shale Member of Mancos Shale _._ _ _ _..... 29 Water from bedrock in the High Plateaus section _ _ __ _ 29 Limestones of Paleozoic age ._ _ __.._.._ _.._ _ .._ _... 31 Rocks of NIississippian age .__ .. __ .. __ ._ _ _ _ _... 31 Rocks of Mississippian age and Molas Formation __ _ _...... 31 Toroweap Formation .. __ .__ .. _._ __ ._._._ __..______. __ _._ _... 31 Cedar Mesa Sandstone Member of Cutler Formation .._ _...... 31 Coconino Sandstone _. __ ._. ._ _ _..______._._. 31 Kaibab Limestone _ _ _ _ _...... 31 Shinarump Member of Chinle FOrrIlation _ _ _...... 31 Moenkopi Formation ______.._.__ 32 Wingate Sandstone ______.... 32 Wingate Sandstone and Kayenta Formation _.._ _._ __._ _...... 32 Navajo Sandstone ._ __ __._ _._..__ __.._. 32 Carmel Formation _ _._._._ _ _ _.._ _..__.._.._ __ _ _..... 32 Morrison and Cedar Mountain Formations _ _...... 32 Winsor Formation and Dakota Sandstone _..__._.._ _ _ _._ _ _.._.. _. 32 Dakota Sandstone .._ _.. _ _ _. __ _ _..______...... 33 Tropic Shale .. __.. ______, _..__.._ _ _._.._...... 33 Ferron Sandstone Member of Mancos Shale __ .______._.._...... 33 Straight Cliffs and Wahweap Sandstones _. __ _.._ _.._.._...... 33 Wahweap Sandstone ______.._ _.._.._.._._...... 33 Emery Sandstone Member of Mancos Shale __ _ _._ _._ .. 34 Star Point Sandstone and Blackhawk Formation _. __ _._._. __ ._ __ .. .. 34 Blackhawk Formation __ _._ .. __ _. .. __ _ _.. _._._. _ _._..... 34 Price River Formation _ ..______.__ _ _.._ _ 34 Kaiparowits Formation __ _ _ _.._._ _ _.. __ .._ _ _.._. 34 North Horn Formation _ _._ _.._ __.. __ _.. _...... 35 Flagstaff Limestone _ _ _ __._" "_""."'.' __'."'.""."_'" 35 Wasatch Formation ______36 Wasatch and Brian Head Formations _ _.. __ _._...... 36 Green River Formation _ _ , _ __ _...... 36 Crazy Hollow Formation _ _ _ _ .._...... 36 Igneous rocks of Tertiary age _ _ _.. _. __ ._ _.._._ _ __ .. __ ._ _...... 36 Conclusions and recommendations __ ._. __ _ _.. _. __ _ _...... 37 Selected references .. __ .__ .. .. _ _ _.. .. _ __ .. __ .. 39 Publications of the Utah State Engineer's Office _. ._ _.._ 80

- 2 - CONTENTS Page Abstract _ _ _ __._.._ _ _...... 5 Introduction _.._ _ _ _...... 6 Physiographic subdivisions of the Colorado Plateau...... 6 Distribution of precipitation on the Colorado Plateau _...... 8 Classification of natural water 8 Water from bedrock in the Uinta Basin section _...... 9 Madison Limestone and Morgan Formation _ _..... 12 Weber Sandstone _.._...... 12 Phosphoria Formation _...... 12 Park City Formation _...... 14 Navajo Sandstone _ _...... 14 Entrada Sandstone __ _...... 14 Frontier Sandstone Member of Mancos Shale _...... 14 Mancos Shale 15 Castlegate Sandstone _...... 15 Mesaverde Group _...... 15 Flagstaff Limestone 15 Wasatch Formation _ _...... 15 Green River Formation 17 Uinta Formation 17 Duchesne River Formation 19 Water from bedrock in the Canyon Lands section _.._...... 19 Rocks of Cambrian and Devonian age _ _...... 2l Rocks of Mississippian age _...... 21 Hermosa Group _...... 22 Molas Formation _ __ _...... 22 Rico Formation 22 Coconino Sandstone __ __ 23 Toroweap Formation 23 Kaibab Limestone _ __ 23 Cutler Formation _ __ _...... 23 Cedar Mesa Sandstone Member of Cutler Formation ._ _...... 23 Organ Rock Tongue of Cutler Formation 23 De Chelly Sandstone Member of Cutler Formation 24 White Rim Sandstone Member of Cutler Formation 24 Moenkopi Formation _...... 24 Sinbad Limestone Member of Moenkopi Formation 24 Chinle Formation _ _..... 24 Shinarump Member of Chinle Formation 25 Moss Back Member of Chinle Formation 25 Glen Canyon Group _...... 25 Wingate Sandstone __ __ _..... 25 Kayenta Formation _ _ __ _ .._...... 26 Navajo Sandstone _._ _.. _ _ _. __ 26 Carmel Formation _ __ 26

- 1 . TABLES Table Page 1. Correlation chart of bedrock formations of the Colorado Plateau of Utah _. __ .. __ _ 42 2. Selected hydrogeologic data from springs, water wells, and oil and gas wells in bedrock in the Uinta Basin section 44 3. Selected hydrogeologic data from springs, water wells, and oil and gas wells in bedrock in the Canyon Lands section...... 52 '01. Selected hydrogeologic data from springs, water wells, and oil and gas wells in bedrock in the High Plateaus section . 72

- 4 - ILLUSTRATIONS Figure Page 1. Index map of the Colorado Plateau in Ctah i 2. Isohyetal map In pocket 3. Geologic section A-A' of the Uinta Basin section near Vernal... .. 10 4. Geologic section B-B' of the Uinta Basin section near Roosevelt...... 11 5. Map showing locations of wells and springs in rocks of Paleozoic and Mesozoic age in the Uinta Basin section 13 6. Map showing locations of wells and springs in the Flagstaff Limestone and Wasatch, Uinta. and Duchesne River For- mations in the Uinta Basin section...... 16 i. Map showing locations of wells and springs in the Green River Formation in the Uinta Basin section...... 18 8. Geologic section C-C' of the Blanding Basin in the Canyon Lands section 20 9. Map showing locations of wells in rocks of Cambrian. Devonian. and Mississippian age in the Canyon Lands and High Pla- teaus sections In pocket 10. Map showing locations of wells and springs in rocks of Penn- sylvanian and Permian age in the Canyon Lands and High Plateas sections In pocket 11. Map showing locations of wells. springs. test holes, and water- yielding mine tunnels in the Moenkopi and Chinle Forma- tions in the Canyon Lands and High Plateaus sections ...... In pocket 12. Map showing locations of wells and springs in the Glen Canyon Group In pocket 13. Map showing locations of wells, springs. and water-yielding mine tunnels in the Carmel Formation, Entrada and Bluff Sandstones, and Morrison and Winsor Formations in the Canyon Lands and High Plateaus sections...... In pocket 14. Map showing locations of wells and springs in the Cedar Mountain and Burro Canyon Formations, Dakota Sand­ stone, and Mancos Shale (except Ferron Sandstone Mem- ber) in the Canyon Lands and High Plateaus sections ...... _ In pocket 15. Map showing locations of 'rells and a water-yielding mine tunnel in the Ferron Sandstone Member of Mancos Shale in the Canyon Lands and High Plateaus sections In pocket 16. Geologic section D-D' of part of the High Plateaus section...... 30 17. Map showing locations of wells and springs in rocks of Late Cretaceous age (except Dakota Sandstone and Mancos Shale in the High Plateaus section In pocket 18. Map showing locations of wells. springs, and water-yielding mine tunnels in rocks of Tertiary age in the High Plateaus section In pocket

- 3 - The High Plateaus section receives the greatest precipitation in the Colorado Plateau of Utah. and more than 16 inches a year falls on most of the section. This provides for abun­ dant recharge by direct infiltration to bedrock aquifers and by infiltration from perennial streams that flow into the Canyon Lands section. Very little water is withdrawn by wells from the aquifers in the High Plateaus. however, in relation to the potential yield of the aquifers. The formations that are known to contain fresh water in the High Plateaus include limestones of Paleozoic age, the Wingate and Navajo Sandstones, Carmel Formation. Tropic Shale, Wahweap and Straight Cliffs Sandstones, Emery Sandstone Member of the Mancos Shale, Blackhawk, Price River. Kaiparowits. and North Horn Formations, Flagstaff Lime­ stone. Wasatch. Brian Head, Green River, and Crazy Hollow Formations, and igneous rocks of Tertiary age.

INTRODUCTION This report on the bedrock aquifers of the Colorado Plateau of Utah was prepared by the U.S. Geological Survey in cooperation with the Utah Oil and Gas Conservation Commis­ sion. The purpose of the study was to determine which bedrock formations are water bearing and to report on the quality of water in these formations and their yield of water to springs, water wells, and oil and gas wells. The information is needed by the Oil and Gas Conservation Commission and by other State and Federal authorities to determine usability of the water and· to determine what protective measures may be needed to prevent water of poor quality from polluting usable ground and surface water. The study covered the I-year period from July 1964 to June 1965. This report is based on data compiled from published reports, which are listed in the sectior. "Selected refere:lces," and from unpublished data in the files of the U.S. Geological Survey, the Utah Oil and Gas Con­ servation Commission, the Utah State Engineer, and the Utah State Department of Health. Stratigraphic nomenclature used in this report is from published sources, mainly from the Utah State Geologic Map (Stokes, 1964), and may not agree with that used by the C'. S. Geo­ logical Survey. Many oil and gas companies provided upon request chemical analyses ofwater and other data from their files. The scope of the study did not permit a field check of exist­ ing wells. If this were done, undoubtedly data could be collected for many more wells. A discussion of the hydrology of ground water in bedrock is beyond the scope of this re­ port. R. E. Marsell (1964), however, describes the occurrence of ground water in bedrock, the bedrock ground-water provinces in Utah, and the effects of rock composition and geologic structure on ground water in bedrock.

Physiographic subdivisions of the Colorado Plateau The Colorado Plateau of Utah comprises about half the area of the State and is divided into three sections (Hunt, 1956, p. 3)-the Uinta Basin, Canyon Lands, and High Plateaus (fig. 1). Small parts of two other sections also extend a few miles into the southern part of Utah, but in this report they are included with the Canyon Lands and High Plateaus sections.

The Uinta Basin section is at the north edge of the Colorado Plateau. The section is elongated east-west and is structurally the lowest part of the plateau. The upturned strata on the north flank of the Uinta Basin form hogbacks along the south edge of the Uinta Moun­ tains, and the nearly horizontal strata of the south flank form the steep escarpments of the Roan and Book Cliffs. AJtitudes in the basin range from about 4,650 feet above sea level near Ouray on the Green River to 10,000 feet along the Roan Cliffs.

·6- WATER FROM BEDROCK IN THE COLORADO PLATEAU OF UTAH

by R. D. Feltis

Geologist, U. S. Geological Survey

ABSTRACT The bedrock aquifers in the Colorado Plateau of Utah supply water that ranges widely in chemical quality and yield. The range of dissolved solids in 649 samples collected from 534 wells, springs, and water-yielding mine tUImels was from less than 100 to more than 390.000 ppm (parts per million). The yield of wells ranged from less than 1 to 54,000 barrels of water per day (less than 1 to 1,600 gallons per minute); whereas the yield of springs ranged from less than 1 to 4,100,000 barrels of water per day (less than 1 to 121,000 gallons per minute). The Colorado Plateau of Utah is divided into three sections-the Uinta Basin, Can' yon Lands, and the High Plateaus. In the Uinta Basin, wells and springs have produced fresh to slightly saline water from the Madison Limestone, Morgan Formation, Weber Sandstone, Phosphoria and Park City Formations, Navajo and Entrada Sandstones, Frontier Sandstone Member of the Mancos Shale, Mesaverde Group, and the Wasatch, Green River, Uinta, and Duchesne River Formations. The major areas of recharge are the north flank of the basin, the Uinta Mountains on the north edge of the basin, and the high areas of the south flank. .'ill the permeable formations that crop out along the north flank of the basin are potential fresh­ water aquifers. Few wells have been drilled, however, and the areal extent of the fresh water is unknown. In most of the central part of the basin, the thick sequence of rocks of Tertiary age and the underlying rocks of Cretaceous age contain water too saline for most uses. The Canyon Lands section is divided into numerous hydrologic units by structural features such as the San Rafael Swell, Circle Cliffs and Monument Upwarps, the Abajo, Henry, and La Sal Mountains, and the faulted anticlines such as Salt, Spanish, and Lisbon Valleys. Most wells in the bedrock aquifers are restricted to a few areas, and few data are available for large parts of the section. In the Canyon Lands section, fresh to slightly saline water is produced from wells and springs in the Hermosa Group, Rico and Cutler Formations, Cedar Mesa Sandstone Member. Organ Rock Tongue, and De Chelly Sandstone Member of the Cutler Formation, Chinle Forma­ tion, Shinarump Member of the Chinle Formation, Wingate Sandstone, Kayenta Formation, Navajo Sandstone, Carmel Formation, Entrada and Bluff Sandstones, Morrison and Burro Can­ yon Formations, and the Dakota Sandstone. The quality of water changes from area to area, however, and an aquifer containing fresh water in one area may contain saline water or brine in another. The area of greatest development of ground water in the Canyon Lands section is the Blanding Basin in southeastern San Juan County. In the western part of the basin, n, '.r Bluff, wells in the Glen Canyon Group yield water containing less than 500 ppm of dis­ solved solids. Toward the east near Aneth, however, the ground water contains more than 8,000 ppm of dissolved solids.

- 5 - The Canyon Lands section is south of the Uinta Basin. The generally flat-lying rocks of this section are incised by streams that form the canyons. leaving intervening broad mesas and buttes. An intricate system of deep canyons along and across hogbacks and cuestas has resulted from faulting, upwarps (such as the San Rafael Swell), and distortion of rocks around mountains formed by intrusive rocks (such as the Henry Mountains). The Canyon Lands sec­ tion generally ranges in altitude from 4,000 to 7,000 feet, with peaks of mountains ranging from about 8,000 to 12,700 feet. The High Plateaus section consists of long, north-trending plateaus along the west edge of the Canyon Lands section. The topography of the section is mostly controlled by faults. al­ though some of the escarpments were caused by differential erosion. Most of the plateaus are 9.000 feet high, but some are as high as ll,OOO feet.

Distribution of precipitation on the Colorado Plateau

Precipitation is the source of the water in the bedrock aquifers in the Colorado Plateau. The normal annual precipitation on the plateau ranges from less than 6 to more than 40 in­ ches. but on most of the plateau the precipitation is less than 12 inches (fig. 2). The High Plateaus section has the greatest precipitation and more than 16 inches falls on most of the section. In addition to providing recharge to the aquifers. there is sufficient pre­ cipitation to maintain the flow of several perennial streams that are tributary to the Colorado River or that flow into the Great Basin. In the Canyon Lands section. peaks in the Henry, La Sal, and Abajo Mountains receive more than 30 inches of percipitation. These areas are very small in comparison to the vast area of the Canyon Lands, however, al'1d less than 10 inches falls on most of the section. Few perennial streams head in the section. In the Uinta Basin section, high areas along the south flank and on the west end receive more than 30 inches of precipitatio\1; but these areas are small in comparison to the size of the basin. Less than 12 inches falls on most of the basin. A large part of the Uinta Moun­ tains north of the Uinta Basin receives more than 30 inches of precipitation. These mountains contribute a large amount of water to the bedrock aquifers along the north edge of the basin, and several perennial streams head in the mountains and flow into the basin.

Classification of natural water

The water from springs. water wells, oil and gas tests, bore holes, and mines in the Colo­ rado Plateau varies greatly in chemical quality because of different geologic and hydrologic environments. In order to classify these waters as fresh. saline, or briny, the following clas­ sification based on concentration of dissolved solids or specific conductance (Robinove. Lang­ ford, and Brookhart, 1958, p. 3) is used: Specific Dissolved solids conductance Class (ppm) (micromhosjcm at 25°C) Fresh _ _ __..__ o to 1,000 o to 1,400 Slightly saline ._ 1,000 to 3.000 1.400 to 4,000 Moderately saline _.. 3.000 to 10,000 4,000 to 14,000 Very saline _ .. 10,000 to 35.000 14,000 to 50,000 Briny _ . More than 35,000 More than 50,000

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Figure 3. - Geologic section A-A' of the Uinta Basin section near Vernal.

. 10 - WATER FROM BEDROCK IN THE UINTA BASIN SECTION

The Uinta Basin is an asymmetric syncline with an axis that is concave southward and generally parallel to the eastward-trending Uinta Mountains that lie to the north. Beds that form the north flank of the basin dip steeply southward away from the Uinta Mountains. Beds that form the south fb.nk dip up to 5° northward toward the axis of the syncline. Rocks of Precambrian, Cambrian, and Mississippian through Tertiary ages are exposed in and around the basin or have been identified in oil wells. Table 1, columns 2, 3, 4, and 5, show the strati­ graphic section for the Uinta Basin.

Chemical analyses of water from springs, water wells, and oil and gas wells show that the following formations contain fresh water: Madison Limestone, Morgan Formation, Weber Sandstone, Phosphoria and Park City Formations, Navajo and Entrada Sandstones, Frontier Sandstone Member of the Mancos Shale, Mesaverde Group, and the Wasatch, Green River. Uinta, and Duchesne River Formations. The areal extent of the fresh water in each forma­ tion is not fully known because of the scarcity of points at which samples could be obtained.

The electrical logs of oil and gas wells used in constructing figure 3 indicate slightly sa­ line water in the Navajo. Entrada, and Dakota Sandstones, and the Frontier Sandstone Mem­ ber of the Mancos Shale. Electrical logs used in constructing figure 4 indicate fresh or slightly saline water in the Weber and Navajo Sandstones and the Green River and Duchesne River Formations.

Hydrologic data are not available fo::, many of the formations in the basin, mainly because water wells have not been drilled to test the quantity or quality of water and because such data were not collected during oil and gas exploration. Data are least available in the north­ western part of the basin where oil and gas exploration has not been extensive and water wells have not been drilled deep enough to penetrate all potential aquifers.

Recharge to bedrock aquifers of the Uinta Basin occurs mostly along the north flank of the basin and to a Jesser extent on the areas of highest elevations on the south flank of the basin. Along the north flank runoff from the Uinta Mountains, Split Mountain, and Blue Mountain Plateau percolates into the upturned outcrops of formations that dip steeply into the basin. Precipitation directly on these outcrops also is a source of recharge. Because numerous formations are exposed to recharge, fresh or slightly saline water should be ex­ pected in most permeable formations near the north edge of the basin. On the south flank of the basin, most recharge is in the areas of highest altitude where precipitation is greatest. However, because of the low dip of the south flank, few formations except the Green River Formation are exposed to recharge. Wells drilled below the formation that crops out seldom yield fresh or slightly saline water.

Table 2 contains selected hydrogeologic data from springs, water wells, and oil and gas wells in bedrock in the Uinta Basin section; locations of the sampling sites are shown in fig­ ures 5, 6, and 7. Following is a summary of the data by formation.

·9- Madison Limestone and Morgan Formation

Water from warm springs issuing near the top of the Madison Limestone, or possibly at the base of the Morgan Formation in T. '" S.. R. 24 E.. flows into the Green River about 2 miles above the mouth of the canyon at Split Mountain. The dissolved-sclids content of the water is 942 ppm (parts per million) (fig. 5 and table 2). In September, 1948, the discharge of the springs above river level was estimated to be 6 cfs (cubic feet per second) (2,700 gpm. gallons per minute. or 1.500 bwpd. barrels of water per day) and an equal amount or more was believed to discharge directly into the river (Thomas, 1952. p. 12). The source of water for the springs is probably from the south flank of the Uinta Mountains where the Madison and Morgan formations crop out. These formations could also be a partial source of the water produced in the Ashley Valley oil field. (See discussion of Weber Sandstone below.) The Morgan Formation. Madison Limestone. and other limestones of Mississippian age crop out over a wide area along the south flank of the Uinta Mountains, and they all should be con­ sidered potential fresh-water aquifers along the north edge of the basin.

Weber Sandstone

The water from oil wells, abandoned oil tests converted to water wells, and springs in the Weber Sandstone ranges from about 400 t-o 2.600 ppm of dissolved solids (fig. 5 and table 2). The source of the water in the Weber is from recharge to areas of outcrop in Split Mountain and along the south flank of the Uinta Mountains. Oil wells in the Ashley Valley oil field produce water from the Weber Sandstone. but some of the water possibly comes from limestone of Pennsylvanian and Mississippian ages which underlies the Weber (Goode and Feltis. 1962. p. 12). Normal faults in the oil field, described by Peterson (1957, p. 191), could {:Ossibly form conduits between the underlying limestones and the Weber. Some of the wells in the Ashley Valley oil field are open to both the Weber and the overlying Phosphoria Formation. and the range in dissolved solids in water from these wells is about 500 to 2.600 ppm (fig. 5 and table 2). During 1964. the 28 oil wells in Ashley Valley oil field produced about 36.5 million barrels of water. Some of the high-volume pumps produce more than 9.000 bwpd (270 gpm) (Johnson. 1964. p. 187). Yields of individual wells at the time of sampling are listed in table 2. The Weber Sandstone should be considered as a potential fresh-water aquifer all along the northern edge of the basin.

Phosphoric Formation Water is produced with oil from wells developed in the Phosphoria Formation' in the Ashley Valley oil "field; however, it is questionable whether or not the Phosphoria actually yields the water. V. E. Peterson (1957, p. 191) described the reservoir as follows: "Where porosity is present within the Phosphoria Formation. it is probable that this reservoir is common with that of the Weber Sandstone. Pronounced vertical fracturing in the Phosphoria in many of the wells probably connects the two reservoirs. * * * All of the W(~lls are now producing ma­ terial amounts of water with the oil and it is believed that water has invaded the oil reservoir through fractures." Therefore, most of the water in the Phosphoria probably comes from the Weber Sandstone or underlying formations.

1 See discussion on nomenclature in the section on Park City Formation below.

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Figure 4. - Geologic section 6-6' of the Uinta Basin section near Roosevelt.

- II - Park City Formation

The Park City Formation is a potential aquifer along the north flank of the Uinta Basin, especially where the formation thickens toward the west. Although rocks of Permian age that crop out in the eastern Uinta Mountains are mapped as Park City (Kinney. 1955, pI. 1), for the subsurface, the term Phosphoria Formation has been used in most logs of oil tests. Consequently, water samples obtained from oil tests are considered to be from the Phos­ phoria. A spring in T. 2 S., R. 22 E., yields water from near the base of the Park City (fig. 5). The water contains 228 ppm of dissolved solids (table 2). and the spring was discharg­ ing at a rate of about 3 cis (46,000 bwpd or 1,350 gpm) when visited in August 1950.

Navajo Sandstone

Few wells produce water from the Navajo Sandstone in the Uinta Basin, although it is an aquifer that probably contains fresh or slightly saline water along the north flank of the basin. Along the north flank of the basin. most oil tests that penetrate the Navajo are re­ ported to obtain potable water or water suitable for irrigation. An oil well in sec. 12, T. 4 S., R. 20 E., in 1950 had an artesian flow of approximately 2,000 bwpd 160 gpm) of potable water from the Navajo; however, by 1958 the flow had declined to about 850 bwpd (25 gpm). Water from a well in the Navajo in T. 4 S., R. 21 E., contained 1,894 ppm of dissolved solids (fig. 5 and table 2); however, the sample was reportedly contaminated by drilling mud. No yield data are available. Two springs, in T. 1 N., R. 7 W. (USM, Uinta Special Meridian). and T. 4 S., R. 23 E., -yield water containing 148 and 342 ppm of dissolved solids at estimated rates of 1,400 and 70 bwpd (40 and 2 gpm). In the northwestern part of the Uinta Basin, the name Nugget Sandstone is generally used instead of Navajo Sandstone. -

Entrada Sandstone

Chemical analyses are available for water from the Entrada Sandstone on the north fla1"'J< -of the Uinta Basin from a spring in T. 4 S., R. 23 E., and from two oil wells in T. 5 S., R. 22 E., and on the south flank from four gas tests in Tps. 15, 151/:.:, and 17 S., Rs. 22, 23. and 24 E. (fig 5 and table 2). The spring water is fresh; and the two oil wells yielded water con­ taining 479 and 1,165 ppm of dissolved solids at rates of 664 and 375 bwpd (19 and 11 gpm). Also on the north flank of the basin. electrical logs of oil wells used in constructing figure 3 indicate fresh or slightly saline water in the Entrada. On the south flank of the basin, water from the gas tests contained from 58,000 to 104,000 ppm of dissolved solids. Drilling reports of oil wells in the Cisco area, south of the Book Cliffs, also report "briny" or "salty" water from the Entrada.

Frontier Sandstone Member of Mancos Shale

Two springs in the Frontier Sandstone Member at T. 1 S., R. 8 W. (USM) , and T. 4 S., R. 23 E., each yield about 1 gpm of water containing 786 and 2,620 ppm of dissolved solids (fig. 5 and table 2). The electrical logs of oil wells used in constructing figure 3 indicate fresh or slightly saline water in the Frontier.

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Figure 5. - Locations of wells and springs in rocks of Paleozoic and Mesozoic age In the Uinta Basin section.

• 13 - , I :::0•• I ~~§

EXPLANATION I'tthrn of ..II ~ ~"l ...i", outcroo ".t.,...... ,.,", t i'IIlDOI ,,_001 G r.r Ouc".s", Ii ~.r FOr.llatlon 9 ~ r. Uinta FOr"INtion 0 0- I ~ r. _•••lefl FO"l(lo" • ... , lIGJ] TI F1 ...utt I..i,..ston. .1 "...... ,. "".1' 1,"1:101 ''''chcat.. clau.ficatlon of ..... ur ,...1. (,.. II. 5\. ,..:--:- ·-1" I, t,...,,: 1. ,I,,"tl., s.l in': l. iflO4.,.aU', ,al ina: Il. • .,,.,.., ul,i".: 15. ,r,ny '..-1 - ~- _~~ I ---,,>,r.,- I r--.J.J ' )/' I, I / .

Ba,. from U. S. GoolaqicaJ StI'''." State o 10 lO ~o 40 IU~ES Sa •• "-lao. /9'9; .cal. I;~OO.OOO I I I Goeoloq,. tr04ll Stoll;u (:i}6~1. I I H.,drOloqy ~, ~. J. ;:''!! tl t.

Figure 6. - Locations of wells and springs in the Flagstaff Limestone and Wasatch, Uinta, and Duchesne River Formations in the Uinta Basin sedion.

- 16 - Mancos Shale The fine-grained materials and abundance of soluble salts in the Mancos Shale suggest that this formation does not contain fresh water. Water from an oil well in the shale in T. 11 S., R. 25 E., contained 5,800 ppm of dissolved solids (fig. 5).

Castlegate Sandstone Chemical analyses of water from the Castlegate Sandstone at two oil wells in Tps. 14 and 15 S., Rs. 20 and 21 E., in southern Uintah County showed a dissolved-solids content of 4,711 and 33,253 ppm (fig. 5 and table 2). Another analysis of water from the Castlegate and the Mesaverde Group in T. 10 S., R. 24 E., showed a dissolved-solids content of 20,452 ppm. Fresher water may be present in the Castlegate along the southwest edge of the basin north and northwest of Price, where the area of outcrop is larger and recharge is greater.

Mesaverde Group Six chemical analyses of water from four oil wells in the Mesaverde Group show a range of 12,511 to 62,502 ppm of dissolved solids (table 2). The wells were in T. 9 S., R. 23 E., T. 10 S., R. 24 E. (two wells), and T. 12 S., R. 14 E. (fig. 5); and the reported yield of water from one of the wells in T. 10 S., R. 24 E., was 38 bwpd (1 gpm). One spring in T. 17 S., R. 17 E., and two springs in T. 20 S., R. 20 E., all three in the Mesaverde, yield water con­ taining 707, 660, and 1,090 ppm of dissolved solids, respectively.

Flagstaff Limestone Water from an oil well in the Flagstaff Limestone in T. 14 S., R. 20 E., contained 8,245 ppm of dissolved solids (fig. 6 and table 2) .. The oil well is near the eastern extent of the for­ mation and distant from possible recharge areas. The formation may contain fresh water in the southwestern part of the basin adjacent to the High Plateaus, in which area the forma­ tion does yield fresh water to water wells and springs. (See discussion of High Pleateaus section.)

Wasatch Formation Chemical analyses of 11 water samples collected from the Wasatch Formation in 7 oil and gas wells indicate that 2 of the samples are slightly saline and the other 9 range from moderately saline to briny (fig. 6). One of the samples of slightly saline water was obtained from a well in T. 15 S., R. 21 E. The water contained 1,966 ppm of dissolved solids, and the aquifer probably is being recharged in the area of relatively high precipitation north of the Roan Cliffs. The other sample of slightly saline water was obtained from a well in T. 1 N., R. 1 E. (USM). The water contained 1,302 ppm of dissolved solids, and the aquifer probably is being recharged in the subsurface by interformational leakage along the south flank of the Uinta Mountains rather than by direct infiltration in the area of outcrop. Yield data are not available for the seven oil and gas wells. A spring in T. 16 S., R. 17 E., yielded fresh water having 596 ppm of dissolved solids while flowing at a rate of 7,650 bwpd (225 gpm) in Septem­ ber 1948. ,Additional smaller springs probably discharge from the Wasatch along the escarp­ ment of the Roan Cliffs.

- 15 - , . ·,.:.;":.",-',1. ·..·1 , , ...... , '" '--.I ~- ....-.~.... _,~.. --,

~f_....__- "'l:v,.f':~ .~ :. i:..!'?..... _ " -r-__ ...J ....;..~ 1 ~~~-~ ,[0.' - --'[ ...- -,' ,> , ~ a . .;..... I

EXPLANATION 'uu,... ot ..,1 So .. ,", ou tento .et',...,••,.,", 'oI .. t t ,,-., .y••' m T, -i,•.,. JI~'" rOntlatlol'l 0 0-

... ~"' .... .".,. 1._001 ,rlC~lcat •• alu,.fiedlon ot ..ce," ulIRol. (s.. l). !J. I. f,.uft: Z. sli1/tt1y sali",: J. lIOcI,rat"r ••1,,,,: :4".r., laillte: 5. 0"''''1

.. , i .. ~

30 ..1 from U.S. ~.o.()qic:ol 5""",'1' 5'CI" o 10 20 30 40 MI~ES !a.1 Mao, t9~9; ,cale 1:'00,000 I ! I Q.alot, frOli Stell•• (1-9."'. I it'cirolQ4J l), ~. O. f,lta.

Figure 7. - Locations of wells and springs in the Green River Formation in the Uinta Basin section.

- 18 - Green River Formation

The chemical quality of the water in the Green River Formation ranges from fresh to briny. Analyses of 73 water samples collected from 51 wells and 1 spring indicate that 4 were fresh, 18 were slightly saline. and the remaining 51 were moderately saline to briny (fig. 7). Three of the samples of fresh water came from two wells and a spring, and most of the slightly saline water came from wells on the scuthern flank of the Uinta Basin. The fresh water was obtained from a gas well in T. 11 S., R. 12 E., an oil well in T. 14 S., R. 20 E., and a spring in T. 15 S., R. 23 E.; and they contained 619, 818, and 381 ppm of dissolved solids, respectively. The occurrence of fresh and slightly saline water along the southern flank of the basin suggests that the aquifers are recharged in the area of high precipitation north of the Roan Cliffs (fig. 2). The fourth sample of fresh water was obtained from an oil well in T. 2 N., R. 2 W. (USM). The well yielded. water containing only 348 ppm of dissolved solids from a depth of 4,115 feet. The Green River does not crop out in the central part of the north flank of the Uinta Basin; therefore, recharge to the aquifer in T. 2 N., R. 2 W. (USM) , probably is by interformational leakage. The electrical logs used in constructing figures 3 and 4 show the occurrence of fresh and saline water in the Green River in the southeastern and northern parts of the Uinta Basin.

The yield of water from the Green River Formation, as indicated by tests at 17 oil and gas wells, ranges from 17 bwpd (0.5 gpm) to 7.200 bwpd (200 gpm). Two gas wells in sec. 35, T. 10 S., R. 20 E., and sec. 17, T. 10 S.. R. 22 E., were converted to water wells; and in 1964 they flowed. at rates of 2,700 bwpd (80 gpm) and 340 bwpd (10 gpm). The largest re­ ported yield of water from the Green River ~ from an oil well in T. 9 S., R. 24 E., which p~ duced 7,200 bwpd (220 gpm) from a depth of 1,932 feet.

On the south flank of the Uinta Basin the Green River Formation is a potential source of fresh or slightly saline water that could be used. in the process of oil extraction from bi­ tuminous sand and oil shale.

Uinta Formation

The Uinta Formation yields water that ranges in chemical quality from fresh to briny (fig. 6). In T. 7 S., Rs. 22 and 24 E., two oil wells yielded water containing 2,365 and 898 ppm of dissolved solids (table 2), the latter at a rate of 3,600 bwpd (liO gpm). Two oil wells in T. 9 S., R. 23 E., and T. 4 S., R. 5 W. (USM), yielded water containing 81,200 and 22,915 ppm of dissolved solids, the latter at a rate of 1,000 bwpd (30 gpm). A spring in the Uinta in T. 1 S., R. 8 W. (USM) , yielded. water containing 237 ppm of dissolved. solids at a rate of 1,700 bwpd (50 gpm). Three springs in T. 4 S., R. 7 W. (USM) , and T. 5 S., Rs. 6 and 7 W. (USM) , yielded. water containing 7,320, 1,840, and 2,710 ppm of dissolved. solids at rates of 680, 6,800, and 7,800 bwpd (20, 200, and 225 gpm).

Water from three water wells in T. 2 S., R. 5 W. (USM) , and T. 3 S., Rs. 3 and 8 W., (USM) , contained. 439, 788, and 4,430 ppm of dissolved solids and the well in T. 3 S., R. 3 W., yielded 680 bwpd (20 gpm).

- 17 - c

~200'

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.1 c.- l!=O..-LIOl'/ / ,lOG / / / / / / (il_ , ....,0" ~,.~. / / / / ,..... / / / I / ]2oa'~ "..,. I I lt~:~~'~.i:II,,~:d;;~.~, f~:':::-?:;~"'t"~ '~QlI I I I 111 l~Il." ':::31tU,ct, llU"llneo )<'I t!\. ''''1' I .Jt electrlca' ' ..0 1.' •• Oft 1eo·"'ll'<;011 t~... 1"'1" J' lI''' I ra. tile stan ,.oloqlc I •• ( '"I. ,-'-! ,- Hot'i zanul scale Verti eal scale ,x_'t.ratecl Location ot s.ction Oft tiq",.. 12 Oatu. ,. ".... ,.. le"el

Figure 8. - Geologic section C·C' of the Blonding Basin in the Canyon Lands section.

- 20 • The chemical quality of water in the Uinta Formation is determined principally by the lithology of the formation and local re<:harge conditions. In the central part of the basin. the formation is composed predominantly of fine-grained lake deposits that contain large quan­ tities of soluble salts; but it yields fresh and slightly saline water where local pre<:ipitation or runoff from the Uinta Mountains re<:harges the formation. In the eastern part of the basin. where there is little precipitation, wells may yield fresh or slightly saline water from coarse­ grained fluvial deposits that contain few soluble salts (Picard, 1957, p. 128).

Duchesne River Formation

Sandstone beds in the Duchesne River Formation are a source of fresh water for the city of Roosevelt and for private domestic wells. Data from five water wells indicate a range in dissolved solids from 234 to 528 ppm (fig. 6 and table 2) and a range in yield from about 60 to 340 bwpd (2 to 10 gpm). The source of water in the formation is from recharge by surface streams that cross the area of outcrop and by pre<:ipitation directly on the area of outcrop along the north flank of the basin. The formation dips southward. and artesian conditions occur where water wells tap the aquifer in T. 2 S., R. 1 W. (USM). Water wells penetrate the Duchesne River to a maximum known depth of 810 feet; however. logs of oil wells show the formation to be as much as 4,000 feet thick. The electrical log of the well in se<:. 5, T. 1 N., R. 2 W. (USM) in figure 4 indicates that the base of the slightly saline water in the Duchesne River may be as much as 3,460 feet deep.

WATER FROM BEDROCK IN THE CANYON LANDS SECTION

The Canyon Lands section is the most structurally complex part of the Colorado Plateau in Utah. Three upwarps-the San Rafael Swell and Circle Cliffs and Monument Upwarps­ are the major structural elements in the section. The upwarps and adjacent basins are modified by numerous subsidiary folds and faults and by the intrusives that formed the Abajo and Henry Mountains. In the northeastern part of the Canyon Lands section is a northwest-trending belt of faulted anticlines, including Salt, Spanish, and Lisbon Valleys. Near the center of this area is the La Sal Mountains. also formed by an intrusive. Sedimentary rock of Cambrian and Devonian through Cretaceous age are exposed in the Canyon Lands section or have been identified in oil wells. Table 1, columns 6, i, 8, and 9, show the strati­ graphie section for the Canyon Lands.

Chemical analyses of water from water wells. oil and gas wells, and springs show that fresh water is in the Hermosa Group, the Rico and Cutler Formations, the Cedar Mesa Sandstone Member, Organ Rock Tongue, and De Chelly Sandstone Member of the Cutler For­ mation. Chinle Formation, Shinarump Member of the Chinle Formation, Wingate Sandstone, Kayenta Formation, Navajo Sandstone. Carmel Formation. Entrada and Bluff Sandstones, Morrison and Burro Canyon Formations. and the Dakota Sandstone. Many of the analyses are for water from scattered springs and stock wells that are the only source of ground water for hundreds of square miles.

The electrical logs of oil and gas tests used in constructing figure 8 indicate that water in bedrock in the Blanding Basin ranges from fresh to saline in chemical quality.

• 19 - the Leadville Limestone and the Ouray Limestone of Devonian age contained 31.583 and 71,948 ppm of dissolved solids. The Madison Limestone yielded water containing 54.624 and 8.037 ppm of dissolved solids to oil wells in T. 16 S., R. 12 E., and T. 29 S., R. 10 E. lfig. 9 and table 3). In T. 16 S., R. 9 E., and T. 36 S., R. 10 E., oil wells in the Redwall Limestone yielded water containing 73,653 and 4.669 ppm of dissolved solids and in T. 15 S.. R. 12 E., an oil well in the Redwall Limestone and Elbert Formation of Devonian age yielded water containing 67.769 ppm of dissolved solids (fig. 9 and table 3). Chemical analyses of 52 water samples from the undifferentiated rocks of Mississippian age showed a range of from 7,172 to 3Z7,283 ppm of dissolved solids (fig. 9 and table 3). Six of the water samples were moderately saline, 16 samples were very saline, and 30 samples were brines. In T. 40 S., R. 7 E., rocks of Mississippian and Devonian age yielded water containing 2,339 ppm of dissolved solids; and in T. 40 S., R. 26 E., and T. 41 S., R. 21 E .. rocks of Mississippian age and the Ouray Limestone of Devonian age yielded water containing 39,869 and 83,940 ppm of dissolved solids (fig. 9 and table 3).

An oil well in rocks of Mississippian age and the overlying Molas Formation in T. 35 S., R. 3 E., yielded water containing 9,378 ppm of dissolved solids lfig. 9 and table 3) at a rate of 528 bwpd (16 gpm).

Hermosa Group

Most of the water samples from the Hermosa Group for which chemical analyses are available are from oil wells in the Paradox Formation. Analyses of 34 samples show a range of 5,342 to 397,061 ppm of dissolved solids (fig. 10 and table 3); and 25 of the samples were brines containing more than 35,000 ppm of dissolved solids. A spring in the Hermosa in T. 33 S.• R. 16 E .• yielded water at a rate of 15,300 bwpd l450 gpm) that contained 414 ppm of dissolved solids.

Molas Formation

A water sample from the :\'Iolas Formation in an oil well in T. 39 S., R. 13 E., contained 6,035 ppm of dissolved solids lfig. 10 and table 3).

Rico Formation

Chemical analyses of water from the Rico Formation are available for water from five springs and one water well. Three springs in T. 33 S., R. 15 E., yielded water with 1,220, 3.920. and 4,770 ppm of dissolved solids at rates of about 70, 510, and 850 bwpd (2, 15, and 25 gpm) (fig. 10 and table 3). Two springs in T. 40 S., R. 17 E., and T. 41 S., R. 19 E., yielded water containing 719 and 3,070 ppm of dissolved solids, each at a rate of about 170 bwpd (5 gpm). A water well in T. 35 S., R. 15 E., yielded water containing 318 ppm of dissolved solids at a rate of 350 bwpd (10 gpm).

- 22 - De Chelly Sandstone Member of Cutler Formation In T. 41 S., Rs. 24 and 25 E., the De Chelly Sandstone Member yielded water containing 17,262 and 52,187 ppm of dissolved solids from two oil wells (fig. 10 and table 3). The yield of the well in T. 41 S., R. 24 E., was 270 bwpd (8 gpm). Three springs in the sandstone in T. 43 S., Rs. 14 and 19 E., yielded fresh water at rates generally less than 140 bwpd (4 gpm). At Chinle, Ariz., about 90 miles south of Bluff. Utah, water wells in the De Chelly yielded water containing less than 400 ppm of dissolved solids. Electrical logs of oil wells in the Blanding Basin indicate that the De Chelly contains fresh or slightly saline water along the Comb Ridge Monocline, but the water becomes more saline toward the center of the basin.

White Rim Sandstone Member of Cutler Formation The dissolved-solids content of water from six oil wells in the White Rim Sandstone Mem­ ber in the west-central Canyon Lands section ranged from 2,045 to 6,045 ppm of dissolved solids (fig. 10 and table 3). Water from two springs in the White Rim in T. 40 S., R. 10 E., yielded water containing 2,470 and 4,060 ppm of dissolved solids at rates of about 70 and 5,100 bwpd (2 and 150 gpm).

Moenkopi Formation In T. 24 S., R. 13 E., water sampled at two depths in an oil well in the lYIoenkopi Forma­ tion contained 12,472 and 15,999 ppm of dissolved solids. The latter sample was obtained with a reported yield of 94 bwpd (2.8 gpm). In T. 24 S., R. 14 E., however, another oil well yielded water from the formation that contained only 4,187 ppm of dissolved solids lfig. 11 and table 3). Two springs in T. 35 S.• Rs. 13 and 14 E., yielded water containing 1,700 and 1,860 ppm of dissolved solids at rates of 15,300 bwpd (450 gpm) and l,iOO to 13,700 bwpd (50 to 400 gpm). Another spring in T. 31 S.• R. 14 E., yielded water containing 2,355 ppm of dissolved solids; and a spring in T. 20 S.. R. 11 E., yielded water containing 2,250 ppm of dissolved solids at a rate of 680 bwpd (20 gpm).

Sinbad Limestone Member of Moenkopi Formation In T. 16 S., R. 12 E., oil wells in the Sinbad Limestone Member yielded very saline to briny water. In T. 24 S., R. 13 E., an oil well in the Sinbad yielded water containing 18,125 ppm of dissolved solids (fig. 11 and table 3). In oil wells in T. 29 S.. Rs. 10 and 12 E .• the Sinbad yielded water containing ·!,437 and 9.130 ppm of dissolved solids. \vith the latter at the rate of 432 bwpd (13 gpm). A water sample collected from the Kaibab Limestone, the Sinbad Limestone Member, and undifferentiated beds in the :Yloenkopi Formation in an oil well in T. 29 S., R. 11 E., contained 6,167 ppm of dissolved solids.

Chinle Formation Water from the Chinle Formation in oil tests in T. 22 S.. R. 22 E., and T. 26 S.. R. 7 E., contained 20,070 and 20.797 ppm of dissolved solids (fig. 11 and table 3), with the former at the' rate of 34 bwpd (1 gpm). A spring in T. 39 S., R. 14 E., yielded \vater conta'ning 747 ppm of dissolved solids. The water from this spring, however, may be discharging at the top of the Chinle after percolating downward through rocks of the overlying more permea,ble Glen Canyon Group.

- 24 - Coconino Sandstone

Chemical analyses of water from three oil wells in the Coconino Sandstone in T. 16 S.. R. 12 E., T. 18 S., R. 14 E., and T. 'l:7 S., R. 15 E., showed 17,249,49,902, and 3,378 ppm of dis­ solved solids (fig. 10 and table 3).

Toroweap Formation

Water from an oil well in the Toroweap Formation in T. 35 S., R. 3 E., contained 7,583 ppm of dissolved solids (fig. 10 and table 3).

Kaibab limestone

Water from four oil wells in the Kaibab Limestone in T. 29 S., R. 10 E., T. 37 S., R. 2 E., T. 18 S., R. 14 E., and T. 20 S., R. 7 E., contained 3,720. 14.179. 35,985, and 72,000 ppm of dis­ solved solids (fig. 10 and table 3). A spring in T. 24 S., R. 10 E., yielded water having 2,150 ppm of dissolved solids at a rate of about 170 bwpd (5 gpm). (A water sample from the Kaibab Limestone and the Sinbad Limestone Member of the Moenkopi Formation is discussed in the section on the Sinbad Limestone Member.)

Cutler Formation

A water well in the Cutler Formation in T. 25 S.,P... 23 E., yielded water having 931 ppm of dissolved solids at a rate of about 6.800 bwpd (200 gpm) (fig. 10 and table 3). The Cutler probably contains fresh or slightly saline water in other areas around the flanks of the La Sal Mountains. A spring in T. 33 S., R. 16 E., yielded water containing 770 ppm of dissolved solids at a rate of 12,200 bwpd (360 gpm). In T. 29 S., R. 26 E., and T. 28 S.• R. 23 E., water from two oil wells in the Cutler contained 4,957 and 16,331 ppm of dissolved solids.

Cedar Mesa Sandstone Member of Cutler Formation

Two water wells in the Cedar Mesa Sandstone Member in T. 41 S.• R. 16 E., and T. 43 S., R. 14 E., yielded water of 1,890 and 656 ppm of dissolved solids at rates of about 100 and 70 bwpd (3 and 2 gpm) (fig. 10 and table 3). Seven springs (in Tps. 36, 37, and 42 S., Rs. 16­ 18 E.) in the sandstone in San Juan County yielded water containing 298 to 596 ppm of dissolved solids at rates generally less than 170 bwpd (5 gpm).

Organ Rock Tongue of Cutler Formation

A water sample from an oil well in thE' Organ Rock Tongue in T. 29 S.. R. 10 E., con­ tained 4,487 ppm of dissolved solids (fig. 10 and table 3). Two springs, one in T. 43 S., R. 16 E., and another in T. 34 S., R. 14 E., yielded water containing 944 and 375 ppm of dissolved solids. The former }ielded less than 3 bwpd (0.1 gpm) , but the latter flowed at a rate of about 1,000 bwpd (30 gpm).

. 23 - Kayenta Formation

The Kayenta Formation generally acts as a barrier to the vertical movement of ground water rather than as an aquifer (M. E. Cooley, written commun.. 1965). Many springs in the Glen Canyon Group issue at the base of the Navajo Sandstone or near the top of the Kayenta because the more impermeable rock of the Kayenta restricts or stops the downward flow of water. Three springs in the Kayenta in T. 31 S., R. 15 E., T. 39 S., R. 11 E., and T. 42 S., R. 12 E., yielded water containing 220, 115, and 144 ppm of dissolved solids at rates of 70 bwpd (2 gpm) or less lUg. 12 and table 3).

Navajo Sandstone

Most water wells in the Glen Canyon Group draw water from the Navajo Sandstone, prob­ ably because it is the shallowest and most permeable formation in the group. Twenty-one water wells in the Navajo yielded water containing from 171 to 7,250 ppm of dissolved solids at rates ranging from 70 to 45,400 bwpd (2 to 1,335 gpm) (fig. 12 and table 3). Five of the wells in Tps. U and 42 S., Rs. 21 to 23 E., are in the Blanding Basin, east of Comb Ridge. These five wells in the Navajo yielded water containing from about 170 to 500 ppm of dissolved solids at rates ranging from 70 to 1.200 bwpd (2 to 35 gpm). The chemical quality deterio­ rates toward the east, however, and two water' wells_ in the Navajo in T. ·n S., R. 25 E., yielded water containing 7,080 and 7.250 ppm of dissolved solids at rates of 2,000 and 2,450 bwpd (60 and 72 gpm). The recharge area for the aquifer in the Blanding Basin is in the area of out· crop of the sandstone along the length of Comb Ridge r.lonocline. Ten wells drilled in the ~avajo in Arizona and Utah to supply water at the Glen Canyon Dam construction facility in Arizona yielded water containing from 216 to 1,814 ppm of dissolved solids at rates rang­ ing from 1,200 to 45,400 bwpd (35 to 1,335 gpm) lGoode, 19?4, p. 45 and 60). Chemical analyses of water from 14 springs in the Navajo Sandstone showed a range of dissolved solids from 129 to 354 ppm. The yield of the springs ranges from less than 34 bwpd (1 gpm) to 1,700 bwpd (50 gpm); but most of the springs yield 340 bwpd (10 gpm) or less. Chemical analyses are available for four water samples from the Navajo Sandstone obtained from oil wells. Two wells in T. 41 S., R. 24 E., yielded water containing 3,410 and 3,890 ppm of dissolved solids, and wells in T. 15 S., R. 11 E., and T. 26 S., R. 7 E., yielded water containing 3,607 and 320 ppm of dissolved solids. Water produced from the Navajo in wells that also tap other formations is discussed in the section on the Entrada Sandstone.

Carmel Formation The Carmel Formation has yielded water that ranges from fresh to moderately saline. The dissolved-solids content of water from three water wells in T. 25 S., R. 12 E., and T. 'Z7 S., R. 11 E., ranged from 2,730 to 6,360 ppm (fig. 13 and table 3). The yields of two of the wells were 100 and 580 bwpd (3 and 17 gpm). Chemical analyses of water from three springs in T. 22 S., R. 8 E., T. 24 S., R. 13 E., and T. 28 S., R. 14 E., showed 7,450,437, and 2,390 ppm of dissolved solids. The yield of the springs ranged from 34 to 170 bwpd (1 to 5 gpm). In most areas, however, the Carmel forms an aquiclude above the Navajo Sandstone. An ex­ ample of this is the Blanding Basin, where the water in the Navajo is confined under artesian pressure by the overlying Carmel.

- 26 • Shinarump Member of Chinle Formation

Water has been produced in oil wells, water wells, springs, mines, and test holes from the Shinarump Member of the Chinle Formation (fig. 11). The dissolved-solids content of the water from the several sources were: oil well in T. 24 S., R. 13 E., 5,750 ppm; two water wells in T. 43 S., R. 41/:: W., 646 and 710 ppm, with one well yielding 15,300 bwpd (450 gpm): springs in T. 31 S., R. 14 E., 1.613 ppm; and T. 41 S.. R. 12 E., 840 ppm with the latter spring yielding 100 bwpd (3 gpm): mines in T. 35 S., R. 7 E., 8,510 ppm, and T. 37 S., R. 16 E., 5,840 ppm; and test holes in T. 41 S., R. 12 E., 1,670 and 3,340 ppm (table 3).

Moss Back Member of Chinle Formation

Water from the Moss Back Member in an oil test in T. 27 S., R. 14 E., yielded water con­ taining 4,980 ppm of dissolved solids (fig. 11 and table 3).

Glen Canyon Group

The Glen Canyon Group consists of the Wingate Sandstone, the Kayenta Formation, and the Navajo Sandstone. This widespread sequence of predominantly san.dstone is one of the most important aquifers in the Canyon Lands section because it generally yields fresh water to springs, and in many areas it yields water to wells that is at least suitable for livestock I (fig. 12).

In some wells, the subsurface data available are not detailed enough to identify the aqui­ fer other than as the Glen Canyon Group. Five water wells in T. 40 S., Rs. 21-22 E., yielded water containing from 239 to 403 ppm of dissolved solids at rates of 750 to 3,400 bwpd (22 to 100 gpm) (table 3). A water well in T. 39 S., R. 25 E., yielded water containing 791 ppm of dissolved solids at a rate of 4,320 bwpd (130 gpm). In an oil well in T. 41 S., R. 25 E., the sandstones yield water containing 3,815 ppm of dissolved ~olids. An oil well in T. 16 S., R. 13 E., yielded very saline or briny water at a rate of 1,680 bwpd (50 gpm).

Wingate Sandstone

Four water wells in T. 23 S., R. 21 E .. T. 30 S., R. 24 E., T. 31 S.. R. 23 E., and T. 43 S., R. 24 E., yielded water from the Wingate Sandstone that contained from about 300 to 400 ppm of dissolved solids (fig. 12 and table 3). The yield of two of the wells was 70 and 140 bwpd (2 and 4 gpm). Sixteen springs in the Wingate yielded water containing from 133 to 914 ppm of dissolved solids at rates ranging from 17 to 3,840 bwpd (0.5 to 113 gpm). In T. 26 S., R. 7 E., water from an oil well in the Wingate contained 4,079 ppm of dissolved solids. Water produced from a well that taps the Wingate and also the Entrada and Navajo Sandstones is discussed in the section on the Entrada Sandstone. Recharge to the Wingate is restricted by the overlying relatively impermeable Kayenta Formation. Where fracturing and faulting extend through the Glen Canyon Group, however, water moves downward from the Navajo Sandstone through the Kayenta into the Wingate.

'A~ording to the Western Australia Department of Agriculture (1950), beef cattle and adult sheep will tolerate water containing 10,000 and 12.000 ppm of dissolved solids, respectively.

- 25 - Eight springs in the Morrison Formation in southeastern San Juan County yielded water containing from 216 to 712 ppm of dissolved solids. Seven of the springs yielded less than 10 bwpd (less than 1 gpm), and the other yielded 120 bwpd (3.5 gpm). A spring in Emery County in T. 19 S., R. 10 E., yielded water containing 768 ppm of dissolved solids at a rate of 34 bwpd (1 gpm) . In Grand and San Juan Counties, in T. 22 S., R. 22 E., T. 23 S., R. 22 E., and T. 37 S., R. 21 E., water from three mines in the :YIorrison Formation contained 1,430, 759, and 1,400 ppm of dissolved solids. In T. 39 S., Rs. 24 and 25 E., and T. 40 S., Rs. 23 and 24 E., five water wells in the Bluff Sandstone and Morrison Formation yielded water containing 354, 450, 362, 438, and 2,035 ppm of dissolved solids at known rates of 1,000, 170, 5,100, 5,100, and 370 bwpd (30, 5, 150, 150, and 11 gpm). Two wells in the Morrison Formation, the Dakota Sandstone, and the Burro Can­ yon Formation in T. 33 S., R. 24 E., yielded water containing 292 and 414 ppm of dissolved solids at rates of 750 and 510 bwpd (22 and 15 gpm).

Dakota Sandstone The Dakota Sandstone has yielded fresh to slightly saline water to springs and wells. Four springs in T. 34 S., R. 11 E., T. 39 S., R. 26 ~o (two springs), and T. 41 So, R. 6 E., yielded water containing 199,1,760,1,220, and 186 ppm of dissolved solids (fig. 14 and table 3). The spring in T. 34 S., R. 11 E., flowed 510 bwpd (15 gpm), whereas the other three yielded 34 bwpd (1 gpm) or less. Eight water wells east of Monticello penetrate the Dakota Sandstone and the Burro Can­ yon Formation, and two of the wells were drilled down into the Morrison Formation. For the six wells penetrating the Dakota and Burro Canyon, the dissolved-solids content of the water ranged from 290 to 453 ppm and the yields ranged from 750 to 4,250 bwpd (22 to 125 gpm) 0 The two wells drilled to the Morrison produced water containing 292 and 41-1 ppm of dis­ solved solids at rates of 750 and 510 bwpd (22 and 15 gpm). The Dakota Sandstone is not differentiated from the Cedar Mountain Formation in logs of oil wells along the north edge of the Canyon Lands section. The combined formational unit is reported to contain "salty" or "brackish" water.

Burro Canyon Formation

The BWTO Canyon Formation has yielded fresh to slightly saline water to springs and wells. Six springs in San Juan and Garfield Counties yield water that ranges from 324 to 2,890 ppm of dissolved solids (fig. 14 and table 3) at known rates of 34 bwpd (1 gpm) or less. Water produced from the Burro Canyon Formation in wells that also tap other formations is discussed in the section on the Dakota Sandstone.

Mancos Shale The preponderance of fine-grained sediments and water soluble salts in the Mancos Shale suggests that this formation generally is not a fresh-water aquifer. Water wells in T. 15 S., R. 12 E., and T. 18 S., R. 14 E., yielded water containing 6,280 and 4,710 ppm of dissolved solids (fig. 14 and table 3) 0

- 28 - Entrada Sandstone The Entrada Sandstone has yielded fresh water to water wells in some areas and saline water in others. The sandstone yielded water having 360 to 801 ppm of dissolved solids from six wells in eastern San Juan County; 380 to 3,500 ppm from seven wells in Emery, Kane, and Wayne Counties; and from 9,470 to 14,300 ppm from two wells in Grand County (fig 13 and table 3). Although the Entrada contained saline water in northeastern Grand County, in the Grand Junction area of Colorado water from the sandstone contained from 291 to 1,210 ppm of dissolved solids (Lohman, 1965, p. 115). Data for eight wells indicate that yields from the Entrada Sandstone range from about 85 to 40,000 bwpd (2.5 to 1,200 gpm). Five of these wells are in San Juan County, and their yields average 4,860 bwpd (143 gpm). Chemical analyses of water from nine springs, which issue from the Entrada Sandstone at rates ranging from 17 to 170 bwpd {0.5 to 5 gpm), indicate a range in dissolved solids from about 190 to 740 ppm (fig. 13). Several wells in the Blanding Basin produce water from the Entrada Sandstone and one or more other formations, including the Bluff, Navajo, and Wingate Sandstones. In T. 39 S., R. 26 E., the Navajo and Entrada yielded water containing 1,070 ppm of dissolved solids at a rate of 990 bwpd (29 gpm); but in T. 41 S., R. 23 E., these formations yielded water contain­ ing 6,851 ppm at a rate of 1,070 bwpd (31.5 gpm). In T. 40 S., R. 24 E., and T. 41 S., R. 23 E., wells in the Navajo, Entrada, and Bluff Sandstones yielded water containing 4,526 and 1,735 ppm of dissolved solids; and in T. 41 S., R. 25 E., water from the Entrada, Navajo, and Wingate Sandstones contained 8,640 ppm. In T. 41 S., R. 25 E., a well in the Entrada and Bluff Sandstones yielded water containing 2,180 ppm of dissolved solids at a rate of 34 bwpd (1 gpm).

Bluff Sandstone The Bluff Sandstone in Utah is found only in southern San Juan County. Two wells in T. 40 S., R. 23 E., yielded water containing 1,850 and 7,350 ppm of dissolved solids at rates of 440 to 850 bwpd (13 to 25 gpm) (fig. 13 and table 3). Two springs in the Bluff in T. 40 S., R. 22 E., and T. 41 S., R. 21 E., yield water containing 139 and 241 ppm of dissolved solids, and the latter discharges less than 34 bwpd (1 gpm). Water produced from the Bluff in wells that also tap other formations is discussed in the sections on the Entrada Sandstone and the Morrison Formation.

Morrison Formation 1 In Grand County, water from five wells in the Morrison Formation in Tps. 19-22 S. con­ tained from 2,090 to 25,700 ppm of dissolved solids (fig. 13 and table 3). A sixth well in T. 22 S., R. 22 E., yielded water containing only 517 ppm, and this probably indicates that re­ charge to the formation is at or near the well site. Yields from three of the wells were 70 bwpd (2 gpm) or less. In San Juan County, in T. 36 S., R. 21 E., and T. 40 S., R. 25 E., the Morrison yielded water containing 844 and 1,460 ppm of dissolved solids, the latter at a rate of 70 bwpd (2 gpm).

I II' this discussion, data for wells and springs in all members of the Morrison Formation are treated as a unit. In figure 13 and table 3, however, the specific member is identified when possible.

- 27 - o 0'

-

~,.. j•• 1aI 1IMt , .. ~ I I ) .. f ...... "'..,--",-._,a__USh.. _.1_._.. • u. _ •• """1 NAtal I,C"'. ~ .....,_ ~.__ """".u.I ,_ ~ut Ical leal ...... t ... __1'__ '_U.IU . '--cati..., I_ti.. 0tI lit.,. 11 ,.::.i:=-:..::-..:..... _ i: ,,,,.

Figure 16. - Geologic section 0-0' of port of the High Plateaus section.

• 30 • Ferron Sandstone Member of Mancos Shale Two water samples were collected while drilling an oil well with air through the Ferron Sandstone in T. 14 S., R. 9 E. (fig. 15). Chemical analyses of water showed a dissolved-solids content of 37,860 and 51,950 ppm (table 3). A gas well in T. 20 S., R. 7 E., yielded water containing 21,534 ppm of dissolved solids. The Ferron yielded water containing 3,454 ppm of dissolved solids in a coal mine in T. 22 S., R. 6 E.

Tununk Shale Member of Mancos Shale Two water samples were collected while drilling an oil well with air through the Tununk Shale in T. 14 S., R. 9 E. (fig. 14). Chemical analyses of the water showed a dissolved­ solids content of 11,117 and 12,093 ppm (table 3).

WATER FROM BEDROCK IN THE HIGH PLATEAUS SECTION

The High Plateaus section is divided into three longitudinal strips, each consisting of two to four plateaus that generally are separated by escarpments or valleys. The variations in relief generally are controlled by faults, but a few escarpments were formed solely by ero­ sion. Except where distorted locally along faults, the rocks generally are horizontal or gently dipping, as indicated by the attitude of the tops of the individual plateaus. An exception is along the west edge of the Wasatch Plateau where for 50 miles strata of the Wasatch mono­ cline plunge downward from the top of the plateau into Sanpete Valley. Rocks exposed in the High Plateaus section range from Permian to Tertiary in age, and oil and gas wells have penetrated rocks of Cambrian, Devonian, Mississippian, and Pennsyl­ vanian ages. The rocks include sedimentary and igneous types. Table 1, columns 10, 11, and 12, show the stratigraphic sections for the High Plateaus. Chemical analyses of water from water wells, oil and gas wells, and springs show that· fresh water is in limestones of Paleozoic age, Wingate and Navajo Sandstones, Carmel For­ mation, Tropic Shale, Wahweap and Straight Cliffs Sandstones, Emery Sandstone Member of the Mancos Shale, Blackhawk. Price River, Kaiparowits, and North Horn Fonnations, Flagstaff Limestone, Wasatch, Briar!Head, Green River, and Crazy Hollow Formations, and igneous rocks of Tertiary age. The extent of fresh water in these formations is poorly known because few water wells penetrate bedrock, and oil and gas exploration has not been extensive in most of the section. The electrical logs of oil and gas wells used in constructing figure 16 indicate that water in bedrock in the Wasatch Plateau ranges from fresh to saline in chemical quality. Many communities in the High Plateaus section obtain their water supplies from springs that issue from bedrock. Sedimentary rocks of Tertiary age yield water to most of these springs in the northern part of the Plateaus, and igneous rocks of Tertiary age are the source of most springs in the central part of the High Plateaus. In the southern part of the High Pla­ teaus, limestones of Tertiary age yield water to springs atop the plateaus, but along the es­ carpments sandstones of Mesozoic age are the principal aquifers. The numerous springs that yield large quantities of fresh water in the High Plateaus is a reflection of the great amount of precipitation on this area (fig, 2). Table 4 contains selected hydrogeologic data from springs, water wells, and oil and gas wells in bedrock in the High Plateaus section; locations of the sampling sites are shown in figures 9, 10, 11, 12, 13, 14, 15, 17, and 18. Following is a summary of the data by formation.

- 29 - Moenkopi Formation Water from an oil well in the Moenkopi Formation in the Virgin oil field, T. US., R. 12 W., contained 84,i14 ppm of dissolved solids (fig. 11 and table -1). Water of poor quality is to be expected from the Moenkopi in most areas because the formation contains interbedded evaporite deposits.

Wingate Sandstone A spring in the Wingate Sandstone in T. 28 S., R. -1 E., yielded water containing 440 ppm of dissolved solids at a rate of 34 bwpd (1 gpm) (fig. 12 and table -l).

Wingate Sandstone and Kayenta Formation Water from an oil well in the Navajo Sandstone and the Kayenta Formation in T. 14 S., R. 7 E., contained 41,i16 ppm of dissolved solids (fig. 12 and table 4).

Navajo Sandstone :\1any springs issue from the Navajo Sandstone in the southern High Plateaus. Analyses of water samples from five springs indicate that all of them contained less than 200 ppm of dissolved solids (table 4). In Zion National Park, in T. -U So, R. 10 W. (fig. 12), water-supply systems obtain water from springs in the Navajo that yield as much as 3,000 bwpd (90 gpm). In Kanab Creek, in T. 42 S., R. 6 W., nine springs in the Navajo reportedly yielded from 340 to 13,600 bwpd (10 to 400 gpm) (Goode, 1964, p. 30). • Two watn' wells in the Navajo Sandstone in T. 41 S., R. 9 W., and T. 42 S., R. 7 W., yielded water containing 254 and 220 ppm of dissolved solids and the former yielded 290 bwpd (9 gpm). Four water wells in sees. I, 23, 26, and 35, T. 42 S., R. 5 W., reportedly yielded 8,500, 1,200, 34,000, and 1,500 bwpd (250, 35, 1,000. and -15 gpm) (Goode, 1964, p. cl5). An oil well in the Navajo Sandstone in T. 22 S., R. 1 W., yielded water containing 50,163 ppm of dissolved solids.

Carmel Formation Chemical analyses of water from springs issuing from the Carmel Formation in T. 39 So, R. 10 W., T. -10 So, R. i W., and T. -11 S., R. i W., showed dissolved solids of 1-15, 809, and 1,OU ppm (fig. 13 and table 4). The yields of the three springs were 1,300, 1iO, and iO bwpd (38, 5, and 2 gpm).

Morrison and Cedar Mountain Formations Water from an oU well in the Morrison and Cedar Mountain Formations in T. 22 S., R. -1 E., contained 53,361 ppm of dissolved solids (fig. 13 and table 4).

Winsor Formation and Dakota Sandstone Water from the Winsor Formation and Dakota Sandstone in two oil wells in T. 37 S., Rs. 6 and i W., contained 1,231 and 1,634 ppm of dissolved solids (fig. 13 and table -1).

- 32 - Limestones of Paleozoic age In T. 40 S., R. 13 W., on the west edge of the High Plateaus section, an oil well pro­ duced water from an interval between 410 and 1.440 feet. The well yielded water containing 579 ppm of dissolved solids at a rate of 4.800 bwpd (140 gpm) from limestones of Paleozoic age (fig. 10 and table 4). While still in the limestones, the well reportedly encoW1tered salt water at a depth of 5,000 feet.

Rocks of Mississippian age An oil test in rocks of Mississippian age in T. 36 S., R. 1 E., produced water containing 10,494 ppm of dissolved solids at a rate of 34 bwpd (1 gpm) (fig. 9 and table 4).

Rocks of Mississippian age and Molas Formation An oil well in rocks of Mississippian age and the overlying Molas Formation in T. 32 S., R. 3 E., yielded water containing 12,344 ppm of dissolved solids at a rate of 480 bwpd (14 gpm) (fig. 9 and table 4).

Toroweap Formation Water from an oil wen in the Toroweap Formation in T. 42 S., R. 7 W., contained 19,149 ppm of dissolved solids (fig. 10 and table 4).

Cedar Mesa Sandstone Member of Cutler Formation An oil well in the Cedar Mesa Sandstone Member in T. 36 S., R. 1 E., yielded water con­ taining 4,752 ppm of dissolved solids at a rate of 100 bwpd (3 gpm) (fig. 10 and table 4).

Coconino Sandstone Two oil wells in the Coconino Sandstone in T. 36 S., R. 1 E., yielded water containing 10,630 and 9,869 ppm of dissolved solids; the latter at a rate of 100 bwpd (3 gpm) (fig. 10 and table 4).

Kaibab Limestone Water from four oil wells in the Kaibab Limestone in T. 31 S.. R. 2 W., T. 35 S., R. 2 W., and T. 36 S., R. 1 E. (two wells), contained 2,593. 3,992, 11,375, and 11,800 ppm of dissolved solids (fig. 10 and table 4). LaVerkin Hot Springs in T. 41 S.. R. 13 W.. yielded water con­ taining 9,390 ppm of dissolved solids at a rate of 162,000 bwpd (about 4,760 gpm) in August 1960.

Shinarump Member of Chinle Formation A spring in the Shinarump Member in T. 28 S., R. 5 E., yielded water containing 1,530 ppm of dissolved solids (fig. 11 and table 4) at a rate of les~ than 34 bwpd (1 gpm). An oil well in the Shinarump in T. 35 S., R. 2 W., yielded water containing 9,140 ppm of dissolved solids at a rate of 206 bwpd (6 gpm).

- 31 - Emery Sandstone Member of Mancos Shale Fresh to slightly saline water has been produced from three gas wells in the Emery Sand­ stone Member (fig. H). In T. 14 S.. R. ;) E., one of the gas wells was converted to an irriga­ tion well, and water containing -*21 ppm of dissolved solids flowed at a rate of 20,000 bwpd (600 gpm) (table 4). In T. 16 S.. R. 5 E., and T. 22 S., R. ~ E.. other gas wells yielded water containing 1,304 and 1.793 ppm of dissolved solids. The latter well was open to the lower por- tion of the overlying Masuk Shale Member of Mancos Shale. . Although the Emery Sandstone ?v1ember does not crop out atop the Wasatch Plateau. water from precipitation and runoff on the plateau apparently reaches the formation through the system of faults that traverse the plateau (Spieker, 1949. p. ~4, and Stokes, 1964).

Star Point Sandstone and Blackhawk Formation In T. 22 S., R. 4 E .• a gas well in the Star Point Sandstone and Blackhawk Formation yield­ ed water containing 2,384 ppm of dissolved solids (fig. 17 and table 4). These formations may contain fresh to slightly saline water in other parts of the Wasatch Plateau. particularly in or just downdip from their areas of outcrop. (See section on Blackhawk Formation.)

Blackhawk Formation A gas well in the Blackhawk Formation in T. 22 S., R. 2 E .. yielded water containing 245 ppm of dissolved solids (fig. 17 and table 4). The gas well was converted to a water well that flowed water at a rate of 23.000 bwpd (675 gpm). A coal mine in the formation in T. 22 S.• R. 3 E .• yielded water containing 903 ppm of dissolved solids at a rate of 54,000 bwpd (1,600 gpm). The Blackhawk probably contains fresh or slightly saline water in other parts of the Wasatch and Sevier Plateaus. The most likely of such areas would be where outcroppings are recharged directly by precipitation or runoff, or where faults (Spieker. 1949. p. 44, and Stokes, 1964) permit movement of water to the formation where it does not crop out.

Price River Formation The Price River Formation has yielded fresh water to many springs on the Wasatch Pla­ teau. In Tps. 11 and 12 S., R. 7 E., Cordova (1963, p. 21) reports seven springs that yield water ranging in dissolved solids from 238 to 303 ppm at rates of 17 to 850 bwpd (0.5 to 25 gpm). Data for one of these springs in T. 11 S., R. 7 E., is given in table·t and the loca­ tion is shown in figure 17. A water well in sec. 22, T. 11 S.. R. 8 E.. was drilled 278 feet into the Price River at a total depth of 2.103 feet. but no aquifers were encountered in the Price River. The formation may contain fresh water in the Wasatch Plateau because the for­ mation includes many sandstone beds that crop out where they could receive recharge from precipitation and streamflow.

Kaiparowits Formation Chemical analyses of water from seven springs in the Kaiparowits Formation in Tps. 37-39 S., Rs. 4-7 W.• in western Garfield and Kane Counties showed a range in dissolved solids from 223 to 462 ppm (fig. 17 and table 4). The yields from these springs :.-anged from 340 to 10,000 bwpd (10 to 300 gpm). Many springs probably issue from the formation elsewhere in the High Plateaus.

- 34 - Dakota Sandstone

Water from two gas wells in the Dakota Sandstone in T. 16 S., Rs. 5 and 7 E., con­ tained 3,669 and 5,474 ppm of dissolved solids, but in two gas wells in T. 15 S., R. 3 E., and T. 22 S., R. 4 E., the dissolved solids were 47,751 and 69,909 ppm (fig. 14 and table 4).

Tropic Shale

An oil well in the Tropic Shale in T. 37 S., R. 6 W., yielded water containing 1,530 ppm of dissolved solids (fig. 17 and table 4). In T. 40 S., Rs. 5 and 6 W., two springs in the Tropic yielded water containing 420 and 527 ppm of dissolved solids, both at a rate of about 100 bwpd (3 gpm).

Ferron Sandstone Member of Mancos Shale

Chemical analyses of water from 22 oil and gas wells in the Ferron Sandstone Member in the High Plateaus seetion show a range in dissolved solids from 63 to 25,931 ppm (fig. 15 and table 4). The extremely fresh water from several of the gas wells was water that condensed during gas production. In wells in which formation water was produced together with gas, the formation water was generally diluted by water of condensation. Undiluted formation water in the Ferron Sandstone in Tps. 13-16 S., Rs. 6-7 W., generally contains from 4,000 to 6,000 ppm of dissolved solids. The water yield of the producing gas wells in the Wasatch Plateau was generally less than 1 gpm. East of the plateau, however, the gas well in T. 11 S., R. 7 E., yielded water" at a rate of 2,000 bwpd (60 gpm), and wells in sees. 23 and 34, T. 22 S., R. 5 E., flowed water at rates of 710 and 2,600 bwpd (21 and 75 gpm).

Straight Cliffs and Wahweop Sandstones A water well in T. 37 S., R. -1 W., in Bryce Canyon National Park yielded water contain­ ing 260, 315, and 870 ppm of dissolved solids from the Straight Cliffs and Wahweap Sandstones during three phases of perforating and developing the well (table 4 and fig. 17). Final comple­ tion of the well was in the Straight Cliffs, Wahweap, and the Wasatch Formation, and the well yielded 7,000 bwpd (200 gpm). Springs in the sandstones in T. 36 S., R. 3 W., and T. 37 S., R. 4 W., yielded water con­ taining 227 and 815 ppm of dissolved solids at rates of 580 and 1,630 bwpd (17 and 48 gpm). Many additional springs probably discharge from the sandstones elsewhere in the High Plateaus.

Wahweap Sandstone Nine springs in the Wahweap Sandstone in Tps. 39 and 40 S., Rs. 5-7 W., yielded water containing from 145 to 690 ppm of dissolved solids at rates ranging from less than 34 to about 17,000 bwpd (less than 1 to about 500 gpm) (Goode, 1964, p. 48). Data for two of these springs in T. 39 S., R. 6 Woo and T. 40 S.. R. 7 W., are given in table 4 and their locations are sh'W!1 in figure 17. Many additional springs probably discharge from the sandstone elsewhere in the High Plateaus.

- 33 - Wasatch Formation The Wasatch Formation in the southern part of the High Plateaus section generally yields water to wells or springs from conglomerate or limestone units. Water collected from con­ glomerate while drilling a well through the formation in T. 37 S., R. 4 W., contained 252 ppm of dissolved solids (fig. 18 and table 4). Water from springs in the limestone generally issues from solution channels. Five springs in the eastern parts of Garfield and Kane Counties ranged in yield from less than 34 bwpd (less than 1 gpm) to as much as 4,110,000 bwpd ~12l,000 gpm) , and the dissolved solids in the water ranged from 103 to 287 ppm.

Wasatch and Brian Head Formations Two springs in the Wasatch and Brian Head Formations in T. 32 S., R. 2 W., yielded water containing 255 and 318 ppm of dissolved solids at rates of 15,300 and 55,800 bwpd (450 and 1,640 gpm) (fig. 18 and table 4).

Green River Formation Along the western base of the Wasatch Plateau, \vells and springs yield water from the Green River Formation. The water from two springs in T. 19 S., R. 2 E.; contained -429 and 598 ppm of dissolved solids (fig. 18 and table 4), and the yield of one of the springs was 3,400 bwpd (100 gpm). In Sanpete Valley, several wells have been drilled into the Green River Formation and in the SE1I.l,S~/4SE% sec. 36, T. 17 S., R. 2 E., a well reportedly was pumped at 154,000 bwpd (4,500 gptn) (Marsell. 1958, p. 30). Another well in T. 17 S., R. 2 E. (fig. 18), yielded water containing 375 ppm of dissolved solids at a flow rate of 2,550 bwpd (75 gpm).

Crazy Hollow Formation The Crazy Hollow Formation contains sandstone beds that are potential aquifers in the central and northern High Plateaus section. In T. 16 S., R. 3 E. (fig. 18), a well yields water from this formation (Marsell, 1958, p. 30) containing 894 ppm of dissolved solids at a rate of 30,900 bwpd (910 gpm) (table 4). A spring in the formation in T. 23 S., R. 3 W., yielded water having 310 ppm of dissolved solids at a rate of 47,600 bwpd (1,400 gpm).

Igneous rpcks of Tertiary age Many springs discharge from the igneous rocks that cover much of the central High Plateaus section, and the water is generally fresh (fig. 18). Records for 18 springs indicate a range in dissolved solids from 84 to 235 ppm and a range in yield from 340 to 153,000 bwpd (10 to 4,500 gpm) (table 4). Two hot springs in T. 25 S., Rs. 3 and 4 W., yielded water containing 2,700 and 5,150 ppm of dissolved solids at rates of 1,400 and 3,400 bwpd (40 and 100 gpm). Two water wells in T. 'ZT S., R. 3 E., and T. 26 S., R. 4 W., yielded water containing 1,760 and 1,790 ppm of dissolved solids, the latter at a rate of 850 bwpd (25 gpm). A test hole in T. 31 S., R. 2 W., yielded fresh or slightly saline water, and it flowed at a rate of 1,400 bwpd (40 gpm). Two mine tunnels in T. 'Z7 S., R. 5 W., yielded water containing 150 and 207 ppm of dissolved solids at rates of 3,400 and 13,600 bwpd (100 and 400 gpm).

- 36 • North Horn Formation

A water well in the North Horn Formation in T. 11 S., R. 8 E., yielded water containing 310 ppm of dissolved solids (figs. 17 and 18 and table 4). The well flowed at a rate of 9,200 bwpd (270 gpm) and was pumped at a rate of 54,000 bwpd (1,600 gpm) (Cordova, 1963, p. 15).

A water well in T. 14 S., R. 4 E.. yielded water containing 344 ppm of dissolved solids at rates of 1,700 bwpd (50 gpm) flowing or 24,000 bwpd (700 gpm) pumped. The well is re­ portedly completed in sandstone in the North Horn Formation (Marsell, 1958, p. 30).

In T. 20 S., R. 2 W., an irrigation well drilled into sandstone in the North Horn Forma­ tion yielded water containing 238 ppm of dissolved solids. In February 1957 the well flowed at a rate of 48,000 bwpd (1,400 gpm), but in June 1963 the rate was 10,000 bwpd (290 gpm).

Five springs in T. 11 S., Rs. 7 and 8 E., and T. 12 S., R. 8 E., yielded water containing from 256 to 562 ppm of dissolved solids (Cordova, 1963. p. 21). Two of the springs ;yielded 100 and 680 bwpd (3 and 20 gpm). Data for one of the springs in T. 11 S., R. 7 E., is given in table 4.

Along the western edge of the Wasatch Plateau, two springs in T. 17 S., R. 4 E., and T. 18 S., R. 4 E., yielded water containing 225 and 363 ppm of dissolved solids, the former at a rate of 61,000 bwpd (1,800 gpm).

Flagstaff Limestone

The Flagstaff Limestone has yielded water to many springs in the Wasatch Plateau in­ cluding the Colton Spring' in T. 11 S., R. 8 E., (fig. 18). This spring yielded water containing 209 ppm of dissolved solids and is part of a large spring area that has yielded as much as 690 million gallons per year (average rate of about 1,300 gpm, or 45,000 bwpd) (Cordova, 1963, p. 15). Eight other springs were also reported by Cordova (1963. p. 21) in Tps. 11 and 12 S., R. 8 E. They yielded water containing from 290 to 428 ppm of dissolved solids. Four of the springs yielded from 17 to 170 bwpd (0.5 to 5 gpm). Data for one of these springs in T. 12 S., R. 8 E., is given in table 4.

A water well in the NE%SWl.~NW1;~ sec. 22, T. 11 S., R. 8 E., penetrated an aquifer in the middle of the Flagstaff Limestone; however, another well in the NW~-tSWl.. SEl... sec. 22, T. 11 S., R. 8 E., did not encounter any water (Cordova, 1963, p. 13). This indicates that the water moves through solution channels that may not be connected. Although the water en­ countered in the first well was not sampled or tested, the quality of the water should be similar to that of Colton Spring.

In T. 18 S.. R. 1 E., the Fayette Spring yields water containing 553 ppm of dissolved solids at a rate of 65,000 bwpd (1,900 gpm). The spring issues from solution channels in lime­ stone.

'Although Colton Spring discharges from the Colton Formation, the water probably has risen to the surface along a regional fault from the underlying Flagstaff Limestone.

- 35 - of the aquifers. The formations that are known to contain fresh water in the High Plateaus section include limestones of Paleozoic age, Wingate and Navajo Sandstones, Carmel Forma­ tion, Tropic Shale. Wahweap and Straight Cliffs Sandstones, Emery Sandstone Member of the Mancos Shale, Blackhawk, Price River, Kaiparowits. and North Horn Formations. Flagstaff Limestone, Wasatch, Brian Head, Green River. and Crazy Hollow Formations, and igneous rocks of Tertiary age. Because of the scarcity of available data. this report includes only a general description of the occurrence of water in the bedrock formations of the Colorado Plateau. Chemical analyses of water from many formations are few or nonexistent; and water-yield information from most oil or gas wells is often nonexistent, and where existent it is generally an esti­ mate. This is unfortunate, because many water data could have been obtained during routine drill-stem and production tests on oil and gas wells. Every available source of information must be used in order to gain an understanding of the hydrology of an area as vast as the Colorado Plateau. It is recommended, therefore, that a program be established wherein all tests in oil and gas wells will be conducted so as to furnish a water sample and data on water yield, water pressure, and water levels.

• 38 • CONCLUSIONS AND RECOMMENDATIONS

Water in the bedrock of the Colorado Plateau province in Utah ranges widely in quality and quantity because of many variations in the geology, physiography, and climate in the province. Development of ground water generally has been restricted to local stock, domestic, or municipal supplies; and a systematic effort has not been made to determine which forma­ tions contain fresh water and to delineate the extent of the water. Much of the available data only indicates what the ground-water conditions are in a specific locality, and care should be used when extrapolating such information to other areas. The Colorado Plateau in Utah is divided into three sections-the Uinta Basin, Canyon Lands, and the High Plateaus. In the Uinta Basin, the area of greatest potential for develop­ ment of fresh or slightly saline water is along the north flank where surface water from the Uinta Mountains and local precipitation is available to recharge bedrock aquifers. The Du­ chesne River Formation yields fresh water to wells for domestic and municipal supplies, and the Weber Sandstone yields water from oil wells that is suitable for irrigation. Other formations such as the Navajo, Entrada, and Dakota Sandstones and the Frontier Sand­ stone Member of the Mancos Shale probably contain fresh or slightly saline water along the north flank of the basin. Fresh water has been found at considerable depths in the Weber Sandstone and the Green P.iver Formation on the north flank of the basin, and these forma­ tions may be recharged by interformational leakage. On the south flank of the Uinta Basin. water for livestock is produced from oil and gas wells in the Green River Formation. This water source merits future study in light of water needs in oil l;xtraction from oil shale and bituminous sand. The Canyon Lands section is divided into numerous hydrologic units by structural ele­ ments such as the San Rafael Swell, Circle Cliffs and Monumellt Upwarps, the Abajo, Henry, and La Sal Mountains, and other subsidiary structures. The deeply incised drainage system in some areas drains the exposed bedrock and the aquifers are partially void of water. In several structural basins. northeast of the Henry Mountains and east of the Abajo Mountains and Comb Ridge, the aquifers contain water under artesian pressure and wells flow at the land surface. In the Canyon Lands section, sandstones of the Glen Canyon Group are the most widely tapped fresh-water aquifers. They underlie much of the area, and in most places they can be relied upon to yield fresh water. Other formations that locally yield fresh water are in the Hermosa Group and the Rico. Cutler. Chinle. and Carmel Formations. Entrada and Bluff Sandstones. Morrison and Burro Canyon Formations. and Dakota Sandstone. However, these formations and the sandstones of the Glen Canyon Group contain saline water in some localities. Many parts of the Canyon Lands section have not been adequately explored for water sup­ plies because of the remoteness of the area and the cost of drilling. Fresh or slightly saline water probably occurs along the flanks of high areas such as the La Sal, Henry, and Abajo Mountains where runoff and precipitation recharges permeable formatiOns. The High Plateaus section receives the greatest precipitation in the Colorado Plateau of Utah and more than 16 inches a year falls on most of the section. This provides for abundant recharge by direct infiltration to bedrock aquifers and by infiltration from perenniafstreams that flow into the Canyon Lands section. However. very little water is withdrawn from the aquifers in the High Plateaus in relation to the amount of recharge and the potential yield

- 37 - 'icard, :\'1. D., 1957, Green River and lower Uinta formations-subsurface and stratigraphic changes in central and eastern uinta Basin, in Guidebook to the geology of the Uinta Basin: Guidebook, Eighth Annual Field Conference, Intermountain Assoc. Petroleum Ge­ ologists, p. 116-130. {obinove, C. J., Langford, R. H., and Brookhart, J. W., 1958, Saline-water resources of North Dakota: U. S. GeeL Survey Water-Supply Paper 1428. Spieker, E. M., 1949, The transition between the Colorado Plateaus and the Great Basin in central Utah: Utah Geol. Soc. Guidebook to the geolo~ of Utah, No.4. Stokes, W. L., 1964, Geologic map of Utah: Utah Univ. Thomas, H. E., 1952, Hydrologic ~onnaissance of the Green River in Utah and Colorado: U.S. GeeL Survey eire. 129. Western Australia Department of Agriculture, 1950, Waters for agricultural purposes in west· ern Australia: Perth, Western Australia., Western Australia Jour. Agriculture, v. TI, ser. 2, p. 156.

- 40 • SELECTED REFERENCES Cooley, M. E., 1965, Stratigraphic sections and records of springs in the Glen Canyon re­ gion of Utah and Arizona: Museum of Northern Arizona Tech. Ser. 6. Connor, J. G., Mitchell, C. G., and others, 1958, A compilation of chemical quality data for ground and surface waters in Utah: Utah State Engineer Tech. Pub. 10. Cordova, R. M., 1963. Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah: Utah Geol. and Mineralog. Survey Water-Resources Bull. 4. Goode, H. D., 1958, The geology and distribution of aquifers in the southeastern part of San Juan COW1ty, Utah: U.S. Geel. Survey open-file rept. .... __ 1964, Reconnaissance of water resources of a part of western Kane COW1ty, Utah: Utah Geol. and Mineralog. Survey Water-Resources Bull. 5, p. 60-61. Goode, H. D. and Feltis, R. D., 1962. Water production from oil wells of the Uinta Basin, Uintah and Duchesne Counties, Utah: Utah Geol. and Mineralog. Survey Water-Resources Bull. 1. Gregory, H. E., 1916, The Navajo country-a geologic and hydrologic reconnaissance of parts of Arizona, New Mexico, and Utah: U.S. Geol. Survey Water-Supply Paper 380. Hunt, C. B., 1956, Cenozoic geology of the Colorado Plateau: U.S. Geol. Survey Prof. Paper 279. Johnson, C. E., 1964, Ashley Valley oil field, Uintah County, Utah: Guidebook, Thirteenth An­ nual Field Conference, Intermountain Assoc. Petroleum Geologists, p. 187-189. Kinney, D. M., 1955, Geology of the Uinta River-Brush Creek area, Duchesne and Uintah Counties, Utah: U.S. Geol. Survey Bull. 1007. • Lofgren, B. E., 1954, Ground-water possibilities of bedrock aquifers in southeastern Utah in Progress report on selected ground-water basins in Utah: Utah State Engineer Tech. Pub. 9. Lohman, S. W., 1965, Geology and artesian water supply, Grand Junction area, Colorado: U.S. Geel. Survey Prof. Paper 451. Marine, 1. W., 1962, Water-supply possibilities at Capitol Reef National Monument, Utah: U.S. Geol. Survey Water-Supply Paper 1475-G. .__ ._ -.1963, Ground-water resources of the Bryce Canyon National Park area, Utah: U.S. Geel. Survey W~ter-Supply Paper 1475-M, Marsell, R. E., 1958, Potential ground-water resources of Sanpete Valley, Utah, in Utah Water and Power Board 6th Bienn. Rept. . 1964, Ground water in bedrock in Utah, in Utah Water and Power Board 9th Bienn. Rept. Peterson, V. E., 1957, The Ashley Valley oil field, in Guidebook to the geology of the Uinta Basin: Guidebook, Bight .-\nnual Field Conference, IntermoW1tain Assoc. Petroleum Geolo­ gists, p. 191-192.

- 39 - Table 1. Correlation chart of bedro4 (See fig. 12 fo

E.utsrn .and. .:en(,r..1 UintA 300ll CHffs .1C ~c ..n lLv,r:. Soak Cliffs I.e :Jc.an.-C.,)lorado 3.ui.n ;';CUl it.ace :.I,.tw (1) (2) (1) ~) 51

Mancos Shale Xaac:os Shale :'ronci.er ;.lnd.tone ~_o.r Mov'l"Y Shale

Dakota :i.&ndlcone 111akoca · ... ndsc·,)o. Coldac ~nuru:... ~n :':C":'"..a::'JO 3uci(:torn ·':.;n·(L:l!'.l!!r::l"~ :iorriJlon :,Jt'1a&cl,.on

JI,l('&Ssi.c

Curti, lormatton Cuc:.i,s i'-'~""Cl.:)n

~-" ... ,... ::... _...... ("._. ':., ...... ~ •."'~g.c 5<1l1d.c~n. t;- H..".1. 0 i ..ndllCOne r;1-"::;~::.:::.::.o;;::...:.;",:n::;J~::s",:::::n::::'-n---! ~~ ::~:, l;:::C:~' ~ !tJ,v.nc~ J • 5r .. .:.J :: :'JC"::1aci,.:n iO Illnl.J.ce 5...ndl~on. j -,3 ;;(r.~u i.andsc;;:Ine .!:3 \lLn~c. S.and.Cone ;,; "" -:.:

Ct1Ah Formation. Ch1a.le ForaaClOl\ Clin.l. F~C"lll&Ci.on Chinle Fonaac1.on Shi.n&~ ~_"r' ihinaC'\lZll9 H..u,4IC' ~o.. l.ck ~...o.C' I:iO.. a.t.ck ~a.C' :iO.okGOi. :~maci.:ln l'toenko,i. :~:n""c1on ij.r.o..d :'~::::':lcon. ~U\o.c i1~o.d !.:.:neaccne :-!cmo., Cue ter: :omac10ft .1\i.CI :U=a S... nulI(.>ne ~elfto.

:l1c.a Formac10n

1 ,~. ~...... !"&c&dox F"r:n&cion I j tftll&y i.:.)ne IPsnnsv banun ~_ ')••• 1': ':1'1." !,j~e I • \k.ln :,.:n. i ;1 ?'"K

t.1&dvit~1 l..i=esc,:nl ~d1son t..uaet con.. ~(h.son LL::".•sccnl vu:J.y :'~":~ISC:lne JavonLan Et:::eC'C :.,~Cl;...:n ~cCt'"ek.:"l :'!ntoer .~._":'*-::'\ :';:-:r.ac:..)n i ~ ~\,;:':'.1n ':raov1ci.an wdor. F'onu.e1.on. t'1'\cn "'t..'ft\i.ta tomc.n OaLo.i.et :'1.&xiJ... iJ :'i.~• .,::;lr.e lJoi'ti.r :ot'!Mtl.oJn • L:'\c!.:: . \,I.oF.C:::L~. T LncLc OuarczUa fJ1nea :iounc&i..n GC'oup UintA Maua.ea1n Groul'

- 42 • • 41 - Table 2. - Selected hydrogeologic data from springs, water well

we_cion: .s.le: ~ ~ ... .&net ~.r1.d1.an. :iourc:e: J, ai )r ~ .,aU; 5. J~C'i.C.C;: '..I, ·".Car 'oiaU. a~l:'acor ,Jr -,vnar: ~.&mi& J[ Jr;JaracQr JC' )'Wftar ole cUMi .,.car s.amr;Jh ""•• ';.:lllaccact tor cheaut.al Ulalysis. :'rodu.cinc t:H'Illatioa: :m., !Or.u.Cl.:Hl; Ce.. Crou~; ~ •• Li.:\.Jcona; ~br .• ~elII:a.r; ih., Shale; .i •. , S.&l\dscon. :t.any tOC"llloac1.on n.-. -",ara :'.~r't:.d. ~Cl recorda .)t .:l1.1 uu1 IU :::ma1Jani•• 4.Q4 it.ate "nd. Faderal J.~.ftC~" jo l'\OC :1..c....rily .. cr•• ·.t1.C~ :ha ~.:l.nt:l.tic.ac:''Jn.

?J.t'tl ;Jet'

~A ... K o'-", . ~.. or i.'~dW:inlJ ~ J ~ , ­ , c_ ·=, , , ~ , (\l,D(Mr !ormacion .. ;:2 · ~ t.2E, _ . " .0, !. ;~ ....~ ~"; ..: · SGccioa ·

S 0 Carur au "'...cd, Fa. !. • .36O 5,980 4.658.. 90 os, s- ·j6 ta La 1.742 t,' c•• 4.957-16 OST 5- ·56 9 L5 Sll III 34 r.l .... '.I. i5rava Cuch••a& liver i •• nov .e,·ji 7.0 14 t4 S9 till. 1..ucks N4IvaJQ 5.. .L..::Q.2. do )\ a 4.0 '-O(E) ~I c ~4:!N.lt: 20 0 S e&A4&l'd. 01.1 Cuea iUver FlII. ",030 4,:'1.24til'-4} 'J Co. ot c;;~~;o:~. lw1/ Sl\$WtIfEt a 0 do 6,620 IO,8?8 9,OJ9- os, u- '-6J Ll ).396 Co. i.U7 10.JJ4. OS! t4 l,n7 l, 10.4'3

tS do 6,040 to,19O 9 o n,· Or.1,.n 1,1'. $- 4-00 lJ to 3,610 :"7_, LO,19O l.nco • lap" Clrst1.'" pond LS ;:,1)./ C SW1:1fE\: ., a do do 7 ,~9' 12..082 10,209­ JST L: 10· -;1) 3,)12 ~. 10.1'7 SW'~4::SWJ,; Zl 'J 11.. :1OVar ~O·dlO LS zyll l.~~) nO'- to- 0-04 t8 LJ

LS y,dl :

LS ~I st. Uinta Fs. 1....!.Q2. Fro. L~- 10-10·.j4 ;6 .3.6 110.02 so 2J 5.0 )u(E) lUt••u • :aU in- sllct.n l,.ll 1fE\1I£\:SE' t5 W K. "a mock S.. rllJl to· 0..64 ;6 7.S !.J 2." L5 206 ~""rw.s 1 lS tll1 :l!\1I£\1I£t a " Cley,1 do S... do 1. 6-;a 58 U ).l LO Roo.ev.lt It...rks lS S,,"-I Nt\:SII.\:SEt t9 0 Scan"." au l,1l7 9.698 i . .J

, .lJ3-6J OS, 2 LZ- ·61 LJ.U7 4. I,'-'-Z-IZ OS! t2:- ·61, S,7)9 l.

, .342.·52 OS. Ll to,080

051' 7 to

:, J60

lS a¢.1 SV' L9 'I f't'uitl~ct. U14ca f:ll. 1-53 7.i t6 l.550 Sc.,ac:10(\ I ,.,,1.1 C s£!;St' tJ o C.ac~U· OtL l.O" 7 ,130 3,181­ os LZ ~o. ).569 5,371­ DS l6 L6 ::',237 5,;)6

,-,,1/ .tt5l/\1I£. L5 C"aCiaenc&l do ~,:'62 2,170· :Ore car 3· _."JZ 01.1 co). ),3'0 ulIl.h ,.,,1.1 'lEl:S\I\1I£' t7 0 do do 2..ItZ6 2,{.,38· 1J••b I:ank 1';- '-62 11 l',90d 3,j82 b ,.,,1.1 S'lSII\:tIII.\: t7 0 do 2..~2 3.196- s &i. 'uc }-ll.. 61 (4) LJ ,976 lollO 2,41,0· i.. S

4S r.Jd1 SII.\: Sr::1ll.k:1A1J do .;eO .0 .0 3.110 SpC1r.1 mE" 55 5~/ ~[t t , Indian C.utyOQ do 6,300 U.5 :'2,0 200(£) IS ,.,#1 S£~ t2 1 do 1, iOO 11 Dl 2:'(;)

- 44 • ormations of the Colorado Plateau of Utah cation of numbered areas.)

::ienry ~oun cain. ;(aiparow!c. Plat.au '.I••carn ~••ad loiuhll'l.l(COn ;,;....ccn Pl.ac••u Count:.•• (9) (9) (l0) (1J) (12)

Br1.at1 H••d Fot"lMcion eratV !i.ollO\o' FOr':Utton Gr••n ~lv.r FOrmAc1.o1'1

W••• tc:~ ronut1on Colton For:.acion

~:)rth !ior:'! tOt"'::Ultion K.a10arowi'::s FOnMcion Ul.."Ulc::rvits ::)n:lati::J~ lK

..., Blackhawk Fot"m.ltior. ScraLgnc CliHs Sand.cona Seca1pu: Cliffs S.nd..c.ona Strai.ght Cliif. S.nd.c.onc ~ 5 t.ar :'-01.1'1: Sands :::>na ~co. :0' Shale trop le .ihal. Si'l&h ,WI. Shale ~_b.r M.a,uk Sh.lc H_ber It:-' 5&Q.d. cone ~b.r £aery Shah :1..ber .e Gate Shale ~lIIo.r I!l~ G.&ce Shah Memo.:­ ":01"1. Sandstone Memo.r Ferron S~d.ton. HeaDer 'unil Shah Member Tununk Shale MC1ll:b-r

jO.akoc.a S.nd.tone "'I Kota nd ~n. Cedior ~ount.al,.:1 lOr.:l.lc:'on I :;UCk:lOr~ Cons;lom4:r&ce

· ....0':', rom.acion ~orrison FOr'!'Mcion !"lorC'1.son ionn.ac1.on fJi.n.or Fo~tl.on Formacion !'l.orr1.lon Formati.on -'ru..nv .a..Ul. Shoale Mftl,oer I ;';e.t'W~cer C.aa.yon 5..andacon4: Kamber 1"'·'°' itac:.a.pcure Shal4: Hcmoer I Sal: ''''.aah S.andS'tone :ietnbe= I I aluft 3..ndstone Sl.dlMrvilh iOCTllaC1.on SUfl"llM:t"V1Ue Formacion I Curcis FOt'"!ll.lC10n ad.a So1ndscone ! ::~C!'2:d.l ::.lInast:=ne En::':'"2.da Sandscone ::;::-.c:,.ao.a S.anos::cne I ::11::=.aO& S.ndscone el :on'll4lt:'''n Carmel Formati-on C.x"mal :o~.ci.:Jn C.anMl ror.Il.IClon I C.arnlel tont&c1..:In

Nevalc Sandscone E~ f-::-".-y..:•.:.nt;.•..:.:-;;;.o"",,:';";':;,,":,;;'n---I

~ (.;I i,11npu Sandstone " ie FOn'l.4[lon Ch1nl4: Formation Ch1.nh Formatton Ch1.n14: tormatloa Chi.nle F~nn&tiOt:l. Chinle Fonut.1on ,.r\ll":lp :iamOlir Sbl.ftana, X_ber Mo •• aack li-eer ShinarWlrp Mambu Sh1nar\D~ !ieaoer Sh1naJ:'Ulal' M«mb4:r I Shinar\.llftt) M..mb_= ";:001 FOl"!:l..c1.o:t H04:nkopi. i'ormacion 1 MOenk0'P1. FoftU.t.1.on H04Inkopi. Fonu.t1on MCM:nkopi FO:"ll\&C1.on Moenkopi. Formati.on T:Jn~1! ~eftlo.= ~e!!lber Jild :'i1rIesc:::Jn4: Memb4:r Timoowea, Memo.r ! noskinnirn -:im1)oweap I Sinead !.1,.mestone K.i.10.&0 :"1.lnes cone K.a1.oeo timest::ln. I io:.Ii.:'ab t1.lnesr.Qn.

Coconlno Sana.conll !Cocon1.no S.andscone ICocon1.no S.ndstone nU'llit Shale Cu.c.l...: Fonnation "Per::l1..aa carDonac." Orpn Rock Tont\.le C.dar !1eu S.andlCone :'1.amoer

SUO.al Fonn.::i:::n !\i.co Fonucion I 51,,10a1. :-:Jnucion C.ll~l.... ille :":.t.-.escone C.. l LviiI. l.ioestone C·''-''~'~''''-,"..c'iL'...'--,-,',,-,,,,,,..;La•...'02'"-"_., iiannas. Group §- Honaker !ull :-:J'ntACl en rocks :ie nIlOS" Gr.:luP Jradox :-:Jr.:ation E. Paradox Form.non ~ Ism.ay Zon. O•••rt Cr.ek Zone Auh Zon.

:~r.natl,.or. ~o LIS Fonn.atlOn 1 ~l.an",1.l".~ "=<1n":cl". Sh.ale :-:'lrl10Uq :::l!;!!l"::'~o~ Jest:ec :i.-:loI!sC:ln. R.dw.. ll t.iJne.cone Leadville Li.lDeu:on. Ree:tv.ll LUte.tone R_dwan :'i.1neilcone :-LJ.di.on LJ.mescona

Sedllllenr..r;.· t'"OCk' £lberc Fo~Cion :::l.:14:rc rOrnL&cion ~cCracK..n ~eftlb.t'"

lin car)' roek. '..vntn ~ol~i.tt ~.xf1.ald :':..;nuton. uonu' rOnl.atl,.on ~:'~:l.C Vu.l.c':Zl..:e

. 43 . Tobie 2. Continued

,.. t.ocaC1QQ a~r&COr ?-roctw;i.nl or OVIMIC' fOC'lll.ac1oa. ~, . ..,­- "..­, C Q. , , " 0 SecciOQ '"

'is owl/ C 3£.dW.t J.S 0 R~L. OU Q :.,~&{) J.~90­ ost ) 12 J,919 5• .t.nd a..i1AiJ!1 ). ZSO Co. 15 t.:Jl1 N,tR:\:ll£l: 1 0 Cull Oil c.,("P do I) 4,:)79 it,l13­ .27 ~42 10.6&J :...)45 lS a,-I C ll\I"'w~ 1 0 Cuur Ot.l do S,78' 9.JS7-H '!r••ceC' :".J62 Co. , ..~Le 2S 22£ tR:l: n 5 bel1U' 9..aIlc.h :.6 ,)00 nov ') .02 2.J 1.J 1.J50(E) )S Ii! KE~-t:s!-t lS 'J Sur••u. of l •.5i'5-H do 10 L9 l..lncl ~a••­ 1,.575- :.. iQO <0 7\ 19 ""nc 2,.552 t40(R) 1..5i5- do L2-ll-51 11 ;8 2; 2.552

]5 2U SW4::SI\::SU:)O 'J Uinc.&il--6eJl.! do A.t 2.560 6,'100(E) do 10- ;-53 \l 10 2& '.0 ~ at.! CG. HO ~ 2U SJr$W-tsw~ t6 a ConUuftu! 1,8"'" ;,;20 1,852­ J- J-ll 10 au Co. ;,600 Weber Sa. 1,1560 7.367. :)ST ] 2& 120 1.960 .5 Z)£ ll\I~ 2S National Park Red W••h do [40 \) II Servic.e S"ri.nl 26 S jQ Qu.act"Y SI'nDll EQcracia .5 •• ;) JZ 22

<0 Orctlard Orav NavaJo 5•• I] 2. 11 Sprtnl

.:.s ZJ[ SW!:. 27 ; <0 P'rond.ar Ss.. Mb'C. 221 L25 :..26 of :1.anco. Sh. Split XoUll" Kad.ison :..... uui 12 (9) t..aj".a. loI'am Mor~&4 Fm. Spnal 5S 20E C ~tswt 5 0 C4.cter AU 1 ~,t.OO LO,LlO 6,;'15-H JST 1- 3-11 H 975 L, Co. 0, ~94- ;:)S1' )-l9-H 19] 1. ;,915 is H£ C S£I:5V~ lJ 0 do do !.,350 6,"55 ",290- ast 1943 t1.J L; 2,716 1, .,J11 f.o.,J97.. ~o 1943 lJ. " 6.; 1,))0 ;, 4,f.o.U 5,'51 6,117.. ]1 do l1.J 278 2. 7,012-18 :10 123 ",719 5S '22.£ S!.\S"J.l4Clc 22 0 lan .war1.cJI.C 40,126 4,217 4,:66-13 ~ lJeLL .J4 t03 18 20 ?crol.... L10 b Le.der C,)C1'. ;H~

5:i 2n: 5t':S£t:a:~ 22 Equl.CY au Col 1.,040 ., :85 ., l50·00 ',J.ll head. ~O- -H 129 :& 552 53 22£ &E.~.ts!.c!2 h,d ~r1UA '-,134 "" :!4_ do l:3--H L02 )) tOJ Pecrol.\aI ;',.306 Colr-;t. lS 22£ N£I:SW.,.£l: 22 0 do 10 Phol,horU Fill. "',210 ':',3284,323-]0 1 UO(!'.) WeU U- )-59 112 19 5Z W.IMr Ss. ",J2& )S ~l..d..r "1M is 22£ SW.\:S£\:!IW~ IJ 0 Equ

55 !2E NE.tsWtsY-t U 0 Pat/, ~Z"1.~all "',094 ;',097- J 050(~) 'JeLl hud 11· J-59 120 20 [51 1& 198 ?ecroL.\aI 4, 195 ~O ColC'l'. 55 2:[ S'IoI.\:tfEldEt 2J 0 C~Li.f:lt'fti.a do 78 157 01.1 Co. is 12! ~tsW..\d,U: 2J a Ho U.and.awortt'l [Qcrad. S.s. I,oU 2,06.3-",.lL.ll.!U. n"v .H :'lO o&n4 !rav1:l L1 4,016 "',016'" ~4-0(R) Tnauc 11- 3-59 '1.7 109 It ~,LZ4 4 d1. .. cn&C'~ do 4,163 4, L6]-~ t 700pq SuO-aLU' L1- )-)9 2J lJ8 I. 163 iO Pl.~ troal cre.cer 55 22% NW~.l,jtV.lt 23 a Pan "'-ric.. "',02l 4,16t 4,141-45 fJ.l.l h.e.d to.. -59 )95 79 ?crol.~ ColC1'.

PholphorLi !'.s. J,BO ",091 .,on- 189 ,0 li4 Vae>.r S•• ",09) '-,243 WaDer S•• ",1106 ",290­ OJST 4 LO] 4.310 :",096... 1 '90pq WeLL h..ad ll- )-19 111 22 J6 ~6t 4,2'1 57 55 22! ~.ldE\:nk 25 0 Y.o It.ndsvoc'th 1-' 2,190-95 ;64(~) Flow :& [65 J.nd. !rav1.s L9 55 2tt ~J,j(r;ttN~ 2! 0 Pan .-lolMC'ic.aQ 4,1"'6 4,L4a- ~lJ.U .05 19Z 111 ".crol.... <",287 100 bleeder COtV· "1M Ss. 22!: ~E!:SW-tffWJc 26 0 Holl.andswolt'd' ",26S 39] 4,312-i] JST L ;6 2J 78 and '!rA'" lS

~rl.r:.n ;. Pan 1J./:HIr S•• :0., ,6' It P.ero!..... Carl' . C... liforni~ Pho.pnort.a F" :",272 :.08 ",,366- !)ST 1 1_ -~q tSB :Hi C". '.laM\" .i •• ':","'Q8 4,414 ;$ Z4£ 12 Marl:' i.. l.nclt l,j"ab&r S•• J ,-LJ-58 ;J U 160

- 46 - ~ oil and gas wells In bedrock In the Uinta Basin section

I: ~. lIart'ch of "'.clr plIt' day; na. plloM P4'1' :Ilinuta; (E) ••ciJu,caci; (M). 'llle...urad; (R). report-ad. &1: e~ ..,acar 'CDlI'la w•• c:allaccH for chea1e&l ~ly.1•. (£). (M). or (R) is baai.da the p.van unit. The om-r u.n1.C i.s c~lcuhc.d on '::hc but. of 1 iPG equal. )4 '~ aad 1 Ovpd aqu.ala 0.03 ~. >0 or poi.Dc of collection: flaW'. i..nciic.at•• eolhc:cion at. .. sprina or flavine ..,.11; OS'!, drill-ac_ c••c tor oil or po., 'u' OS!. drill-seal CI.e. data ra'POre-d by oil or ,at c~y. :11111 ion .u 'N=~

~ ~. . · '0 ·..3 ...... • u ~u= • -e : 8 =.. • • = " =.=~=o

l8 1,.530 10 ,358 L.50 8.6 eGL CST 1 racoverld ~ t•• e .Jt dl'i:ltn, lIIUd and 3.300 t ••e of f'r••h wlur. ') 200 1.)02 ... 208.5 eGL OS! 2 recovered 90 t••e ot lias-cut lWei &nd ).~OO t •• t of ga.-cut fr••h "'atar. 12 1) 0.0 30. 48 ~2J 1.b cS W.ll i. 150 t ..c d••". Raported yteld v .. 1... chaA to rJM 0 ... tnaa )40 ~d).

':'.1 2.; 1.8 148 Ll4 .2 20~ 7.3 cS

t80 (4) )1.8 19.0 8.2 eeL OST 1 recov4;red ).':'35 teee of ",lillnelv llNddy "".cer. Toeal depth of hoh at CUM of OST w•• 4,143 faac .

1 )00 3,700 .0,390 . &88.5 eCL OST 2 recoVllrad a~ tact of .11.ahcl.y I ....cut laIddy "'ac.r S..ph frOtl siddle ot forace 10ft "'atar. 1,000 3.700 10,J95 7) 7.8 CGL OST j recoverad 106 teee of hllh pour potne oil, 2,'92 fect of .....y oli~eut "'ecee, 4,416 t.ee of .Uli\c1y oil-cu( W.CU, .nd 2,762 teee of vcry .11abcly oll~cuc ..,.car.

1; :',100 9.210 110 98 152 14, baa 8.5 CS Analysu includes 29 j)l"Il aaron.

190 ),180 8,':'22 .868.3 eGL DST 17 t".coy.r~d 360 teet ;J! .1ightlv g.u-c'-Ic mud .and 4,290 fut at ~r.c.ki~h ...ter.

.1 1.9 .1 192 18 12 .4 38) 7.6 CS Held on 9.. LJ·61 "" .. reportedb 10 1'1'. (340 bwtId) by fr.. flow and 200 Ipta (6,800 b"lld) by .u lit:.. 9.9 ).8 1.4 380 ))1 .) 0)2 7.J CS j04 ", .0 786 4)' 2.1 1.160 7.6 cS

3.5 :.2 2)1 219 ~ ~ 7.8 CS An..lvst. includea 0.1 port dUIlI.i.num, 0.0 P'P"'I !luo't'ide. 0.00 ~~ m.an••n•••• and 0.1 p~ phosph..ee.

7i '9 .J 528 12 97 26 ,)9 8.; cS aaportad flow on o-13~39 ...... 5 IprlI (170 avod). Analyu.a includ.. 0.06 pfl'lll borem and 1.1 1''' fluoride. 5) . ~ 12 8.6 GS R.porud!low on 12-1.~,"6 was 2.5 IlJa (8S In,,,d).

1.)00 6,194 1.:28.7 eCL OST 6 recov.red , .. to ,urf.c. i.n 9 l!Iinuta.. ; .ttu .2 hours 40 cl1,nutas .aused 20,000 arra ~~:~:t::~~/~.~·:n::t:;: :~d 6ig/ 1. of wuer ?er ~aur. Fonucion ..,.ur 5.5 .8 439 729 9.4 GS aCl'orc.ed 101.11 depth, 180 fut.

5.0 l.O 779 10 ! ,210

~ ,.520 8. 93~ .dS 9.4 (6) OST S racov.red 140 f •• t of oil ... na ! ....cue :IlUd ... nd 540 i.et of lu-cue ft'••h .....c.r.

;0 :,070 3.709.0 GCL OST 8 tacoverad UO {Ut of rmud .nd 3,165 feet of .lightly ,uay muddy ..... tar. 5,100 2b,159 )6 10.0 eel. OST '- recoveuc: 180 feec of 'li.ahtly s.a·cue 3lU4dy ..... ter ·oI1.:n neck. of 01.1 and 3, 753 ~.et of .1iltU:ly g...·cu: W.Cer with necka of oiL l) 7,000 31 ,468 .309.9 eeL OST.2 recoYllced 4,~98 feee of "'.ter, (he tO~ 10 f ••t b.1n~ sl1.ahtly -.d cut. 2, 3.)20 iJ,772 .549.3 eGL OST 5 recov.r.d 846 fut of WUar', the top '-0 e.at ba1ft1111iShcly ald cut wUh e fev neCk. of oil. 5.400 24.140 .37 9.6 eet. OST 3 recoyerad '-00 feat of .l1.ihtly i ••-cue .:wddy "'.'er ""leh Clcciu of 011 and ..00 teat of .11Ine1:- ! •• ~cut ""acar. (~I 1 •.200 5,890 1.)0 1 9 eeL OST 1 shut In I hour, ooen " hours, shut 11'~ i hour: ,as in Z7 ~inueas, flll1.C :':1 1 hour 12 llnnut... ; floved :'DUd co muddy w.ter ~n first) m.inutes. slightly lUIS'" ..... t.l" in l.st )5 minuee• .at ~sc ..:n.eed rate of 510·570 ':J.:'t"elJ :'Jer d.ay; recoyered 3,524 feet at sl1.lncly ,.asv ..... ear 1,200 ) ,665 l )0 ].6 eGL OST 5: shut 1.n ~ hour, oo.n '-2 m.inutu, snut in l hour; g.. UllDedutt ly. 1.lU!ed 43,000 cuiac taet of las par d.y; I."v .~,H1 .. n 23 lAinut.. , !lINed 8".u)' muddy water tor t5 *lnut•• at e.timated rite of Z.'-OO b.rrels par d.y; recovarad 8,360 f.et of I •••Y w.ter. 1 •• 70 1,130 2. ; 4,':'30 135 9b ~8 6.610 8.2 as

104 380 2,b95 2.709.0 (6) OS1' 12 recov~red 500 feat of drilling, IftI.Id and 2,980 teet at frash WU":, ha.vtly , •• cut .nd slilhtly oil ::ue . 79 5,)00 10,in . 708.5 (6) OST 16 l"ecoverad l,nO fue of S..~cut drUl1.nl lIUd and Il .. gnc.ly J ..lty ",.ur.

66.000 178.213 . 08 9.1 CCl.

t2.5oo 38,796 .24 9.6 eGL

15.2 3,900 3J .653 .27 9.4 Ce:t.

'8) 31,700 20 109,400 3)0 o :00 1,080 93.500 9.6 cS Yiald w•• 1... th.n 1 Ipm (l... chan }4 bw1=ld).

.. ).100 189,200 ~/01 9.7 CO AnalVu.. inclUdes U,450 Pl* hYdroxyl. ),400 22, 91~ .40 10..2 eGL "nalytt...ncludu 545 PpIlI hydroX1.d•.

l! 0'8 1.3 ;',320 100 a 10,700 10.1 cs Andvsu inc1.udaa 20 p~ bot'on.

68Z .9 ~8 7. i 4.520

881 .1 :. no 0)2 ).690 8.a cS Analyst .. 1.nc:lud.. o.b PP'lI baron.

- 45 - Table 2. Continued

?aZ'tJ 04C'

:fA .. K ; 1.ocacion Q~racor ?rodUCinll or iN1Ier tOnMoci.oa u.

t,121 ;5 lOt W'lSl/

~nc 6S ,4.1; Morris R.A.ndl ia ~ f'l".)v 7-LJ· 58 0)4 1J 72 COtE) 5 a 1&4 "-:r1C:a4 l,llZ o,.:.n 5,J.J2·}1 )5T 7 .0 !.o2 (4) l,OD :'..::ro1.... Carl'. 6, U6.. Z6 J5T 2 0)-11-6) .0 l12 "1 9,550 .,

2,00 is 22! C ~t 22 a C....1ifornu 1. do 3,002 6,1" Se. Stor,l,~e 0.0 l.O 5,9150 au CoJ. Reaa&'X. t.ank. 75 22!: C swJc5wt; zr. ia l' U1nc.a ~. ),040 2,524-51 CST 1 9-19-35 lO 1 >57 15 2JE NW.l:;S'W.lcS!\: 9 Pac "-eric_ Creen River !"~. 2.304 S,i98 Sa. Tre.tec­ 'j. tlJ-04 '.0 l.O Z,09l l.croi.... R....C'u dr.1.n Corp. is 2JE C ~ElcSW-t 14 () C.aaforniA do 1.,906 5,t..89- lllill P..... lJ .0 OU C,J. ) ,308 _.1 b lilledar 75 lJ! C SlI'::SW" l8 do t4 do 3,171 6.154 Se. 1illl. !r••tar 2.0 l.0 2.000 l.amark. L::i sUl91a

is 24l C S\l~t 13 a H~Ol. au do 2,360 1,607 1,""7-3& Jill do 9-l0-ll 5.7" U\c1 a.finial

as :::! c n~.\:. 4 0 &e Leo i_cra- do l,S'3 I,n.·ll oST 10·H-H to, '174 Leta Corp. 5,1)91· OST lO-JO-'H t7,3S3 t,9 ;,70S is 2:z:t stl:SW<:stt 4 0 dQ do 2,:..ao j ,389 4,~6i..d: OST J IS LJ "7 II l,;

~,4

~s :O! C ~~E\:: 29 0 ia lJin.c:& Flit. a l,4.iO;"C. t,4JO C... sinlC :1 all z.:.ooo h.ad. 15 11.£ C Wt5Et ~. 'J hc:Ui.c. ;.lac... • 1,240 ::'at G.&.1 ~x. :.J. :1ounc,.l.t\ :.~. i JST "3 lOS t1t ;lI'::St\::lW~ 1 0 io OST t HO 19,905

4.11&­ OST J i98 l85 ",40& ia llO 4,"30 4,041-dO OST l,057 13 ,;3' lOS l8t St\;llll\;llll~ l4 0 30 do 467 .,d61 l,Hl­ OS! 1. l-l;-.t to 2,HJ t, 2.=52 l,;8t­ OST 1 loot 191 lOS :8,0;,01 1,746 ),311· DS1' .:. :,.. ':-ot 981 !74 26,370 l,n, ",2J1· 1,ns 21.500 4,ltO lOS 191 SE\;NW.\o;SV": t a jo do 1.:"30 r.,465 2,,,0-n s... 10-t5-0) II lO J,.:.4'i 28 Returics LOS 10E :N-tsw4o;SW.!t :10 1,18' 4,100 2,100.. • ~ 7. -6) t, 'J77 J,OOO 1;;:'O(!t) lOS ZOE N\l4::S£-\::S1I.\!:; 7 a do do 1• .33' 4,680 2,070-~6 DST J 10 .. 16-00 It 39,367 l,102-4 ,z oST '5 lO-H·oO II HZ lOS ZOt C YEl:SW~ 3 a do do l,.JI 4,120 3,llO-17 :1ST 1 7-10-60.2. , >2S l,"as- DST Z "-11.·04 112 lO ,506 J ,lt4 .5 .0 7.l 319 LOS ZOE iW~~~)3 'ol !uceau.Jc do 7SO 4,233 ilae:::it. !~ l...l.nd :Una,_· llea.c lOS liE st\:St!:fl!\: l6 0 0_0:.1.&. do l,l30 4,450 1,~O- 5.. i .. .0 781 ,\er1c. 1,520 ~C''''. 't

- 48 - m1.liion . ;

zEf

58 2.';'Ou

"',336 t5. ~OO

541 .:. .800 .b'" ~.b eCL Oil enc.rln" l::re.cer cone"lnt Ir.c-Q·llC. enemic.1

lO 0.5 228 214 3a J99 7 9 CS Sprlrl!S U'. ;'oc,leed .lorl~ t~. Gr.en R.t~er ~;"I Splte. Haunt,ltn C..nyon A.n.lYIlI H',C lud.s a.} ppm fll,jonde .nd 0 _01 ppm boron. (4) 3a2 )0:<, llJ '.2 0.5 S ;h. "".11 "'•• drtlled .a. an .Jl~ t ••t lor. 1929 .no l.t.r converted co • ",.. car ..... 1 .. J86 ~S

\J4 2..1 "lb J26 IDH AnaLystS tnclud•• 0.8 ppm ilutJride.

3.5 J52 t6~ 654 i ] iCS ~,05 " 70S 1.89':' 1:.7 0 .1Q.{::.,4 :, co

J45 2.1 56' JJ5 . J l.OOO 5CS

lOJ 291 'OJ CS '(aid

~ 09 .0 "'2 2e\ 5.. ; 10-i-56 ...... 2 iPIIl(E) (70 h\olpd) AnalvllS tneluoes 0.0 pOI'll fluortde

o ~ 70e 20 2. 2,b20 1.060 '75 '" 7 ~ 7 3. lOO 6.5 CS Yleld ~e6 Less th." ~ ~l"T' (;~H :h41~ ).. .,.... ed) A~411':sts lnC)cJdes C, 3 ;ll'm :: iuor.d~ 211 ;-7'} CS Or. 9-lS-':'8 :::he •• C1.:r..ated jis;;,~ .. rge ...... s 6 cublo.~ het ~r ••C::lnd .oov. th.. wolter lev.l oi che river anc •• much or lftQr. ciisch.. q~.d direc.tly lnto the river (!':-:c:n.&s 1 ~ ~:.,:: :'::). 2.. JSl 2. ~o 8., (6) OS! i. uccveu

.5 Ie 1,;:'0 S.lel

.0 ~. 078

') ,3)6 C..o OS! recQwr.d l. .J~O teet of I!••-cut ",atar 10.086 18.009 C.ao OST r.co..... r.d 3,150 f •• t of sl.q:htly g••-cue ""at,er and ':10 fue <:It ~J,.: :04 J.; 'J) 55 7.8 GS F'lo.... tng ell ""ell .... ith ...... e.r drl~e Anal)'slS lnelud•• 0.2& ppm boron.

700 .:.10 1. .01 i 3.35~,: Cl Flowln~ <:Iii ""el1 ''''t~h ".I.ce!' dove '0 6S2 :'2.0 ~.2 C~ :lO'oltn~ otl .... l1 .... tt!'1 ....aCe!' C:-''1f! ·.... te~ tent.atn! JI ~lo\Jc" y",i~o""-:o.ored or~.nlC. filerace

J I 532 \29 :: 6 ~ 3 b ..

158 ..il 3,.. l,J30 ~ 5 CS Do

'J J62 ~ 70 .5 1.090 J4J. '8 62 5.9 \,J90 ,6 GS Do.

'.08 3. J l.210 2b5 "-4 3 _; t .d&O .• S Do

~oo ~ . ;02 i 7 CGL Do

1. 2. l , 16; 35 1.030 8 ! at! F~:i.~~U~~~d~~U .... lo.th ·.... c.r jl:1.V•. An&lvli., :.ncluda. 0.95 pOlll ~oron .lnd 5J 1.9ilO .:.00 7; t2 ,500 ~o GS FlaVine ,"i.l ~.1l with Wolter driv•.

L2'J L.930 1.150 920 24 , 2,340 7 • GS Do

,0 t .68: S.·JO 8.1 ...... 00

i10 1,595 ... 50 8.0 CC1.

.:.:/8.08.0 OG OST:. recov.red 780 feet ot sulfur waCilr .

ib2 . :80 BJ4 574 .. t 3.9 2 .4bO I 8,0 S Flovtn!! od "'ell '11th ..... ter d!'tva

.2 i71 7 a cs

.380 35 2. 9 .!)O .. CS F'low1ng oll ""ell .... 1th Analvsts l"elude. 0.44 i'l'ftl boron

J) " 564 fli U •OS . 4 SOC OST ~ ~ecov"'reo 1.)70 feet Jt s\,Ilfur "'at.ar.

J8C

'S 'DO .'Ji.8 OST : recover.d :.ao te.t "f slt3f'ltly ga.-cue. mud and )90 ta.t of tre.h. ",..t.r

210 ,c : . ~bG 290 .3 ... 10

1'" GS

- 47 - Table 2. - Continued

AA .. !C. o ., , ?t'Oducin~ ­ , OoeraCoc , , -Jr ~.r tOnlac'l.Qn ..,­ =­. ~ ~ , .:t.

0.0 11 '.as 22% C ~E\:::tlElc l i ',J Bureau 0 C Gc••n Rivet; E'm. l.WO ':'.J18 1,)lL­ Land. :ian.~." 3,.:.05 ..ftC ~OS ZJE NY.lt:S\JtN!t 2 0 Rt.aole OU l,l••accn i'm. '-,:.s2 ",B'Z- i)s-r ) It- -(,1 roz l26 LO. J05 .lad. itaiinJ.n1 ". ';L4 CO). lOS 2)[ NEl:ttV4::f(W-t 2t. 0 Shall all Co. Crua lHnr FnI. 375 J ,U.s ) .066 aeturn 10-lS-ol 572 t,:J7: line LOS 24£ SE~JcsEt Zg 0 £lPuo ~.cu­ ~••av.rd. Gr. 4,560 3. '::9~­ Swao ::ut o-ll-;'f l.nJ 32 5.194 ,.aL C". Co. '), )05 ~:{ ~OS l4E C :-;E'cS'W~ 12 0 Shall OU Cq. Iol_satcn Fill. 3. )06 :'. 1)8 ".J90~ JST Z L-Z:'-':'l 21 Ll J.iJ6B t, '-,4.1

5.130­ ,)S! 1 L-l8-~2 La,3BO 5,JOl do 4-, :JJ8 ~ .. l87­ l!!!2. Prod-uetLon :.-)0-02 lJ8 7,917 ~,~94 l X..c..rc1. Gr. 4,938 ';.310­ Cuclepu S.. 1j',3)0 ". ~47 1.040 290 6,J2J 4..

liS 12! NE~~Jc t4 a KinlJ OU C". l.3

J Hl.Dot. 'Jt.l :.tu.acch fm. 3.39Z "i,~Ol 4.715-J6 )ST ~ 104 2ll mel. RetiIUt1j: t:",. 5,119-47 LO- ·.,1 LJO LJ,iJ8 ~ is 24£ S\lJaN4:SE\: ~ a Sh.alu·oc.k all L671 22J- 3~ :6-':''' l2 . ~ .:.)a mel. c.. C~r"p 2,207 do 10 2,318 H6· .i •• '0 l2 .5 I. 396 R"~CKS ;0 2., :l1! At l. :7~ 1. J6 ]., 1.5 ;')7 •. '::

US I !s! YE-'::S£.:swJo; ~2 0 COo.ciMnu1. 22·l Mancos 51\. (,.. ~J2 At ~. 22S '54 78 l,lOO ,2 OLl Co. ~2S :"~E C 511·t:iEt !oJ a Cutar au I),aL4 9,.:.46 3,505­ J~O 9,l90 l.Ol Co. 3.H1 ~, ;04­ CST 15 '·\2 ll7 :6 4,196 II ;,789 ~)S 2JE SE'tSW\:!tt~:S 0 Sir.yU.n. OLl o 2.170 2.000 .1>0 40.11 10.4 1. 26l Co. / :45 ZOE ~.l:SE~t 7 0 Ph 1. 11 i:J' 7,0:13 ~,zas 7.080­ JST J , ,012 ?crol.t.a 7, t60 Co. 1.45 IO! C 5W.ldf!k::: JO 0 do l,J90 to,nO 3,790- S•• 5.. : ·'l-65 2l 6,4 ll,9oo n ].3'20 bCllarlc.s itemarKs to,J20 4.631 4,5JO-dQ ~ 5"'.0 ~.!lC II l.:' Ccun Uver :m. J l.lOO 1,38J- j"')(~) '0 '"!~." ) ~ j" :J Jb ~,HO II :j5 ZU: c s~tsEt 22 ;J AcL

Eacnd.. 3•• ~. 1.94 , ,J6O lCO") 5.LU )]4 1 34 Fl.lW" :.i L7 i5 36 l7 30 TIX) !ilIUc.o. tnc. ~orrl.son Flit. '.lOO ~, iOb ~. 530- E:t.crad.. is. ;, i06 I ~ . ., L C.iD\_l .'oelll; '.J.a•• cc::~ em. , 1_ !5-4;3 5prt:li [:: to

~7S Z4E ~:SWJ:SE!l.:: 1 Entrad.a :is. 5 .~c.o S .147-70 oST 1 ll-Z1-~ Z.FO ]0. :00 1is 24£ :roltsW.t5Et ~2 jo 3,070 Ac 5.1..60 :i.. ll- 1-60 !.J04 10,100 il~.rks lOS ZOt ThOl!l,.on ~ ••ver4. GC'. .'0 55 ,4 ~04 ipr1.Q 'i ZOS ZOE !7 Chutu'tta14 S.~ 5~r'1n. ~o 2.-14-41 [98 C.:J ... 1 C.:J. "

~I )usotved. l.Jl~d.s :J,!.c';,1l ... o:e4 ;rotll d.cer:m:a.n.et ~~n.t.:'':UAlnt' exceoc as noced. I/ Anal:,u.s "y: C...0. CJ,cc.r Oil C.J. ';CL. ::h..i.c&! Uta C.Oh1§1ca,1. ~...ooC'ator:.." .;....\1c• .I:', ''''~o. C!.. :.Jra :....oot'ac~(l.U, Inc: •• Ja1.1.1., r.x. CO, C"nc1nencd au Co. CS, (';.i. c..o1.o§i.eal. Sune., 1M, ::t.&h SCi-ce iJeoac::Mnc :t iof. • .a1.th ?.\., ?1Il .-Yl:ertean ?ec-:" LeOli C"t'i'. ?.."!1:, l~C:KY :1.oW'\cai.n !:n,p,n••ri.nt: Co •• Crand Junet1on, Colo. ShOo ihdl 'J11 C". 500, it.&noLi.nd. Oll .&nd c... Co. '':C. '';t.&il. 3c.ac. Chuu.,t 31 ':lnc.& io.cu.l :'!.. n.di....n. :1 !ace. Ti [n i01·..Ic1.o(l i.~ o:.:"=:. lC U\ah·!llJ. II ,.o..n.. lpu .up~U..d ",v <: ... rcer Oil ";0. :' :.;c.al Lr~n. ~ .. ~. S tJ c:.. 'J t C'J i.e ~ 2-7 . "il ;tU1.du. ~c L.30-O: . .:il ~e.1.Jc:'V1.c.·J loC 7'S-? 11/ :tuLscivi.C., I.e ~7-!. ll/ ,: ... L~ul.&ced ::""lIl. ~;)4lci..f.!.: ::ondw:t.a.ne•. ~)I ~u i..Hi.·/icy IC 11-:. :-:1 ::l••iJci.'/i.:·1 .. c 7':'-:. TIl ? •• LJlCi'I1.C}- ~t "'-7. • 50 - wu.lhon ... ~e ~~ -> ~ ..~ 'i ...... -: i. - c .. ! < .., ~ o

151 8.990 ~~. 940 96 its - GS

130 30.209 .Ll/C. 2J 8.6 PA OST 5 racovered 110 hat at .lightl:-r .....~ut drlll1nl mud; l80 t ..t of -.ad"'cut .nd .11lhtly S••-cut "".t.r; and l.226 f.at of .llihely •••-<:ut "'.t.r o t .1~0 78 1.870 1.2.00 1.090 1,1 2,200 7.b CS 011 t.tt convart.d to w.. t.r ..... 11. An.alyu.l includ•• 0,,30 PlM boron, 1.8 ppa !luorid•• .lind 0.00 P'PlI ..nlan... '!lald on 7-lJ-~8 ••u ..cad at 200 1;- (6.800 bvpd) 485 911 570 422 22 1.J 1.260 7.2 GS The oK of rhe w.ter at tM u_ of cell.CC.lan ",•• 7.0. An.. ly.i. Lnc1.wi•• 0.8 plllll fluorida ~. JSO 2. 92& 2.25 10 CCL l:lst i, w.tar and '.'·C'.lt :aud to 'urhc. in 35 ali.nu'•••ft.r tool 101 •• open.d. A.nalYli. l.nelude. 1 p~ 11tnl,U1Il . a : ... 50 13.700 tS .207 . JO 8.3 eCt OS! 2 recovered 82J hee ~t ....'"r .... ieh 'cu. of all on ~op. An.ly.i. include. ) P1XlI lithiWll.

188 7.230 14.970 1001.JOO

820 I.JEtS 2.8080 eGl. :>st 1 recov.red 190 feet of mud-cut ....t.r .nd 2.000 f •• t of cle.r ..... t.r. l.OSO Ii. ill. t 198.7 PI. Per-toueedec. 4.74], 4,7Sl. 5 •.345. ~.J66. ud S.J86 f ..c

191 S .8JO 58 GS

B.O 421 4 .~90 100 290

)04 6.210 100 290 GS

l~O )8 l.J Z .J)O 90 96 4) J, 190

It :! ,6JO 95 li8 S .230 8.1 CS OS! Z recover..d 19~ t..e of aIIuddv I.'-cue ""aeer and 1.020 teee ~f chan p.-cue ~r••h loIater 90 998 9.9i 9 eCL W..c.er praGueed ",tuI. dr1l1in1 "'lch .a•. _..eer lncr••••d ae t.b80 feee. bue 'CJrI'e ...eter- also c .... frOft'l other 1.01'1.'. Drill1na.e 2.310 fe.e when ._pled. '4 3.100 ~ .528 1.006.2. eel ;:)sr 1 recovered 180 f.et of he.Yily la.~ uld ""ater-cut. =.rod. 280 teet of heav11y Illud- .nd la.-cue "'.t.r. and 2.651 het ot h••vi.!y ••'-Cut "".tar 1 • ~ so 29.000 31.7..8 .18 7 .• CGL OST 2 r.eovered lO~ f••t of s1i4htly oil- and au-cue IIlUddy water, 90 f.et ot vaur .... 1ch a SCUIll ot 0\1, and 51; faat of v.tar ( ....pl. ta"en ae t.)ol). 1,;85 l~ .000 29.611 . .26 7.7 eCL OST 5 reeoverad 5 fue of ~1l and 225 f ..t 0 f ftlUddy ",.c.ar ~ • 19 J 2~ .000 ':'c .130 18 7 ;) cct OST t r.cov.reel 30 ieat ~i Oil. 270 i••t of wae-r-cut 1,""U~, and 1.900 ta.t of "'.tar, S

.000 ~~.)OO 55.900 • GS hrforae.d frO'/ll 2,726-80 and 3.970-4.00S tut

':'1,':'00 62.502 lQ/~J 7) eo

2.aoo 8.1..;:00 .1.5 9 CO

l26 ~.. J.O 2.090

':. iOa 3.0b8 20 3 CGL l:lST t. r-@coyered 7)0 fe.t af .I1l-ghel" "'ud-cut

, ':00 ,:.. DOO La 7 0 eet OS! i r.covered .. 70 tUt ot "".t.r, 900 feat of bl.ck sulfur ..... c.r with a sheN of ~uvy black. 011. )9 ,000 ,,13 7 fCC"'.. OS!) recov.r.d 60 t.ae. ot w.car-cue IllUd and 440 f.et of :BuQ-cut ....ter

~. j80 )8,000 67,751..

2 • .5 .. 9 6,462 1. O~ 8 6 eet OST 2 rotco,,-ud 60 feet of Wolter-cut mud and 1.170 fut of traIn WolC.ar.

,j27 )7.152 79.792 .12 8.4 CGl. OST] recoyer.d 60 f••t at W.tar-cut IIlUd .nd t.6l0 i ••e of ...lty sul.furv&c.r.

_. :'98 ;. t .280 ~l 8.1 Cet OST'" r.coy.red &0 te.t of ·.... c.r. 180 f ••e at sli.nt.ly 1••-cut w.e.r, ..nd • trac. o! d.rk Ira.n 011 J, '18 )4 •.572 13 8.1 CGL OST; r-ecov.r.d 7~ feet of B.....cut mud. 105 feet of ga.-cue ....t..r)' lIIud. and ]60 t ••t oi lIa,-cue sait ....t.r ~ .600 ~, 700 9,078 .81.. 8.'- eet Onl11nl ""tth .ir; ....t.r lola ••ncountered batvean 2.850 and :.815 feat .nd tha '01.11 produced. )·J.nch terten of fOMll.tion w.. ter ~ )0 1.190 :.. .832 .(,,7 8 9 CGL At drillinl d.pth of 2.S94 i ...t .....e.r flo,", 101•• tncount..r.d; H d.pth ot J.60' t••e yald ...... ppr01C.1IUt.lv 120 IJn (4.l00 ~d) 3':~ 45.000 97.937 .lO 9.: eet OST) recover.d 720 tue of slightly ••tty .ulfur "'..c.r. lOi 1':'0 t.966 L55 8.1 eel. OST 5 r.coYH.d 1.050 hat of tli.htly gu·cut lII'Uddv buckun ",aur s. 296 2 •.221 ).JO 8 seC".. OST 1 flow.d or'C~l.h ..,.t.r eo .urfae. \.1'1 J~ l'Il1nue••. ) .37C 1). too !E. ,(,,89 .Z78 0 eC"... OST Z rlcov.red 860 f.et of :DUd~<:ut .... u.r.

~ .0 70 JO 98 68).)40 9.0 GS iJ.etr :rom .nnylu. !).hlnd 5'~lnch ca.1.n~ from 168 to aoproxu"aeely ':'.000 fUi:. 'W .. t.r ul'IIple col~ectld b.tora fin.a~ converslon ot .b.ndoned i"...... 11 to .... t.r ",ell. ·••ter encount.red .... hil. drill1ns from .IIbout Z.OOO to 4,000 feee at r.te of 200 to BO :2.arra1s per hour (140 to 170 IIpm) Complet.d Wolter well produc:lon. 30 gplll (2,700 ~wpd) ~ 9; ,370 10 99 108 3.080 8.8 GS Reported fleN on 9-29-59101'•• l,25 gpm ((".JOO bwpd) .._eer produc.d from .nnu1u. b.t"'••n 7 7/S-1neh hale and 5~-inch e ••inl .

• 49 - Table 3. - Selected hydrogeologic data from springs, water wei

~.JC.(.1011: SaLt l.ua ,It• ..nd :nacid,1£n. :;"u.rca: ~. :u.na l:;ann.eJ.; 0, .n.l JC' ;&. ".eLl; ), j~rin,; 1', e. •• t ho1.e; :J, "",ce, -.... Ll. O~.r.tor or ;)"""4r: ::..... '.It J"ar&toC' Jt' J..",.r ole :1,tM ""aCU' Jam9L.. <01&' ;;)Uac.cad ;oC' ,::"t"Lcai olnaiysis. ?TodUCio,l t:::Il:m&cl"~Q: :llI. •• :Or.ll.&Cl0o.; Cr., Crou9; L~ •• :'~.t::ln.; :i1H' •• ~_oeC'; Jad., '.c:itm.nt&ry; j'h, 5haLe. 3•• , i

, -,,,-­ !..~c..c.10Q ?:,;)dUG1.D.1I - , ;ot":uc1.oa, , -. 'n C.

3ac'C1on

Shi.tlar~ l1.br. a1 269 217 - ,09 :L':' )! Chtnl. em. :')5 4.¥i NW.lt:tNt:tfI.t]3 !J R1c.h.&rd. 'loa. ;0 2J .~!o. ll9 ,I :4..... l4.5 9~ S""" 4,,2 )20 19,178 hcroL... ~t ~co. 5h. At Z. J06 ;0 12- -"2 !~a t4,911 J, C.J • !.utunk in. ~r. ),023 3,:'16 At ),',"4 ;0 l2- -,2 l20 ii.D7 L. ~l ~ac~s .i'h. At ), J:~ '0 12 4 ·.,l 10 i . )"'9 tSS lOt C ~ij(!.t 16 a Sh.U au Co. M.b.U.tP9i.~ 3,.i50 lO,i63 lO.05S· 0ST 3 S·l) .. ja ~, 5)0 o. Sa3 ,.d.. :oc.x.. LOt l65 t5S iLl HE\SE\::Sv.\: l. 0 C...rboll 01.0JlXa ~.v.Jo i •. ),095 l.ll4 ),095· l-21-J9 (I) J. &Ad Che.1.­ ).114 c.d Co. l.~S III swtsW.t5w-t 7 0 Pall "'-rtc:aa KiUi..UP9u.a 7,')42 S,tS4 ;,!..33· OST \ (lJ t ,144 111 10.3l6 I. !ac.ralala ,.d.. rocb 7 ,~e6 Corll. l~~ 12! SlJQW.lQWt, S 0 Shall au C~. R.d",.11 U. ],no CJ,UO 3,H3· Elb.rc e:ll. i,UO i.174 CST ~-"' ), :.Q6 716

:55 12t l~ Manclu Sh. I') ').)0 \l 302 141 ~6S 9£ '.l'."a~t l2 Pun all Co). t-~ l.d",.ll !.5. 1,300 tl,~2S lO.Ul· DST 2 l,Jl.J .:.62 22.050 J. LO .ll9 ~6S La C m:~t 1 a CHi.. Sino.d. r.•• :ibr • t.,ul4 4,Jl4·dJ DST ] i.rvtca au .Jf ~o.nfILop1 c•. F!Il. Miuiul:PPL&.d 5.l12 7.Ul· OST f.d. C'?cks 1 })O

~o~ 1.2.E: C n-t:Nt ::.. a tq,~i.Cy an Si.obad. LJ. :ttIr. !..,l41 Co. ~f ~oenko~( .... l· .;) ". LSl­ t- ·IJ ~, ~07 l65 U£ C ,:,"U'l:!Itt ~7 0 C...rter 011 Coconino Sol. 3,'H~ 4,dJO 4.~2.. "j8 051: Z l-l4... ;7 l.lSS ]11 4. ,'49 c•. Mad.ison r... €I. 5d 5 "i. ;98- OST 2.. .)7 i..936 .14 IS.111 ], !.J3 i6S tJ£ £~JcsWJe Zl a R•••rft au Ghn C4Ayon Gr. t.771 4,64'. At :.400 ~ s •• &Oct. c.. Co. ;0 ~1B.rkA

Ko.nko9L F'Ia. 2.11Z 3,396 ],494... S lno.et L•. :1br. J.l16 J.114 J.110 05T 1 3-17 ·,,3 ,t ~.nk.olli. ::n. SE!:SIll:SE~ 9 " Ro.d..U_ Manc:)s 5h. J-l4-41 .i2 'as 1S8 150 c.ys.r lSS ~4£ NWl:SIll:SIll: JO 0 a....l. Ot! I K.&i.bab u. J.;o6 J.710 1.006·1J OST l :,:.uo uul Ralini.nll C•• J.710 ',119 J.717. u5T ! J.au M.iUi"ni9'1.£ft 6,614 5.~61- CST 7 tz·,zo-oZ J'S 2. ~OO l6,l74 Jad. ~ocu 1,'lSl

~ 95 tOE 5 5 3ru.sny!.anA J4 lO-ll·IS 57 ].J .J 3h .. :ihc. Ot mr ~on"tson ea .. :15 UE SE~E\:SE\: 12 a P.lAIlbl. 011 Paradox FItI. j .Jll 5,4.07 ;.ne­ IJST II ;I., t ,O2l ..ad. aatini.n'l: s, ,OS Co. Missi.s.l.p'Pia!l 1,242 ~, 716 .. iJST lZ t.d. t':)ck. 'i,HS 1. 95 242: S\lJaf\l4::SE\:: J5 a ?rCtllOftc0C'l' Bcuahy 3••i.n l,)70 1.:.44· ,dJ ),1lC Oll CQ. .ih. ~bc. ot l, SOS l'loC'c1soa :'II .. 19S Z:s! S!~.&ac!C lO "J £. Elbotldo MaC'rtsoa E'II. .llil ,-11-61 1.7 S. n <1 HI II 5.3 J4 l,620 r:1(i) ZOS 7! N!~E~t Z1 0 Pall ",-ric&Q KAib.b u. 7,llO '; ,~ao ',110· j ... JS ~, J20 ;:s :~. 700 !'.crol_1.a ] ,220 a-rk. COrti.

205 7! SWJo::a..1r:SW4:; 27 ') Enc,1.i.sb. 011 !J .. 17 FU:'C':In 5•• ~'C'. 190 ,It 504-d06 "9 :J Co. ;Jf ~nc.o• .ih. lOS ll! ~ S Buc.khOnl 'rl'un Mo.rUtolti("?) LF1I. ....ill­ :low 1:9 L24 194 '0(0) ZOS 2Z!: C S'E\:tCW4:: 30 0 C.&b..a. !Xltio" !·l :iorrt.sOQ em. 2.064 1,)88... :)ST ! ill "I f.'~4 t'acion Co ~'O • 2, :.'6 ZOS 24t tfEkS!lz;SW4:: 29 a G. a.rub do Joo 384.....aO 1.1 3:0 Z.J'SO ta' 761·711 z.,;. ;65 L.o5v 3J 872·.ae8 '0 ~ • J ~ . f:J :94 :0 115 15£ tN.\:;SWJ:SW~ 14 " Sutl.ri~'C' OU ~1J1si..t'LO~1&l:l i,j3J lO.2'J5 1,333~ JST 1 tOt .... )70 t2').957 Co. ,.d. :':;'ICKJI ~ ,1i;2 9,705·)2 JST 3 .• LO, ::":'0 l.':'10 36. 32~

215 1.6E Nt-'!;:SE~£t}t.. '>I C. Ruby Cr-"cal ~nt.::ad.. is. H ... H~ :. )00 ':',010 ~Y'.t' t.:OQ 2lS t3E SE\::SE\:SW,,: 33 0 Poc.un co. ,f t, ;)6 t07 ),554 .w.l:'tc.& 2:S 6E trJ.It ]J ~ Zr~Ul1 C.Jal ,u'ron i •• ~br. 196 J .315 ~. ~t :u.c..c:o' .in.. US aE ~J SO. rl .. 3uCOn J.nun Sprin1 C.&r.Dal !tao nov 4-11·\9 Il z26 l.670

zs 'J F, 1. :uc '90 1~·200 10- 2S-18 ;l 10 III - 52 - :ftdl1on . -0 ~ ~~ ~ :8 ~" • Q • " 0 =; ­ • ~~u ,,-' H

,) L~ 9 ... 040 8.2 10,0500 )99

5, :0) IJ ,500 ~9. 941 0.29 7 7 eCL CST J recowred 150 feet of l!lUd &nd 1.553 tuc ot la.-:=ue. bucklth v.ur

99 U, 2 8.9 ShO

t 1.:50 19,536

'2 620 ) .550 3.562 96 OS! 2. racovared 374 hee. or 111ane.1v g••-cut :'lIUd, 280 taee of naavlly g,u"cue and ",aur-cut mud, 9) teet: of very sligntly ,""'cu' lIl.uddy \I.cer, .and 93 tnt ~t muddy "".t.r ·.... e..r u.zrt;l1e =ol~eCt.Cl &t :ooi. ~70 ~5 . 762 1.020 11/ 27 7.8 ShO OST 3 recovered 236 hat :Ji J.'~cuc mud, )08 tect of lalnly I ••-cut, o1.l-cut, and ",ud-cut ",.ter ••nd 186 f.at ot Ililhel)' otl-cut &nd 1111ne1y I •• ~CU' lDUddy ..,.Car )08 i3.J12 23.326 2. ,bOO ll~:H 6.6 ShO

.:.iO ~ 1 .85 '; 20.452 3,825

:. 7~ :: \ 6L9 )4 93 16 942 a cs

.500 )~ .961 . .2J i J CGL OS!:: recovered )00 f.et of g••·cut :nudd ...... tu .Inc ~5':" feet or mUddy. 1111hcly ,.lty ....ter Analvl:,.5 :r~ ::Iottom sol.tllDle ':',005 19,500 )9.1a8 .21 6.0 eCL OS! 5 recoverad 1,230 f .. t at lllUddy u1.t ..... ter ....t.r l.ample from 90 fe., .IDove tool ))" 6<3 1.0 1,170 10 99 60 1.300 8.2 CS

)10 10 " 58 1,720 2 GS Report yuld of 250 !3&t'rals of loI.ter per hour (175 IpaI) "'iul. drlll1nl ,I.e 1.~.59 fe.' . oJ . 6 ~ ,200 i .320 j GS A!'Iai.vHs i.nclud•• O,4~ ~OTT' ~cror: ... ~ :''0'1'/: £1..,;onoe .•nd GOO pp:n m.an~ ..nese. S.amoi.e ;;;01i"ce.e<: .... ner.....at.r (lo", lola. enC:OL:rHer~C ,.m~le dr~11ing .... L .

;00 lSe . 300

523 I •• :)00 )4 b 9 eGL OST 21 ..... t.r 5.600 t2.,511 .59 a eCL OST 2~ r.cover"d 600 fa.e. of .al-cut. &nd sl11htly ,;Jll-cut :!Iud. 450 het of "'acar-cut llud, &nd S.970 teet ;;t sliane1:: :nud-~·.Jt wolter 17 L .086 6 UC

'40 .. ,711 2.65 9.3 Cc:. OST) racoverad 630 feet of ..... ur-cut mud (escllll.cad

-) l,:'90 18.300 15 J2.iOO l.910 l. ••.70 93 119 48 900 .J GS W.. ter .;ollect.d .c d:l.scnaqte l1n. to C1SP0.1ool1 pH .fter :reacmene. 0;;0 re.-ove oil. Yield "'.I.' 1 bvpd nau tnan i gpal) )20 !! .245 L02 9.'0 CCL

818 q 35 8 ': Cct

.01::5 l.9M .97 S . .:. CL 057 • recovered ~ •.:.82 ieat at" ~.s~C\,lt w.'er ]55 ..... ~8b 66 8.6 CL DST ! racovilred 525 ! ••e "f tlraCkl.5n ",.cltr .... t.th suUur water ~! 3 1_,981 3~ . .2 5) 23 J Ct ~S7 ~ recoveree dO ide. ,;Jf u1inU;: ~ ••-<:ut muddy w.c.er .and 950 fea' of sl.tincly S.$-cu' 'Dr.ckiln ..,.ter

'2 54.000 ea .052 L0 3 eCL Swabb.d ~ barn i..1o 0 i j)er hour frOl'll 8,800 feee "'un fluu:l lavel Handtn, at 8.000 tue :.3 )81 )12 04 ,06 7 CS

ooe 10<0.·:.)8 .09 b ) CG1. Report of analylis lists tha [ncrad.. S.ndscon... the "'at.r-b••rina !.;Jnulc1on. 596 )4) '0 12 ,42 CS 92 10 • ,CloO -os

. L ~2 Si. .500 So db 086.3!UiE OST 1 recovered 40 feee af drt.!:Ltn! jlud .nd 1,460 f .. t Qf sl1.gntly , ..-cut talC waur . .}52 J) .500 56,)69 i':' ~,O JUo(E Drl1lad ·"tcn .air from 930 to 5,161 feet.; encouncend Watar ac 5,100 tea' and the wolter rau )00 feet . a.o 1.2 "0 ..00 • CS

26 .0 1~.090 .. 32 7.5 10M M&1yIU induct.. 0.1 p'Pfll fluor1de

. 51 . hie 3. Continued

I o ~ ~ ~ !.oe.cion t'roc:tucing j cormacioo. .: "J_

~ .".~ Q 0 Z

V .-\lDlIn4& Parad01l iftl. :'low 35, ~50 ~.crol.l.8 Co. do l,rn.. S•• do 76,176 9,434 58,J01 "0 5,396 a..-rlu

12·)4 M1.s.i.U1.p-pi,&a \0,020 \0,0;)- ~ST ) 8- • S8 '~, l'57 t,441 00,729 Jed. rock. lO,ln 19£ ~~-ttCEt. ~fI; J P'JcuQ. Co. ;)t Morri.soft. tID • ~03 l.J63 1.1l5·j~ (l) )29 US ".H) .\laIar1.ca S • .Lc "";&.0. 511. 0.0) tol l; ]4) :-!be. ~i. :1orri.on ::11.

Uc&b. SOUoctlern 298-319 \2·19-); :05 Oil Co. Cht.al. FII.. t.lOO .:.]4 U7

15 10E 3 S Clut OWeUu- loIt.ap'. S•• 7.j l27 L12 )9 ;)9('1,0.1 51:1..11 oJil Co, L :-{1..isi.uLo~L.an r.;'H 1.jOO- osT l L,4J04 208 r, ,,53 Jed.. :'OClt' 1,,'02 ~obU ail C.J. ~2- .) 3,J55 ~, 5)0­ ]S1' 3- -61. l.165 i5.n1 '0 ','l; 35 16£ ~EtsW.{5t1l:: ~ 5 0 io )4-l; '.tntc. UIII :).1. ~,Sw.O :'.301,) i.. i.e. :t'JW }- ·..,1 6d\ :1.tlc ;){ Cutt.r :teCl\aC'k. Remarkl :11I. t1i.U1U1.~pLan 3,028 3,HO­ ]sT l j .092 2,H6 I I_ct. ,:,oclt.l ~ ,<.40

J ?sn ..\lJl.. t'1.C.aa. 3.188 ~,o18. OST) )- .,,1. } , ..69 7'52 :'.crolelJlll i, 76a ClJr~. ~JS liS C iEt:tE~ i.7 !.x.aco. tnc. 10 3,458 d,7')2-18 lZ- ·aZ .,,30::! 1,002 i6. l75 :JS ti'! C :''W~SE~ ~: do do 3,t.41 8,10Q·l6 Swao tUC l2· ·,1 i.ilH \,"SJ ~6. :354 ~JS ".. ::iE~WJojiY~ Z,7 :-laC-1.ona1 lark Wt.npce SJI. "\ 1~_~ l4Q Yell ~...d. lO-H-6Z ~l 5.v '8 \8 ;4 Secv1.ce :rEr :.Ulol.r1d.. Solie. '...,un Sa. ;.. 1!'~9'ld .;-Zq... 50 30 Ll i::.~zo 39 L29 O. L :Co. 1.3 ~bC'. ot aalUock. ~orrhon F••

!JS DE Sq\I&V hrk £ntrau 3•• )4 now 1.\ Sl'rinl TIEr Dev.y SUdp :10 do u 147 i9C1tll T.a.a i ••, K.&ioalll L.a. do to ... )0-58 1.1. 124 \8

:~ ~JE ~",.Ioj

do 1,562 2.2.00 l,t!OO-dS lim t'Ulllped 1;8 16 l.d '. Si,noaQ l.... :ibr. : .ln8 :1ST 5 ~- . sa ) ,6 5,HO ;, JC ~o.nko~i. ea. 29 C.l.r:tlel :':!l. '0 :-10"" ;0 ]; IT5"

~~ !.4£ ~E:~tsEt ~l oJ C"""toer 'HL !, n.:.­ OS'1' .0 '-"0 :,J. :.;!.C "'00" '0 .-... eo I.I . )G._". - J iheU.Jl,l:;.:._ ~ilSl'Jl"fj)l..n ~fla· JST !l-l2-;8 L,}57 ]84 i.a. :'-:c«', ~ , )b i Co\U'chous. ~"'V&P i.,. I~:;- i,1)-"J l5 5pnnlli l':'/ Turnoov ColO i. Encrada S•• 170 -.00 .i~n·1,J\1 5{'E) Oai.on -Cr ••'" ?a&a401( Fm. 16; u: ~pri:t.g

~8l ))9 :55 I "1'1/' SOli;; w J. ~C'tLn' 'relll~l.. Jut:Lceioa. Z3S .... '1/' SE"dWJdWJr; ]'" 3uraau oJ! Gil.loa. 3uc.u tner"," S.s. 298 S.. i ... ]72 lO; l..&nd. :-!..ana.e.. ~....S'iu a."CIc.. :\\ene Z",s :3£ C ~ioI~£t ~.5 0 5u~C'ior oJLl H-U R.C"!\'Io,,,, Gc. ~,196 4,319·;5 OST L i- .;;] ~o • t.l'lMY Zone Q t J.070 ?.&cadoll: :aa. 255' Bt: C .iU~t 1':" Q C~n.ci.n.nC.al aet"lllOI. Gt. 3,2.33 5.He 4,34'.';1

~i ... i.sli,O)pi..an oi, '07 ',;63 'J ,398· OS1: l ,ed, :'-JClilS 7,-B, ~5S l6E Ci£~~-t o SeancUd au do S,359 .; •.:..30­ 'JST J ~ J,• ~2 '';0. ·,c ., ,394 C.al1J!ornh o Su.~t1.oC' au c.3-1.0 do ',010 ',66' 6.)61-" oST ; 560 \ ,069 C,J. a Pt'~cory '-1\iee iiA S•• \ ....; \,71; \ ....\. \6 1.O~0 79 OU Co. :i!)t.::lf Cuch l,n~ fill.

. 54 - Id oil and gas wells in bedrock in the Canyon Lands section

_14: bvpd. bArrels ~f wacer per 4ay; JP-. gallon. per 4l1nuca; (!), uc1..macad; 00. _ ••urad; (R), rel'QE't.ed at tilM "'acer s~l. 1.1&8 coll.ct..d for c:h~i.c..l .11&1y.is. ~. (t). ('H). or (R.) i., b••ida tn._ liven 1.II11.t. !he ocher unit i.~ c.alcubud OD en. ~.u.s IJf l ipaI &/:tua!t )4 b"lHi and t bvlKi aqu.ah 0.03 gpaa. :bod or poine: of eoLl.ct10D: :low, indicat•• coU_ectaD at ...pri.e. 01:' flavinl w.l1; CST, drill-stem cast ~or oil ~r ;al .. u,arlr.a: OST. dr111-scem cast daca uporud oy 011 or i.U cOSlq)Any.

~i.llion

".... . -.,--,, . ._c­ , - o ::.=. • 0 z Q • · ~ · ~,

112 2' 0.1 046 18 92 15 ~. 020 6.9 GS ~.J)ort.d :--'le!d on 7-17·36·...... 50 gpm (U,JOO bvpd). ADdYIU 1I1c1u4.. 0.8 ppm ~luorld •. 490 21 .4 710 )84 )84 14 . /) 962 3.9 GS An.lyai.' i.nclud•• 0.5 Opal tluorld•.

.;,.(" 40 JO,956 )1.950 1/0 . 14 i _0 C:.. SMl~l. collected whll. dr:lllni wten "0 ..0 11,300 37.860 11 .1S 8.0 Cl Do 36 40 1, B40 ll.ll] ]~ .~: ::~ ~~ Do. 16 40 :. ,S'oO 12.093 Do. o ~,82~ a.600 13.568 ~/ .)0 7. 1 ShO

566 3,607 - es C.rbon dioXld. well ...... t.ar s.&allJl. ~ .. dad frOft! hole ce 2,J20 feee <.lnder pre.aur. 'y lJ.~nl t.ellllDer .. t.ure ob.erv.. t.lon ttlaChlOe

8.400 U,lOO J5.778 .26 1 1 CCL

1.346 38,3'n 6i.169 .ll i.2 eGL OST ;'-A recovered 0.]50 teet o~ silgnel)' iUS)'. si1.ghtiy mudd .... utt "'aear wlt.h cr.. ce ot 011 and sul!:Jrous odor 1.llO 101 "66 e .280 J ,260 2.810 19 .5 CS [)u~ weU. )0 het d.ep, .... n.. i.yus lnc1udes 0.2 opm ttuon.d•. 1.&40 42, &00 13,653 14 6.5 C1. OS! :!. r.cover.d .. )0 f.et :)f he.. v;.t g.. s-cue ~d IC.l.t"Don diox1.de) and 360 teet. of ule .,.. ter. 9.700 (1) OS!] recovered 80 feet ai slightly .lIu1.tur ea.-cut ~ud. 90 teet of _u1.fur water-cut ::Iud, and 450 feet of sulfur ..."'ter.

':'4.000 C') OST S r-cc.:::I..... raa ;::70 ~ee: ::.! ':"$ '.::: ..rOon c.:'oxlde) and "a1: w&cer-cuc 1IIw1 and 1.910 ieet of jAa-c.ut (ca.rbon dlo~lde) sea "'aur :ri:Ml D••aree(~) Fot"IUC1.an

l) , ..0G i8.000 29.200 6.5 PL A.n .. 1.vsl.S Lnclud•• 2.410 PpTll ma,nesll.::J1 ..s :':'lagneslum carbonate and 180 :I;rm free :.arh.::lf'! C1C;-:lj.. j-:.000 is ,':00 38 . .:.00 6. i PL Anaiv5lS :.ncludas ':.&80 ppom :na,n.llum 1.1 :usneS1WTl careonactI! and 210 pllft fr.e C~l'bon OiOXlo.e 10.':'00 88,000 51,no 6.':' PL An.a1YllS includes 3,620 ppm lUsneslum .as IUlJnel1.UIll carDonat...nd ")0 Ppll fr.e c ... rbon cioxide. 642 8.900 Ii ,249 .40 7.9 eCL CST 2 recovered 30 fut .,t .,.atU-cut !:Iud .and )60 teee of ..,ater. ;,i12 29.000 54,624 166.8 eel. OST 5 recovered 1:"0 [eet ... i mud .anG 340 feee ot salt wacer

- (8) While dr111i.ns "'tc.h ai.r .an utlNud n.:J'W of. ;0 :'arrels of ....ur per hour (50 gpm) ,." .... prod.uc.d frOft! ttl. ~.. va~o 5s. below 1,78.. teee. The .an.. l""11.I l:\cludes 10,000 ?'Pf." SOd.i.UIll chlGrlci•.

16.000 (8) OST i recovered 00 faet o~ r .. ~·nole HUH: and .. 03 teet ~f emulsified mud and b1."CK sultur \Jater sliihtly ~as ct.;c,

:15 ';',710 , .120 3.0..0 GS Reuort.f!d ..... 11 deptt. ~30 ieee Anaiy'l.' lociuoas 0.:.. ~Pal ooron. I_0 3~ • 985 9/ .20 t.O CL OS! i recovered 1..0';:0 teee ;)i na ..vv ga.·cut :1.ar", sulfur ''''ac~r. 721 ieet. ~t mud·c:.lC and heavv ~as-cu: sulfur ""ater. toO teet slq;ntl11 ~as .and ....t.er-cut mud, and :',20 teet of mud. 200 22, i20 ':'9.902 91 .Il? 6 a t DST 2 recover.d 160 ~eet ~:: moo, .. SO ieet ~! S~liht;':; Sti.i.ty "'a,ar, ;:iO feee :If I"s­ cut .Ind l.lilJhC1v ~uQ-Cue waeer ;0 :9.110 51 .888 .U6.0t OST ~ recovered 90 Cue of !:IUd and ),366 teet of sde

lB'. 94 18 97 29

320 Ib.lse ~I :0 ;.'s Cl os: ~1 acovend IBO fut ~i Mud and 5,t20 fu~ .;,f sllgntlv ultv ",ater.

300 ':5 'io6& 50.3':' ) ~I.ll 7.0 OS! ., rec:)II.red )00 feet "t ::lud .Inc ~ .160

1..5.tlOO ~./o. 25,700 2,100 2,0]0 91 8i 38.800

l.120 ~, 750 .7 i. J50 510 92 31 1,000

2iO ~ .340 .0 9,410 100 96 91 t ,300 7.8 S

... :10 )8,aOO C1 72 .00(1 S .470 ?, '..70 91 112 84 .600

11,500 2i .334 .34 a.l 12

1.~)0 lb .3 2.:50 1.330 1,140 :.3 ::',550 8. '" GS Anal ys1. lnc tude. ~. i ;Ipn1 fluori-d•.

517 1:,900 22,584

t,"b 2.800 6,880 :.120 2,120 6& 19 17.100 "."e5 Andysu include, 0.11 ppm boron, 0.6 ~pm fluonde, and 790 p~ hydroxlde. 299 :.240 5,510 l."50 1,:050 :'0 19 tJ ,400 U_l GS Analvns lncludu 0.14 =,p'" baron. c..i ;:qml fluoride, .nd 527 ?pIII h.... droxide 60i 612 ::. .1)90 24 o '17 70 Analysis ~nciudes Z.O ?pnl ooron • .:, i ,pm fluoride, .. nd 31 ppm hydrOXide, 3,:00 91 .04 t~~ ~~ :,':'00 19~ ,400 27,28] OST i rolc.overed 173 feolc of r.Nd. at feer. of \lat.er-cut mud, .ane 118 feee of ~4dy ".leer. 100 55,SOO 54.525 9/ .04 5.0 IcL OST a. recovered ~00 feet cf I.l... ceracut :nud and 5,iOO feet o! ...It ...... ter.

I Z, .. Ie .]11} .. .:., JOO J .... 20 · ~ )0 19,400 GS The geyser is an "poen ..oandoned 011 Calt wleh a carbon dloxlde dr1.ve.

. J90 10. :l4 ~ FS •.Icar sazn~i.a from drlll ?lpe .00.... well oacker . : ,112 3,4;';" FS Water trom "1" bed l:'1 coal HInes i.n upper part of Fenon Sand.stone Member.

'. aoo l.200 L8 ~,':'SO ~,120 2,020 6) 16 8,990 .4 ~S An.l1;.rtl. includes 1.5 !'pIII boron and 0.8 ?J"'l fluonde.

'. ~10 1)2 ),31f) : .810 tS.. 40 5.0 1",)l.O .1 FS Analvsu lncludas 0.0 ;lpllt fluorlde

- 53 - Table 3. - Continued

~. K

?'t'oduC:in~ ," ,- !.oc:.~iol1 iL , ~ ~ ~ ::'rm.at1.on : :: ~ ~ , . . ;:-­ , , ~ ~ -~- ~- " Q" 0 , , ~ " ...

!5S 19£ C ~.IOE-\: Z7 a P'J,rf!: ail '::0. Mi.Il•• U.DP1..ut 7.l'lO JS't .:. "LJ J.osz t •• ~.d. ::'ocu :S5 20! lJinpca i •. :"low t11

2'5 ZU: SEtsE~k W 'J N£u.OnA.L Park N.",a,o s•• At. l24 !70 12-U.-'ia 67 12 II !l 75 S.rvt.c.. Wi) 2SS 2U:: S£~.t 26 IJtngac.a :is L'O Flaw 1J ,0 ,S mJ '0 10-1c..-]) 20 16 5.7 ;0 16 19 LO

Cucler ~. l7 .05 ~J5 50

!tu•• i. ••1PP11.A 5.002 ~. ')06 5,4.21J­ )ST 3 It· L5-;,o lOl l,072 tad.. roc... ;,iJO

Oevoa,1&a. Jad.. 6,Z20 6,672 'ockS &,JOO- C...orua, ted .. 0.672 .s. 704 :Js't Z 158 r~c:lu '" 255 7( C:.t: \:SE~ :0 a Shu=wa., N.&v.]o 5•• 5Z 176 .s0,-50 o~ . i 7 1.34 ~C1n1.l._ '';i..nlJAca :i •• :,1;') l,i7S At L.~50 f,- ·3i .:t. ~!:1.ni:J.i ":.,)r,;". Chil1la E'm. ~.515 1,76J 1.~55-«l !. .)7 ,50 Ju:ttr., 'Jell Enc:.r.ad..(!) i •. LO-)0-58 5q l. 3

;55 14£ C :Nid'fW": a Odusa ~.cu· M1•• i.u.L;:l\naa ,5t7 5,6L9­ OST ll·· 59 l,J89 117 J.lt7 r .. 1 C.lS Co. ied. :ocu ), i30 ~5:i lOot: C 5:.'.....slJ~ JO J Humat. Ot. 1 S .::J60­ ~ • 1&0 ana R.ti.nlr.n'l '0 .; ,":ul Co. Z()S l7! SW\:::SlJlojtW-': i 0 Supertor IJU <0 &.OOL 'J.JSO­ j~e ~~ l~·IjZ loO 1..1Q! 1,860 Co. a ,:"lQ :t.m.C'Ks

6. lSO­ •. 3 loa 2.]81 ".J38 .; .4l0 6,~ 10-06 ice t· ·.,z n,i88 ;lamacb JST ~ 1- -62. no 1,021 3,922 t.

265 tS! 5,,"!\:SH ' 0 Pun 011 CQ. <. 'S. H8­ OS"I 1 LO-LtI-sa Jt6 1,,)86 :65 20! S'I;:;!

M1..i.•• .Lpl»t..&n 6.110­ OST ) l. US lJ7 1,6l0 1. ied. ('OClt' ';,1..JO Enc.r.&da is. s•• ?um.oed 17 :75 LJE l'Etm:t "I 'J 3ureau >'>C I H ~n.'.·l !t.acn&rit. I L~.nt...nd

_., ,'~ Ie·...""', ;~?''''';c' I : ~ - 3C ~1.sS1.jsi.~OL"'n ".390 ';.54-1­ )S! -02 1 :'00 ;"1 )I Jed. t'')CiU .;, ':IdS J6i a C~~;b.nt&1 i ;0 '),71':· 12·10- 5d I 1. :00 512 .,)00 \)0 ,hi ,=". 'i,020 I ::'$ 14(; ~'::lt'::i"J.t 3I 'J C.:-I. :ranz l'r.an% '..;.ll N.avajo :is. jaO·QlO to- )0- 58 I !Oc.. I"l :.t !is It.[ :itbW"CfW-t J C.leee" ,)1.1 Mouo.ck ~a)C'. :.1J5 3•• :.2· 3·;; l4 :7 l,380 C~ • ,~~ Chicle rna. :t...rk.

2;'5 14(: C S"JJcjw.lJ; ~7 0

CJC:;Inul.O Ss. :!..JH 1,)90 5... 108 :temar\u

MiuL.ul.ppi.aa t.ZOO L.701 l, J30 tad. C'ociu liS Ut C 5'J~-t 35 0 C.&r:ar 'J1L d. 5, L70 i,IJO- ~sr J :0- .. 3- 56 l.120 J.LJO C•• 5,.tO lTS 16£ :l\l~:;-tf(!.\: JJ a SUpU"1QC Oil 12-1l d. 5 . 779 6,'l5 5.394. ast 3 ll· ·ol t. :00 !.ol8 9,tOa Co. i ,994

3. €I,271 :1ST 3 JZ9 86. ;04 1.00

z:-s 21E S"i"=S£'!SJJr ) a :ll.Sl'ol. au ,. " t!3 ';' 150­ ~st 5 t- -03 :.000 ~c..] J6,LJl md :t.t~i.n, :i. lit. Co.

do 0,360 7.J':" 7,OZ.3-aJ 'ST U-tO-.;Q ~60 1.J6O

a ~.nn.ca OU 7,078 7. ~OO­ CST l- -)1 .00 "to l.tn ClJ. 7,lOL OLd eec :JeU r;nt.rada 5•• 1'lO· 320 15 14 lIS

- 56 - :1I.1.111on

! "o

23t .200 ]6i.';'7S 20£,406 An.ai.YllS lnclud.s '....391 ?!'1fI boratll. 7J ppm hYdrOx1.de ••nd 76 ppm iron .nd ",iunl.1num oXld•.

249,600 397,601229,)01 Analyns 1ncludel :,362 ~pm oorue ..nd 160 p~ 1ron and a.lu.1num oXld•. :lov.d salt lJuar .Ie. 1,000 to 3,000 :'",pd (JO to ~50 Ipm) trOllll July 3 to 17, 1949, fro. .. dnch of 5.792 co 5.0396 !ut. IlJI ~ ,70 123, iQ) 202,907 ]0.284 ~.lO 0.5 SO !:1ST recoveree 500 teet ::Ji :1\l.:ddy S.lJ.t ..,atu· .Ina 2,670 f.lllt at laic "'lIIter. Analy.i. i.ncllJde. 0.0 ppr:l $uLfidlll .. nd ]4£ p~ iron .Inc dUlll1nun ox1dlll. .:.57 8.0]6 13,910 • GS

806 ]1" 140 70 8.5 2,030 7.9 GS Ana ly.SlS 1nc llJdes 0.02 ppm jor-on, o. J ppm fllJonde, and 0.00 !lp!ll tUnlllne...

'4 517 GS '. ,3)0 20,070 GS

285 .2 914 718 247 10 .0 1,380

J ,090 __ .670 ]1 b .;. eCL OS1 rec~vere.j j.2t..O feee \34 barrels) of salt waeer.

?5~ 10b.OOO In 905 06 6 ..:. CGl. OST recovered i, 150 feee ~f :Jlud-cue salt w.. elllr and i ,000 feee of ,ale water

].784 60 i : ec'L Estlln.ted wolter ~low ~f :00 i.lil::ns Del' l'lour (J ~ or 100 bWCld) eneouneerecf whLie dnllin& beew.en Z•.530 .n

:.086 116.000 191,)44 .05 b.g eel DST 1 ucovered 651 flllee ot llud .nd 6,929 f.ec of ..it ",.tlllr.

:)~, 224 22e,517 as 7 ; eGt !J5::; ~l!c::'·.. ered 668 teet of ne",'''''' ~.s-,:ut ~d. }Q.:. feet :Ji

, .. _u ~q . .;00 It,..... :'78 .0005CCL . ;7~ lOt ,000 166.549 06 6 5 CC" Cluud'l: "ellav '-I.t~r ..,Lt~ 1ron oxide .,rt'c1;:'1::.elll lC ~ 2 .:3 ;:63 l42 ~5 2.0 530 3 GS

]88 759 3010 U8 47 "- ,LOO .9 CS ·";.ce:- p\Jlll.p41d from mine ,~? .It rat.e o! JOO j&l1on. !lar day (0.2 ;pm :Jr 76tlVp<1). An.&lysi.s i.ncludu 0.04 ;:''1'"\ boron, O.~ ppm fl~orid •• .Ind 0.00 p~ manpn....

8.2 2010 148 11 3\6 8.4 GS A.n.aiyslS include' 0.10 ppm boron ana D... POII' Huon.dlll.

64 .5 £.ti 42 69J 7.0 GS

,. Je0 2.l50 1.~60 LJIO 11 1.0 2.500 8.4 GS ¥lodd on lO-27·4lo "'.. utllll.illt"d .It 5 gpm n70 bvpd). An.lysu indude. LJ ppm fllJortde 526 5.750 556 1l~'62 J 3 SO OST 1 recovered llO teet "t 5.9 ,ound water-cut :nud. An",ivsu l.ncludes 0.0 ppm sulfide .nd 90 ppm iron .nd .. luminUlll oXl,.da. ~.58 7..:. SO ;)57 • r~COVl!r~c 23C het ~f mud .Inc i ,)':'2 ~eet oi ;,l.aclc. $ul:u:" ·,,;.tcr. Anaiyus InClude" 0.0 0P"' sul:ide .Inri t~ iJpID tron .tld .lWftinuftl oXl,.de. 1:'. 999 ~.::l4l d'" 0 SO :.l~L: ;lUlftp'l!l.0 'DIll su i f'i.dlt ~nd 1) ;lent ~ron .nd aiuminWII oxid~ 18 , ~ 25 61 : .u~;'1 ~( SO OS! ~ recovereo B5 feet of lINd .Ind i,'::5 feet of ":ll.ck sultur ..,at.r. Analyu.' ItlcllJdes .. trace ot sulflde lind 0) pp1l'l Hon .nd alwlILnU1ll oxidlll . '4 l4 4)7 ]40 43 l8 . 8 700

: .0;;20 ]41 n 7.0 CL ;)ST 2 recovered l80 feet JI lll1Jd. ~]O feet of !1u..1<:i-cut wat.r, .no ~:.O t.lllt of br.clcllh

) , ~) 1 85.000 t':'7, )1) 077.: eCL OST ~ rec.overed 6,900 fltet (~'5.) b..rrei.s) oi s.ie ..,..eer •.. 1.Ch hydro,en ,ul..fidlll odor.

1: [,9 288 254 GS

:.0 18 27: i 7 GS 5!'ring 1S urus of seeps in stream bed. AnaiY.lI lnclud•• 0.3 ppm fluoride.

:: .J50 ~, 990 D.lIO :,950 77 )6 • GS

).900 105 41 "::.360 ).840 ].510 16 2.4 3,640 7.? CS ;It! ot .loiter .t ;l0int of col1ec:'1.on ..,•• 7.0. An.lysu lnc:lud•• 0.2 ppm fluor1dlll.

980 ]6 :.~ 3.500 2.lJO 1.0 l,l00 J.a es O.peh of ·.eU 1$ 290 teae l,11.CM cU.Lnl pertor.cllld from ZJO to 290 f ..t. Aeoorud ,ale 1;, M..rch ~953 "'illS 360 i:Nod (11 §pm). pH ot watlllt" .. t ~oint of colllllcc1on was . _.... M.al.yslS LnciudlllS L." !I'Pft! fluorlde. t2C 124,9&0 "09,682 lli05 7.0 a.. OST: recovered 290 t••t of w.tar.

~ ,S-4 3 7,300 24. ]18 .36 7 6 eGL OST b r.eowred ].S70 feee of mud-cut s.le "'at..r and "alt ",..ecr. 5.88£. 9.:'00 23,9'-3 . JJ 8 i eeL OST 2 recovered 60 feee of lIIUd-cue sulfur .., .. ter lind 150 f••t of IU"fttlv ' ....cue sulfur Wat.r. Samaie "'•• clear r.dd1sn-brown w..elllr frorn 10000er ..art of coluam . 3,31i, ~5 ,000 30 •.D4: . 26 6 eel. OS1 ~ recoverllld 5,460 feee of lINd-cut sulfur ..,.. tlllr .nd sulfur wlllelllr. S_pllll 100'''. C LIII.r water. ]94 8::' /:1.90 5 eel. :.le~i ~s 720 feet d.lllp lind ?erfor.ted from. 080 to 720 fe.t. Rlllportad dlllpCh co water .., .. 650 fuc 1n t9S6 .

~, ZSl )4,oao 94,obi . 88 6 9 eCL OST ~ recovered t ,470 fut of IT:udd'Y salc water .Ind .:.. J'?~ fuc of salt ..,atet".

z~, "JOG :'O.bt i .20 .6 eGl OS7) recovered ~80 fut of Watery mud, 900 tnt of muddy .....tu, lind 4,550 fut ot .,i.ek. sulfur w.t.r.

:, ,000 tS .052 .2J 5 5 Ct OST 5 recovered 50 rut of mud. 450 ieet of muddy wolter. And 5,130 feoec of ••It 31.:15 I' :.250 zeD .G • ,04;) 050 295 5,080 7.9 GS AnalvSLS includc' 2.9 p",," boron .. nd 1.4 ppal fluoridc. Table 3. - Continued . !.

jill. t/ '.l lJ7 ~lIImark. Roober'1 Raa.e C...C1IM.L ::11. ]4 dO O.Ot 54/ l02 20 ,:", . .:. 2C i!'nnll LW Blu.e Jabn Encrad.& S•• )4 do .01 ,. 8) 5.2 21 5pcUl~ liRi ,c· !!5S UE S!~E\:S£lc; 29 5 Cr~.ry do '0 ]0 II ipr1nl 28S 1St :iW~t:i\lJc 12 0 PaD. .~r1can l MlU1u1~pi..&n 6,092 5 • .507.~ OS't 'j 1, ;J4 l48 7,078 p.erol.... sed. ::'oc.... j. ,52· ]ST Ii L,563 )98 ll,J'" Carp. ) ,d23 .; ,lJ4 ~.420 ".J91~ ;,509 MC'Crac.k4ia Mbr. Ii. 420 6. !ool ,)f Uben i_. .i •• C..ar1.aa sed.. ".4.62;'.509 l ...ru JST LO ;-l2-62 • 2,364 91 :oc.lt:..

2SS 19! S1oI

!3S 2J£ 'lE\:lIlI

~...vaJo S•• ::to'"' 5-21-')7 4a i.b .01 .l!( !9S 1.,t SJr.iE~~ 20 0 Con.t1Mnul !'U.Ul.u1ppt..a.a ';,603 6,:;35- DST ~ 10- ':'-58 :.1.00 >Ji.l Co. s.d. roclu 6,346 .' 295 20t.: ~1:,ktNio;SV-t !., ,J HtailIL. OU do ,:",z06 4.565 4,J34-44 ::ST 2 .uld. 1.ilc.i.4oi Co, Z.9S Zl.! ~!;SW'.(; l3 a lure iJU CQ. do I),J96 'i,no /j.'-IO­ OST 2 lO .. ;-lit 2.365 ,)2 l, 6,540 .;iZ·';2! II l!!01 ,6 Co. 29S 26£ N1oI-lS£\:St< a Superior au t··j Cutler !'so 2,512 3,512 '.126.. 94 5.. nov i05 lJI ,12 c". Il....rk. M1.Uiu1poian o t1.)l.O Ll,"-) tl,:..o6- DST l 2'20-64 2.360 '-2,34J Z.lOO ud.. rock. tl. S57 S~ri.all )4 HoW' 3-22·57 ':'9 i.3 .!i~oo :..) II l.l French N...vajo 3•• m:r LJ )03 ='-l SC:\:: Zl '. Wt.n1aca i •• 5- ",-59 l2 II 11 91 JlS ::.t 5C:~E\:SP;~!7 0 C~ll.!~rnh. Xhsi••t.;J'l'144 ;,508 JST 1 11-27-61 t, .i.79 1,,zS4 au ':<3. I.d. r':)cks '" Wt.n~.u S•• 100 !lo,", ';-,0-57 S4 ~.l .0t ;~ ,8 ~o 3.5 TW'

Wver :toC't!1 :ioenkO'l'l (2. do 12 - ~ 5a 20 :t&cch St;JC'inll ]15 14£ s..,~~ ]6 S :'onco l'l.Ul 5hift&r1.8" :ibr-. 3- '--58 )6 52 J78 Hee iij:lttn, at Chinle fill. llS lIE t'Jo-iip. K.&y.nu Fm. II do ,. ,16 J6 lS ,6 $~C'inlC ~ 3lS U£ ~RlJ.;s!:.f1fWt ~lJ a Sllopo«ctor au 22~l9 1,/50 l,lSO 2,3J9-04 JST 1 12- -58 t ,076 i.t.,3l0 C<3.

- 58 - J .0 6.10b l1,751 " 112 0.1 6ao - cs ~ )) 4' l.' 762 ".4 GS J6 12 .a \06 12: .. " 2'8 a.l GS 15 t2 .a t64 GS

ZI .5 lOl 168

2.6 ')1 542 3a6 28 l.S 1...00 7.J CS AnalY:HI ~nc:iuQ.s O.Otl ?Oftl ooron, 0.2 ;ltnD. fluondc. ~nd 0.00 ppaa c.an.an•••.

Z.925 )16 7,279 1.~80 ll{ .56 7.4 ShD Anollvsi.. l.ncludu 2.0 Ppn1 aamoni.UIll .nd 2 ..pm ooron. CST) recovered 3,890 fuc (54 ';,a1'·1'c1.5) of ...ter-cut :nud. mud-cut suHurolU water, .and sulluro~ 101&[.1' wi.th .ali.ni.;:v :Jf 1.1.60 9lX1l lodiUl%l c.hloride.

20; 3:50 ,3a 6.142 ::: ,200 -~.6J 7.3 ShQ ArI.aiv.!ls inclU4u ~ pp:r: .a:mlOn1.um .a.nd : ppm :lotor:. OS! 2 ncavered ':'.540 feet (60 o.a.rrl!!~s) ,Jf :tlud-cut ..u .•r .... lth • U~~1"!iC~1 :JI ~.J2,:) :Jpm s~d1UI1l chloride zif'/320 S.;;' UC An.a.l'oslS ~nclude:!l ;:::l; :l~:r. "I .li.k.alu:l:y .1.1 cal:::;.1.0!1\ .:arl)on..t. -:',079 12.1 \:.C "".11';'11.5 lnci..ue..s ~.an ~pft of ,a.lk.lln1C"· .s CalC1Uftl c..roonaca. 21! -:C. ?97 5 1.:C Anal'I'HS ~t'i(=lud.s .. LG ;J~ oi .. i."all:'1tC" "I ca:"clWll carbonat•. 0... 2.150 ~.500 1,320 . 8 2. no 8. J GS An.lysis ~ncludu O. 9 p~ £luCInda .

J .004. S.~O 12,767 .62 7.5 CGI. OS: 2 recovered ~80 fe.t of l!I\u3·cuc su1.fur .....cu .nd 2.5~~ tnt :Jf suLfur ...... c.r.•

2bO 7. )61 2(:".:. t..0 Cl.. ,')s~] ':'l'c':)verel1 ~,:llS ie~t ,)f ,~tghc.1~.. mUCI-cut "" .. ter

:!oo '.9 880 33.061 DS! }; zccoo ::0...· .:: ~as l:T.lec:,. .. t"';.·, tnC:'t' .. .sUHI :0 sCton~ ~n ~ :unut.••• !lr.l1d :0 sur:..c~ ~(' • 'II1l"'uta;.·90 Dereent ':".tet :0 ;J~reent I'mJd .lnd ..u!h.ltic residue rlo"'.d "V he.':.s. cnan~ec ,-C' smal':' u:r.. "· of sulfur ...·.ter. :lSt ! r~C~\I'.rifc :.50 fe.t :Ji ..... ter

:..00 38.906 b6,082 :i~~l 0 Cl DS" 5: ~C'od ~io"" of gas l:TftICdl.ately l.nCt'4I' .. uni thrClu~h Ce.c. fluid to surf.ct l,.n ]5 m1.nuc:cs ,ao 8.09io 1~ J8 7 5 Ct OST 5 recov~r@11 : . .340 fut ('I: sulbr .... acer; 'amole froaa bott.om at fluid column. Samples ::-om lOO .Inc! ;'Iilddle ,Jf flu.l.d column cont.ined 39,876 .lnd 21.242 p'Pftl of dis.olved sodds., :'eIP.C:Cl,.vcly Jac :,:)5 i,i.:':.! 1. ~ i ,J CL OST 3 recovered )00 fut ,Ji muddv ..... tn .and S,OOO f.et of ,li.!Jhtl~· ultv su1.fur ...... er :90.000 :!95.000 Z10,OOQ 220.000 160.000 4 ... G~ P,OduC1nll: formaci.or, rl!oort:ed to b. "C..ne Cr••k HembeC" "f P.r..dOx Fonaac:ion.

;'.1. l37 L4) 16 Jlo ~ GS A".lvS1S InclLld~s 0,07 pam aoron ..nd C .• ppm fluorid•. I 3,391

,:10 2.7JC 28, 0.0 DH

: ,':138 89 7.a CGt OS!] recovered 5..0 ieet vi ...... t.r·cuc mud .lnd :'.920 i ..~t of S~ightly br

"'. 0 ~. 0 J~O 67) - C5 _".1.1 .:lr .. ~ied 1.1'1 lQ35 to ;Jepth ~t 19~ :ut. c....d :., ;')6 if:tt~ d.pth cf w..ter U'l 'lovemoer l~)5 w..s '20 :I!et

J:c CL ~ST ~ recovl!rl!'d sso f.~t ''';

.l • ~ GC .00 . .;.00 CO ~s: :-e-:-:lvere'::l 5.510 feet

. ~JC t, IDe ,aa 5 Lno j" CS AnAlysts ""cludes <).5 opm !luonde ,ao t..: 8.6 Cei. SoUltOl~ co11.Cc:.d .... ~ch i:lot':..:-m :If dr.l.L hole ... t 2.250 feee ~n the :,,\oenK001 :ona.elon .. ne .. ~.acit.r .It :.~:'~ !lIIIet 1n Ch.lr•.i.a FOt":ll.e1ot:;; no"'ever, ~o••o... ck !1.ftla.r of Chlnle Forr.'l"C.l.on u reporteo "reduc1ng :eM!LItlon. CST ~ecov.red SlO fe.t of mud-cut :'relln ..... t.r 6.Jll ,266.0 CL OST 2. reCOVl!!reCl ~.]e~ feee: -:Ji :1luddy frun w.ter

:so ,00 I- l.50 10.5 RM£ lncccv.i t.sted '.. as trom ::,JJC teet lon ~o.nkOo\ FonLacl.on to ~,J66 teec ;.n Coconl.no S.and.c:cne; hO\olever. che ~oItter !"rmaticl". the tepot'ted :rroducln; f.,rmaclon, !lst ~ C'll!covu'eQ /.lSI) ieet .:f ~UQdv :::-est1 ter . &-:.0 :'3.500 30,179 . 51 -: J R.W;£ :JST.:" recovere.d ... 500 tut oJf ..... l.e~ ... nd 10C teet of muc..

3.240 ;, .5iO j'1 5.0 Cl. !lS'I' 9 r.COViUeC ';'12 fut -:i dt~l~1.nl fll.ud ... nd J.Q~5 fut 'Jf orac:iusn ..... ter .... lth sulfur odor ,~ che t .. tt 190 feet. :.200 15. ))C 29.129 ~ZJ7.0CL OST 3 recovereci 580 fee.t oi ~raclc.i.sn mudd" w.ter ..nd ),b53 fe.e of ~r.CJ(ish ...... cer 5.amoles from coo .lnd :uddle ci recovery column concnned ZOJ.592 and 72,~9 :::Ip!n ot dissolve.d solids. resgectlvely. ~ ,200 ,000 JO.G~2 .05 7.5 eCL Lnterv.l teste.d ...... :rom .,.260 fe.t tn ?enn.ylv.nLAn rock co b.':'OO feet tn ~iSSt3S1o'P:..n rocic.. hO....f!ver. tnt: ~.ttar :-ocl< ..... 5 :~~ re'Ported :lrOl1uClng fonn.,u;ion. DST ; recove:-ed :,::; f~et of ':ll .. ci<. saltv sulfur ...... ce:- ~4 ,I .:.....0816.0 C1. DST 5 r.cOvtre..:l 3eO teet Jf Sll~ht~·: uS·C'Jt j:-:.l~J.ng; mue.. ;:70 !eet JI highi.v '.· .. e:e.r­ cuc jrl~lin~ mlH:, .lnd ';','HIC te~t cf £ .. It Wolter ·.. ttn 'uUur 'Jdor: s.I.lIlolll!d ~u.t "oav\l' tool.

: ,tI()O . JO, ~64 2'/:08 .0 L !JST Z reCOvered .. , [H·t::! bl..ck ul:v sul:'.Jr .... ter; s&mpl'l! :.:=llecte.d ".~OO ieet from ooctOTTl. , .:00 _. ~ 30 7, ')4) l.05 0 L DS': 2 recovered ,200 fe.t of ~resh ...... ter l.:'l .:..5"l,.ncn ::l.rlll plpCL

L)O .00 71 5, - ~S AnalvslS l,.ncludel -1.7 ol"" fluQrtde.

- ;) I - Table 3. - Continued

, ~ :..Jcac.ioo. Pt'Od.uc.n~ ~ormaci.on ; ~

...~ , , ., ~

J15 !J! Nloii: 7 'J R. 3,a1lay '\It.npCII .is. lO~l5·JJ 5l JJ J2S l.lE SW

))5 U! lZ 350 10 .04 ~5a 36 '0 :5(E) JJS t6i! t9 5 Cuclu' Fill. 12 :00 '10 lJI ;4 t6 lW(R) )JS L61 t9 5 Kllmo•• Cr. ~S :00 do to- l·;.a .t 1.6 :3 lZ (",jO(il) ))5 lJE Nt~ tsEt)6

Entrada S•• l,'z-S6 ~,QdS­ '0 lOl ; 1 t .Z56 ~O~~~ l.JO' l.6aS ~,JLJ~ ~ Jo t9 l,&]') I 30(R) S4 I lJS ~~c:: N"....lCrt: :sc:!t 30 'J jo Duae. S,t • .lnd. 1~5 H9 20)~Jlq jo ;9 LJ 'Z .S 3urr:J ': .An von :!ft. do do t59 HS zoa- H5 jo a. l ,., ]JS IC"" S~

., l; 3)S 2:.C; Ntol~.l:ffE~ H 'J jo Cakec• .is. Uld. 20Z HO ZOZ·JIJ '0 .,-l6~35 • to OZ 17 .. l.J 3ur':'o ':4.tlyon :111. :1ort'],soo. :lll. no jo Oakoca .i.. J.nd. ZZ6 L.i.2!l !uC'ro C.lClyOft :;U(M) :2. ns 24£ SUJ6"JJa.iW.lc J1 'J do C~oc... SII •.uu1 n, lS '.l 2..:. lurre :.anyon em. l'loC't'uon fm. )[1

Jens.n ) Oaito C... S s. .Ioftd do 3~ ;.i3l )0 U j 3 'J 3urC',J C.lnyon 'Ill. }4S 9£ StJ~c1or O'LL Whic. ilL2 i •. 5,d32 ~,2.S5 3,dS8~ 'JST l u. ,80 115 c•. ~bt" . .:It Cuclu' S, ~qt :-tl1. MluLui.PPUA },240 ~.55S· ilsr :. ; .. ·oiL l6 l70 l, :.85 1.d.. r:)CKS ~, 5az Seal:' R.ancn Oakaca s •• HO "ow :. ... 27-59 53 19 i"nn, t'5'('1\) }4$ l4£ ~ 9 5 Or;u. ilock Li.2.Q. Jo _3 •• -:OftlJU. It lO(E) C-.c1.ct" ttll. ns n: c :;V:NE't 19 ,) 'to'C'Q1oI••O ::n. 1.0, :116 3,OJO to, 185­ JST ) 300 194 3 ,'Jl.S I )';;5 3£ jo MoL-..s rm. ';.3)0 ~,')09 fJ.H2­ ~I l'.)- -0) • )b ;S3 ~ • Jdd 1i1..s.usi.ppi..atl ; ,009 ; ,;:2J ,.et. c:"ocj(s JIS " RA,l,.I1y Oay Shi.nar1Jlll, 1'lbr. 10 2.BtJ :iine If Chta.h :~. JSS 9! 26 5 &u.nau "f Cl.ay Soc-to.. lSur'rO ';.ulTOft :'-26-19 58 l6 '0 ~OJ :..&a.4 :ia4Ap" :~. ..nt ) 5S ~OE 1a t6 ;0

)5$ UE II 5 l25 lZ7

~ do :J-li) i~ tt 150 17 5,](£) ; ... 1... ,61 7.5 ;8 :.6 J 55 13E sw.;;sw~ ~""'9Y J.ck lUco :lI. J<.Q J:.:./ n t9 ~1n. mPJ n 0 ScandaU au Paudax tm. S,057 ",098­ ':)ST .2 Co. -:Ji &, t09 Cd,Horn;'. )65 1£ to s !kccs 5pn.n:c 3ucro C_nyoa. ~ 7 Flow '9 ~. ~ l6S LC!! SIp£ ::SE~ La ,') Cd.i.:orni..a. •..·hi.t. il1.2 S.. 3,no ':',245 ),n4~46 )ST ; au ell. ~bE". ~f ':'loC leE"

J ,164-02 1.63

7,201. 1,305 7 ,Jl6~"~ OST ) ) ~ ~ j2 'll 19!

O.vClni~ UQ. 7,305 O,.3l6 3,H9· OsT • l-U-ll t60 t, :'i6 c:":ll;k. 3,Jl4

J6S tJE It 5 :;J. US "ow l6 :J lJ :J

- 60 . milliol'\

..~ .....r.. ~ : rf - u..,,,.. = .. - ~ . o • z..: .., ..o

l44 :. 5 1.8 4.48 67 82 7.J 688 8.6 CS Rlponld tlov on 5-29-62 "'.. 13 IP"I ("-40 bvod) AJ\llylia includu 0.22 ppi boron ~nd 0.) PlI& fluoridl. : .580 19 .2 1,390 1.780 1,620 • 2. 2.1.70 6.8 CS Analyu. incluci.. 0.12 p~ bot'on cod 0.) p~ fluoride .

240 10) 14 142 209 19 1.7 l,160 6.9 CS Arlalyn. include. 0.07 P'Pdl boron ~nd 0.3 ppm Huoride.

l<'7 12 .2 J20 t.5" .8 140 - GS

11,170 1J,954 .2/ 0 . 28 7 7 PA OS! 5 recovered ],150 {eee. of u1.ty su.lfur w.ter ,",8.935 86,102 11 .097.7 PA OS! 6 :-.cov.red ],600 f.et of :.l.cll sulfur ",at.r.

5.090 ~1 ,J02 lJ5.060 9/ .067.5 PA OS"! to L'"eeovered 219 fece ot ""..car ADC eud .and 2,000 teee of sal.ty black ",aur. An.dyu. report 11.t. Mc:Craciuln He1Qber ot ELbut rOt1UClOn AI tCrat.WI yu1.d1nC

... )00 2t,655 42,%7 r'Q.I.l1 1.2 ShO OS! 2 recovered ]80 f.et (2.8 b..rrd.) of ..,eter-eut 'JNd Ind 3,220 feet (2J. ~ ba'Ct'e1s) of black suLfur ""ate!' wic:h :r.aca of t&n"y residua; s&III1'1e c.,aken ,at too1.. 3,550 0'"' ,000 !l0.342 .086.9 CeL OS"! J recoveud 100 feet of dr:ll.i.nl !!IUd, 3.076 f ..e of :nuddy lai.e "'UIt', Ind ':,250 ieee of bl.ck suliur ..... t.r; '1&n101. from bOe.h stand. d2 J7 )19 283 • GS Analv'l1s uldude. 0.00 ?pm boron.

... jOO 52,000 H,795 .096.2 eGL DSr 1 recovend 460 f.et of dt'illinC flu:Ld .nd 5,550 f.et of bl.ck sdt ""aur.

410 16.JJ1 .12 7.6 CGL

ooe 152,:79 .iJ666CCL Soc com .ample.

21,192 . 05 7 eeL SampLe t.aKcn from arlil co 1 L.u!. .

1. .. .;J.i 504 )96 - GS

).0 .1 190 112 lO H5 8.3 cS An.lysis incL:"lCic. 0,1 pl'ftl Ilwilnum, 0.03 P'PGl boron, and 0.1. PP1l' fb.. orld•.

.. 770 1.75 8. 5 ~CL OS! 1 re<:ovcr.d L,lOa f.cC of sulfur ..,.ur. s illJitt 1)' ~ddy at tOp .

.799 "-0 ),720 :~ 5 ~~ DST reeovn.d "6S t ••, ot sulfur water. .9!!9 460 !o .4&7 28 .3 ..... ~ST ] recov.red 828 ~ ••e .:Jf w..cer~cut mud, ~.J80 fe.e. of stighdy llIUd~cut fr••h ..,aelr, .nd 2,i.2S feat of tra.h .....ter

t 1.090 ~o 7 5 Gi.. nSl ~ recovered :.JOO ie.e ;jf :-ot,ar:, mud 'neavllY .:ut IJtch ..... t.r (50 p.rcent 3J,d .nd SO percent ",.ter). ~.5L 7 5 Gt DS!' ,ecovared 1i.]lO fnt iJf slightly :nudd .... fruh ",..ur.

;:''''0 9) 7.9' ~GL OST 8 recov.red 90 feet ot dril1inl IltUd .nd 6.dOB feee o~ br..clnsh l.Iae.r :, ;00 .98 .2 ~CL ~ST 9 recovered .n e.timated 6.000 feat ot brlc~(lsn ...... ter

l.~O .5 GL OS! 4 t'"ecovared ')40 fe.e of water-cut mud .nd t,81l feet :It sulfut'" uater ~.50 .7 GL 0515 recovered JOO feet of .... t.r~eut """d Anc 1,07! f.et of sulfur water.

• ,j)O J ,620 9,130 • CS

:5 10 :.6 159 l6 . 2 lIS ) CS AnalyS1s lncludll!ll 0.01 i='t"ll'l boron .nd O.~ i='pnl fluol"id.e . 231 S,900 ,",0,500 96, )00 -.Oq .7 CO OST .. recovered 900 feet of lINddv Io:at.r end 680 i.et of bl.ck sulfur \later

S, .!.oS ]9,902 7J. )96 I 3,a.:.O l20.000 "'05,067 096.0 RME OST 1 recov.r.d 60 feet of drtllinl mud and 4,000 f.et of b1..ack salt "'.et.r.

105 J25 760 7.5 DH WaL.r collected frOftl kitchen t.~ in AlMric.n Cafe, l.a 5.. 1 Junctton. S..n .l1.l.n C,junty Analysi. Include. 0.10 P1'!C boron ..nd 0.J8 :'prlI fluortd.

';',957 1.1 .8 CGL rour·inch ..... t..r flO'l frOM 5.165-5,194 fe.e; :hen tner••••d to 8-1nc~ flow At 5,19'"' f••c. nov ...... h.d hole cle..n and clear "".elr yas ~o.er'V.a at suri.c. :. ,:50 71 ,'JOO 21,J99 08 .J GL OST J recover.d :,170 het of muddy ""..e.er. 5."01. "'.5 cloudY or..nge w.ter -..rIch ?rRClplt.. ced uon oxide An.lysi. l.nc1uae. 5 fJptIl 11thlUIIl. 18 , .5 205 l6l 26 1J .4 16' .l los AnalvU5 lnclud•• 0.01 ppm boron .nd 0.1 ?tml fluoride.

20 1.0 JOJ '4 4.7 500 .8 loS A.l'\aly.i. inc1.ude. 0.01 ppm boron .nd 0.2 Pp1III !luoridf; ';',2.60 lO."26 76 .8 CL OST t recovered 2.4JO fHt of .l1~htly br.ckish '-ater,

J.: J" J5 528 .... ~S Analy'is includes 0.06 i='Dm boron and 0.) p"m fluorid•.

592 :,355 n6 A.naLYAlI lnclud•• JJ ppnl lron and dWII..

6SC ]02

220 i52 .9 )14 8.:: GS Sorinll is on south ,ide of ridge .bov. Hot"th Hatch Clnyon.

~, 984 2J ,00) .:0),770 4.650 ll~ 19 6.S 0 OST 1 recovered 270 fue of s liaht1 y mud·c:ut ..,.. ter .

- 59 - Table 3. - Continued

!.ocac1.aa t"roduc:.1.n~ ~ormaC1.on z.

16S to1 J4 C.-d.,&£, :i.••• 3... 11- L9-S8 0.01 :ibr. ~i Cu.cler

16S !8E ""

J1S l~ , l ;80 20 4l 10 lO(') l S bcU..... Unl llO do tJ 10 l7 ~ln.iAI Co. 3(Ei' lis t6E ~ Cal Min.rab Sh1A&rua, !'!be'. 9.l lO. It l,6OO 40 ot CM.nle :'m. liS 17t tl S ~.C1o~1 ?ark Headqurcers C.-dar :ieea 3." 14 Fl~w '.1 .00 "8 1. II 19 .i .. rvl,.ca 31;;11'1.0.1 :ibr . .Jf Cutler '('I

l;S laE II x.a.ne Gulch <0 l-lO- ja II 79 .1 )4 :ipc1n~ '0

)75 2l!. NEt:NW-I:' LO ~ Blu.dinl tJ .2.5 ll6 ll4 ll9 10 48 !1tn•• }1S 2c.l ~~1;SW1: Z4

375 2SE ""J.j(EI;sV~ LI ~ do !o i~ lO~ j~ :5 L61 13 ~dS 1.5, :rJ-'!;..'l'E:..-a:t~: 0 Sl.ncl.,ur ail l,JJ4 2,Jl1 2,291. SwaG ,: •• t La- -)1 "',1'-3 ],]79 utd c.. Co. Z,Jl2 385 ZSE SEti"·~1: i '..I Ii. C. Pukt.ns 'ncrad. is. 26.5-;20 S.. !'tow';·t6- 54 5.3 ].4 III 1.9 ae1ft&ck.s

18S IllE '0 ,LZo-m , .6 L7 1.4 J.9 )95 4! :iW-'::S'W~E'c)6 0 Cnat ~••ucn reft.uyLvani..an 8,326 8.700­ 'S! 1 l·ll·ll sa8 ~64 t,321 l,o 'rilllal Co. Jed. t"oelu 1,016 19S IlL , s <:.1-191 te.&yanc.a rna. 14 .04 9.1 ).4 1.4

19S ltE lO S iNavajO Ss. tl II •.J

J9S 13E. E;-SE~E.~ Z'- 0 Pm ~ti.C:&4 ~l.. Fti. .,886 l,OU· I)ST 1 tl- ~i8 S54 ltl 1,/09 t,2. 1lI.c:':2l..... S,1)1 ~

)CIS t!,.t': Chinle :m.. :'t,:,w ",,-29- S~ U ,96 ns l:'~ l l tn.sh Gee.a. \If.R~ate i~. 70 <0 5- 12·';0 14 l4 l4 1.2 5\,rtR~ HE) .395 14£ LO S fer••n W.car <0 L:' '0 II l, 12 iprln" ii":'i(E) J9S 13£ C ~fE ~rw-!: !.:5 a C.a.rter au I Ouray L.a. 1,.10 1.81l p,oll.4J "0 11- ~)4 .lO Co. J9S 24£ WiSE!::SU: L8 'oJ S. t.. ~C.ch Marrt.on Fti. :.~ 4~5 !458.. 566 l...lQ£. 12 II Slutt' S•• "'95 30(R) '0

W Bureau at Entrada S•• DO .WQQ... 1.0 .Ol 12 U3 II t:1dian ,JO(£) A1t'u:'s Glen ,:..nyon Gr. SH ~.t20 .i ... •. i'~. 52 '.J '9 La R..m.rlts ~or-:'ison Fla. '0-444 t70 ".0 :.0 159 J.5 3tu.ff S•• TW J9S Z,Sl SW~~.\:' 30 Y Bureau of In·l.6 lMOC't'i.soft :ll. 12 ;19 I:-oJ-';80 }! :.00 tJ 10 /0 !ncU...n. 'Stu.ft Sf. H9 6ao 130(1\) Albion )'}S 2!l! Sll.l,j(Et:r!c ~O H.&c1.ona1. lark 1" do 1.1 ,. tJ4 l.2 5_"tc. i'('E)

<0 E~cr..da s•• 1.'J80 1,200 i.... Se.. tJ I.l 186 NavaJo i •. t,22.5 b ..cx. ~rk. 395 ~5! )J Bureau Ot ll1~ t63 Ouoe.. S•• J S . nov !ndtl.11 R rk. Aff..irs ;,.()S 7! C 3t~.lc 2 oJ Shdl 011 C

<0 It 1.1 \6 "0 I. lZS :l\.i~W-!s~J.; Wln~c.e :.as 20E 36 /:fava to ipriRI 5 I. J do LJ '4 :.uS Z:Z ~"'J.~:;~ii:~!: 2.5 'oJ City of Butt 1 Clen C.anyort Ct:'. 200 l ,200 i... .L1!2Q. lO 1.0 ,. a...... ru 50(£) '0 :.{)s m: stl:stl:sEl: ,0 St. ChrUto- ~1"Lon BluU 'i •• do 4-/6-41 :1 tJ "tier ~1. ..1oft. SprtDC :.oS 22,!; n-:tl!t:ft~:'9 Il ~o t Glen C.&A')"On Cr. do l-1l·18 t2 ll~10 ".4 .6 84 1.l

- 62 - "i.llicn ... ~e .~ -> .­

17 14 293 -os L2 .4 124 Z3i 0.8 _ GS ,\,naJ.y.u .. nclud•• 'J.O Pp1II fluorid•.

:1 '1.0 .5 210 32 1.4 562 7.5 CS

1,920 1.800 1.7 ?,5JO 2.920 1,910 47 9.5 3.800 6 7 CS Analyau lnclud.a 2.2 PpnI ooron ..nd :".3 p~ tluor1d•.

.16 '8 .7 1,220 816 60lJ 17 1.:' 1.690 7 6 CS Analysu lnc1.udu 0.16 0,* boron and 0.7 ppm !luonde.

~. 250 '70 ),920 1, d60 ~ ,240 .:.J.i 6. 7 ~ ,430 ;; CS AnaJ.:-ous i..ncludu l.a ppm boron and 0.6 p~ fluoride.

~ ,430 t ,270 1.7 .;. ,770 2. .260 1 ,560 42 ~ ,J10 6.8 CS ~onn, haa h:-,ciroien sulfide odor. Sulfur a.pollt.. at sflr1nl. An.J.Ylt. includ•• 1. 5 PpdI ooron .nd i. B PlIO Huoride 20 .0 770 600 .J os

18) e.o 1. 0 414 324 .J 611

109 LO .1 3'0 19) 41 2.0 612

8l 8.0 .0 lOS lJ2 4'6 8.4 GS DO ;.3 .5 801 " 95 26 L,260 46 5.5 .J 204 128 451 S.4 GS

LO 416 20' .:.2 2..2

s.o .6 45J Z20 )9 1. 9 685 :.1 GS AnaJ.:-osu .. neludes 0.01 ppm "::oron, 1 2 p~ ~~uor'l.de, and ~ i ppra !llAns..ne•• " M...urlPd :./uld 0" ;·17·55101" 200 in'" (6.aoo w~d); ..... tel' cont..i.ned 416 ppe af dlssolvcd S011ds. 13S i.5 ,2 )q .9 7,1 CS S...ple collected de.:- i 5 hours ot ?UI!llU"i. An..lysu .. ncluQe. 0.10 P1'lB boron and o. Z p.- f luorid. 5.0 .1 291 " 75 ':'.9 !.o6I 64 ':'.0 .5 292 " 76 to. 9 :..74 i.5 CS Salll,:Jle coi.lected dt.r 1 hour of plJlIl,:Jlng.

,) 190 '4 76 5.0 7 .; CS Samole colleece-G ~ftlPr ~ nour, .,t .,umtHn@:.

2)177 b'; C.. OS! 2 Cl!covue-d 4,679 tetC d fr••h loIuer

3.'::'00 ;. '5' ill 12 7 a CL OS! .. reeovered 2,400 f.ec of fftUddy waul' l' L99 14' '6 .J )lJ .8 GS AnaJ.ys15 includes 0.07 ppm boron ~nd 0.2 ppm !luond... 4' ~ 75 318 14 .6 647 6.0 GS A"'alvs .. s .. nc:udes 0.08 pm- oOr'on iIInd 0.2

.,00 ;, S83 ill 9) j c;" DS:) recove-red l )00 f •• c ::Ii sul.iur wac.n I 900 : .:l.Z7 ? .J7B :'~-lnr:~ .~:1er sec t::. .~~Z teet; 5""aOotd :'lours \.lP'Ul nOH~), recowred :::: barrel.. )f ..... t.er 'Jer hour

J .300 : .040 :. •.540 ) 7~ 94 64 iO. 9001 .aeer ::'0l'Il ain. sump. Analv!li l.nclude. 0 )1 ;Ipal bOr'on .J.nd t 1 ?~ fluoride

.1 la) ~07 b8 :.) bOa

2.3 441 ,oa 55 :.2 2.1 574 7.5 GS Analysis inc ludes o. Oil pVftl !:loron .ad 0.2 "pm fluoride.

325 3.) 1,700 670 5.5 2.510 7.0 GS

356 3.2 1,860 50) ~ 9 s.) Z, 710 i.5 CS PTinc~pal :10\1 frOlll lac,e Jo .. n:., w.. th s

S6.00 'lO,oao 176 . 22 ~ .07 e 7 CC DS!. Z recovered 030 ieet of I .... :Jil, anel ""atu'-cut :'IlLIG. 180 f ••t af a•• and oil-cut .alt watiPr, .nd tSO h~et at ult water \ltth " skUll of oiL " .5 601 1.' '55 1 7 CS A.nal:vsis lnclude. 0.12 ?psI ooron and D.to !'pet tluor'ld•. ,,, '6 ~ ,Z36 4 0 7.3 CC OST'; recoy_red 10 feee "f rn-hoie mud .nd ~,OlO teet of !:llaek 'l,Il.fur' w..ter' ""1,tl'1 Ht'ong sulfide odor

531 : .0.:05 ., CGL ;)5T., reeov.red )0 ieet of mUddy Water and 1.170 f.et :Jf bl.ek sulfur water w1th a strong sulhde odor 320 .. ,069 J 6 6 CC ost ) r.eoYol!nd 105 f ...t ot ru·nol. mud. 95 fut of :nud and "'etee, .nd l,OOO teet of ""..t.r Sao i:I,S9l 1. 5 7.6 CGt CST 4 r.coy.red )00 f.e' ::If 1'IIlJddy wec:er and SSO te.c: of black sulfur water with a 'tronl .u 1 f i.de oaor,

15 7.8 1.5 181 lIZ Jl 1.0 296 8.0 CS An.l1vsts .. ndud.. 0.00 ppm boron .nd 0.1 ppa fluoride.

- 61 - Table 3. - Continued

I..;lcaci.on ?roducinfC t.:lC"'lft&(1.on =­, ., ~. . . -u " i.etian

Gt.n C.lnyon Gc. 200 l.ZOO ~ :".0 '.l LOO(E) 4.05 2.U NW~1:ift.I~;0 'J Slutt I.rr1.~­ 10 200 l. ZOO 7')0 jo ).2 l.5 J: ::':xl C.J. EW .:..os 2~ S\l4::NW..\ojIV-'l;)O W i.. A • .:i.....1.- zoo l,lOO ) ;,,)0 10 'Oa(E) :.us 2JI S'JJdfWt:ttW-t to. '.I She"""U AU Co. liot''t'1.son ello. o !ZO J1a 7t 591 l' md Stud Sa. 210 ~50 ~

'.Os 2JE NE tlt\I

':'2· t2 b~y lone of 6.lL8 ~<.o('l 24,000 18,csa 1".ra4o.. Fm.. '0 lHuif(?) S•. .::i:2.. '0 u 9.2 D(R) l5a D6 2,110 EW !.OS 24£ C i~.l];SWt J 0 SC&l1d.a~d au D~u.r'C Cr••k l,lJ8 1£ill. :>ST 5 1- -17 Z4,100 5,an dO,872 .;~. of ZOft5 ,Jt 1.7 C..U.forni.& 1"aradox Fm. •

.:.os 24£ S,~-'dfE~ II ., Bureau.:Jt elT-127 Xorrtson em. 10 )- 2· 50 6) lJ n l~ U5 :n.di..ua Btu.if 3". FO Atbin

t4 ;; SU~&'10C' 01.1 Slut! Sa. 16.5­ .;.. ••)7 - t,295 Co. Ent:'ada :i.t. l,07a M.ava JO 3... l5a

;- l2 l, J6.2

T.:'H 1,910 l,.:.aO- )2=Ot) 5...... 0 :uc 5- -02 ';",i!.ol 754 t • .: 1,520 ~,o 7, ;00- OS! ~ 5- -·H III lJ7 It.S4J 7.;85 20 S aur..... ,It tecapcun :itt. tlO L74 tAdi= . :1br. ,[ r:mT Alfai.r1 ~oC'rison. ~:'ft. 40 ~.v.jo :i,. 1.:1.:­ 70 :0 l. lSO l.·:.o2 mr l2lt·l71 BuC'ro C.aa.YOft _J_ do l2 927 ;1lI. 'J.l(') :.os :5. C SE\:S~~ a ~OWlc..in e\~1. Oe.ert Creek. .; .060 Ii ,066... JST J 2S,:aa J,:.oO "'-,328 it.:.;lply ::.:1. !\Jna ,r 6. ~90 ?J.r3.do~ :~. ,) 5hdL JllC3 to 5.2 1.7 561 6. ti !r.d.:..,w :~br. j[ :i •• A.f!J..i.rs ~arr1saft :-m. J.~rK.s 4.05 :6£ N-'!SY.I!S£\: ; 1) She H 01.1 C"'. lAad.v\.lle to.. 7.360 ... 52a ~. ~60­ ~s':" ~ L,108 160 to,334 (luray t..s. 7 ,HO 1,~) 1,330

:iisu... .JI..;nn.....n 7. ~65 ;, J85 7. !!4_ )5"I ) ·56 ied. t'.:lciu . .:.J5 Ouray L.J. ',J85 7,5a5 O.,K:JC:;a i'i. ) ; ... lO .; ~.m.["\(,. l ; H.ol.~:.~-(,h.~ ~.aval',) :i". ....i.l2­ ':'-li- Fl lJ .; •• J ~OCK ~ j (E) '" "'lS 9£ l2 C,J-lS6 :.1.0 mr~ .~I) do :.-t8-H la II 1.3 Shirtar"." :1br. lH.. l9'1. 2l 136 :l( Chini._ C'lft.

156 '0 19 115 l,z 'J Bur••u JC C.dar ::usa is. III lJ1 t:1d.bn :1br. :l( Cu.c.lu· Aib1.C'!1 :Ill. , ; Kal~.1.to !on~ 157 l76 ~t Cu.cier :2. ~lS 19£ 10 ;.;1 i __ do "'.-lO~Sa 2t. l8l tZS l64 :l.ru.rk..1

c,)od.r.... c:h il.ll· Ric:o CIlI. t:O 112 " ;m\l.C' ipr1.tlll TW :'i.S 2lE: ...... Bur.au:Jt ''!-Z20 ~.".Jo :is. DO UO-Z7~ ;/)Q ';Z 17 Lld1~n TW ...i:oi1.rs }5 0 Sh.ll OU ':0. :iL... t,.s.1.?pi. .... n ""JU. .],':55 .. JST ., 5.764 t.':02 1!.o,3t9 1.d.. :'-::Il:'x'jI ., ,)40 Ouray t..J. 6,JU. oli,34O )6 Bureau; f ;Y-Z~ iHua is. 1 'i2 l~ J.J 58 !t\dio&JJ, Altair' 10 ~·~2 fI._c.ae-cun ih. _l_ do 10-21- 54 58 18 )6 '.J ~~r. :l[ u.l(a) ~oC'l:isoft ;".

- 64 . 2illion

R...rlu c ...

_ .1 9J J2 0.7 59' 228 58 947 7.8 CS

50 10 L4 )4l .9 584 7.il cs

766 113,19~ 183,7)4 1/0 . 05 7. ~ PA OST 1 racovered 75 feet of mud-cut ,.1 t weeer .nd 1,300 het of .alt wetar.

J5J 27 .2 Il44 HO 100 40 2.8 1.250 7.7 CS Re~rc.d well de"ch, lOa teet. AndYlli. lndll-de. 0.00 p~ boron and 0.2 p~ !lll-oride . J,786 3,720 14,179 . 61 6.7 eGL DST 7 recovered 1,450 fe4'C oJt .a.-cII-t :nuddy water "'1.t.h .ulfur odot' .I'd 90 f.et of ..... t..r and i ...·cuc mud..

51 16 1.5 354 234 1.2 500 7.t. CS

II 10 1.0 187 18 .5 321 7.7 CS AC.alyU.. Lnc!ud•• 0.02 pP- boron and O.J ppIB !luand•.

, ~ao 50 6.1 S ,840 795 6.920 7.9 CS Wat.r from IIl1Lne su.m-p. Analy.u Lncludes 0.27 ?P'I boron and 1.1 ?p!Il fluoride.

62 18 .1 ]46 tlo 2J ~ .0 578 8.1 CS

:"76 20 5"8 390 III 20 1.0 8S7 7.9 CS

6Jl 91 1.9 1,400 158 J64 ]4 2.9 1,990 7.'" CS \latet' tt'am \!I1fte SUZllp that loI'a. 7S te.t d.ep. A.DaiY.l' Lnclude. 0.00 Ppal boroD and 0.4. p;-. Ouo1'1d. 51 15 E./ )60 68 620 SU Well d"l'ened Ln Harch 19S5 (0 520 iut, lJ1.Ch re"ortad flow of 150 11MI (S,tOO bvpd).

Be 26 11./ 510 780 se t 1 000 ~J, 142 .. 0 Q eGt

5' 32/ ]80 89 64a St1 Reported 'Jater flo'" 0 f 1 a?r.l (70 tJvl)d) !t'01n JJO - !Ut, SO ipul (2,000 DVl'Q) frOID JaB fu.t. -inc 250 Ipm (8.50C oJ"',,'::) !r01l\ .. 90 fu:t flow .. itar 101'.11 101' •• o~en )0 day. we. \4S gpm (4,900 OlJod)

5J lJ a9 065 • SU \/hU. driLlinl "'ell .. t ~o het, Wne! ro.. to land surf..c.; at death of 386 f.ee. water !l9"ed frOlll well Reported flo'"' II-pan "'eU comol«tion. 1.50 J'PII (~,100 bvt>d). 2,701 1,)90 7,"'64 1.2.5 7.' eeL OST] recovered 4 •.n0 f ..t ot tt ..nd. of "'hich 3 ,':'20 f.et we. fr..il "'un.

2.0 4.1 115 92 .2 196 8.0 CS Analy1l1. includes 0.02 ppa boron and 0.1 ppm Huorid•.

t.6 3.0 .4 155 1'0 270 7.8 CS Analysu Lnclud.. 0.02 ?"ftl boron ..nd 0.2 ppm fluoride.

1.126 2.HO 6 ,OJ5

20 2.0 I., 17 1,180 8.0 CS Analvsu Lnclude. ~.4 pprll fluor'l.da. 10 .. , 171 19 .5 29" 7.8 CS Analysli includes 0.05 ppm boron.

t: 7.8 3.2 171 lJO . 5 290 8.2 CS Analy1li..s inc:luo•• 0.00 ?pal boron .nd 0.2 ppm !luor1.o•

:.., J50 5,000 .~ 7.7 eeL Weeer flawed frma ehe ..... 11 when i.t .."... b.l.ns drilled: • ...,,1. wa • .l11~helY cloudy ",i,th trace. of 01.1 .nd ~tha:r .)rsanLe cuc.eri ..l. 39 o 65 354 162 598 7.9 DR Analy.t- i.nclude. 0.24 ppat boron and 0.31 ?p1a fluoride.

55 ,I ':'82 104 o 70 8.0 CS A.n&ly.1.1I i.nclud.. 0.29 pp!ll I)oron and 0.5 p~ fluoride.

99 .1 791 III o 81 1.290 8.2 CS ae'Port.ad flev on '·31-S2 ...... 4.320 !)....ad (l:JO spm). Analysl.'s includes 0.0) ",pili boron and ~. 7 ppnr fluoride. J8 1J..I 4 ;0 9J 770 • sU

362 157 o 5J 2.8 616 7.S CS Analy1l1.1 Lnclude. 1.2 ppa fluoride.

372 20 2.. 1.220 360 L9 1,650

:!99 28 .2 1,070 93 21 l,630 8.4 cs ea.l.nl perforated tTom 1.l.50 tC' 1,200 and t,ns to L.42S f.ee. On 9-7-63 e~4' well 101' •• ?~ed ..e rate of 29 gpnt (990 b"'lld) wlth 140 iaet ,Jf d-ra"t

'. , ~5:' '0 2.)39 J.": 7.) eGL OS'! 1 :.covered "',900 t ••e (67 b",rrtL.I) of muddy fre.h ",atar H.axUl'lUftt sal1n1ty ",a. :,5001'011'I of .Od1Unl chiot'lde:; mud sailrucy oefora Ce.; ...... :,000 ppm of .Od1Uftl chloride.

:. ,..00 100 2,:'70 1.,390 l.,030 29 3.1 J .020

~. 790 2.8 "',060 1, 590 867 52 8.5 5,170 7.J CS Analv.i.. Lnclude. :i.. 7 Pl'Jll boron and 1. 2 p~ fluoride..

3.S 3.1 162 20 66 5.' 250 7.9 GS Analy.l.S lnclud•• 0.00 :1"'" boron anc 0.2 P'P1'l fluoride. -. 149 16 719 286 17 .9 : ,020 7.9 GS An.1V.l.S lnclude. CI.05 ?pal. boron .nd ::>'1 pprII flll-orid•.

a.o 5 279 98 !l2 .J .:.91 - OS ... 0 .5 16, 16 9) 11 .,8 8 ... CS ;.jell dri.ll.d :.n 1910, report.d depth 101' •• aoo ieet Deochs::.o top &rid. oottlJ'la of ehe fot1llation arc .uchor's .SCLcuce. Analyst.l lnclude. 0.& ppIIl fill-orlode 20 ... 0 z.) 106 21 .0 225 .. CS Anel~si' inc:ludes 0.1 ppm ~luorid •.

_8 l.8 :.1 2J9 92 9.9 ]7! 8.1 CS R.~ort.d "'ell d.~el'l., S99 teet '4'~th. to c:)l' aftd bottom of the formac:.i,on are author's e.eal&ce•. An.ly.i.l i.ncll1-dell 0.06 p~ boron &rid 0.1 ppm [lll-oride.

- 63 - Table 3. - Continued

~ocac.1oa ?roduc1.n 1 ro't"lf\&cl.on

~ ..~ , , o ~

:.15 ~J But.au ;)C RAc:.aocura ih. II JI :nd.i~ :1br. "i Altai.u :1.or'risotL FlII.. Itt ]) '.I 10 9K-I09 Nav.alO j,. 4]2~;15 LOa 10-27- 54 64 U J.J iW .. ts !!:ac.racla 3s. .J7 ...L.1.l!L 10 56 2.140 Nav&l0 S•• )74 H.J(R) :.l5 lJt 2. aur...", ";;If ltec.a9cun Sh. J 1 J. I., tlJ !.nd.u.a. ::-!.bC'. Jf ~ Af!.ai.r.s ~.oC'ri.son :'m. lJt IS J. do d. 10-21-\. 16 16 .J ~ .l

.1S 2J! NEtlfltNW~!7 ;.j Elluo ~.eu.. !lu.tf 5•• 183-672 6 •• 'JO 20 cd c.... CST l 12.·l6-5a • 6.J91 P.crot.... ~t. jC Cl"lclat' R.aLl.t'K, CD. :5.

>56 -;. "-3d 196 Rlmack. :.~s ::!t.C: StJ.lCiE':5lj,1t Z1 0 C~nCLtl..ne.al h\ d. Ac 600 5- .)i ,J l, ~~O OiL CQ. ':'15 2,1o.i: ) 1 3ur...u J i J"-41 Rec,J,pcurl :in. ;0 IJ4 tnd1&n ~bt'. of A.tfdrs ~orrison :flI . .. 15 25£ SlJ~l~Et ; r.; SU9.Cioe au Glan C.myon Cc. 600 i.,lOO Ac t,1l2 Ja 1.3 l, 16J t. ~ ~~. -'ls !Sl ~n.:J.;S\lb-Y!:~!J ',J Bureau of. ln~)a8A :'Hc:~ Ss. 131-]00 )4 1.\ ).3 i86 tndi..a.a Encrada Ss. "lTa) Athi.rs

;'2:<·J08 Entrada. :is. lH ]~8~ lal ,. !.940 !8 ~ ...Ya)o .ia. Uld. 509 t,l43 i..~&J K.iylftc'& i'll. 1Ji.n~c. Ss. t. :.~a Sa'/ajo is. :';2 i't: loSZ-''!..7 l.a1.9.!l ,\ :,.510 .,l,)(R) '0 ~ :.510 :'(') .:.15 ZSE: SIJ~E~,t 11 a C"relc Ou nl Cb.lly i.. Z.3Jl Z,510 ~,JJJ~ i •• JST 1 :7.S.1 Co. :-!br. ,c Cl"lchr 2,3u2 Ralu,dt. :m. "lS lSE 13 3l"lre&u. oc lllt-L6104 W••tv,-Clr ~. 1- 54 67 lj \. i; tndi.aa. C6Ayon SSt ~ Albin ~b'C'. oji ~or:'1.Sot\ :'.1l.

.. ~s 2St C :fE~Et ~61 a 'ih.ll ,JU c", I.:SlUY .!oJn.. ojf 5• .50:J~ ..q JST 1 -; ,':'l3 ?aradox. fIB. ~r.J!::tr.J·";.w-!; 271 :J 3n:iJn i, 5,556 •• .;00 1, :t5Z :..0. ~50 .~'Cic&n ut.l 0',:,::.<1 •.: ..""? 35 3l"lr.&l"l :J~ !.ndi.an Albics :<.2S lOl Winpca Ss. ~ do .1 la '.9 lU(R) !o.2.S 10£ l2 S i. lA-LaL ~'-V.jo 5., _1_\_ l- La- 5J .1 2. ,. •. 1 :.1(')

d. lA-26 d. JO 1.5

>.\-293 Cedar ~•• :is. d. I. LJ S8 ~bt' • .>t Cuel.r

Ja s do 1 d. , .0 26 o:i"(Ej .:.2.5 liE d. l6 lJ ~ ~-Z61 l!.&l~a1CO t'onty.lll 10 ~47 ll. Ji Cucler Fa. Tm"

]!. I) 5hdl Oil C". ?aradox f •• 2.n8 l.

.:.2.5 :::.~ l S 3ur••u Jt Entrad.a 5 •• J. :Lov u· ).. ;a fi4 La ~n(U..&n 1(~) At~ai.u :J '.I ~o Ha Ja 'i(iii' .:.Is :1.E 51.l'.\.j{£.I:;SlJ-!; n I) ~r.J.chon au L-JJ ?ar,l,dox till. _.no Z1, .,d4 Go. :.2S ::E C :i';lJo;:(E'c 0 An.a4.at'ko .-1.-1 do 1,IJ6-'6 CST Z -;- ·6] 16,~O 97,! ;) .3\1 ~rod.~:1cn Co).

. 66 - ~ .. 3 ...... 0<'> ~•: =8.. u~<.> :, u z'".

., La 0.2 145 16 92 9.j ]82 8.7 CS Ra1'QrUd well depth, 640 ~ ..c.. o.pch. ~o top and boccC7'I ot the fonaac.1oa ace author' •••ti.J!ulca•. 53 10 .) 387 14 96 17 591 8.0 CS ~.ll drilled ~n 1910, raport.ad depth wa. 82~ f..t. D41pcb. to co, and boccaa of ch. !-;,rmac.lon ... ra author's ••ciJDaca•. l08 LJ .5 403 l" 45 LJ 6Ji 8 ... CS ilAportad lHit da,th, 600 f ••c. i).,pch.::o col' and bocce. of the fonaac:1oa ara ... ucnor', ••ti,.D\.&C ••• An.alYl1.& inclu.d•• 0.) In. Hu.or"1.d•. '69 ]14 2,035 _ eCL C£.inl i. p.c-fora'.d ~roltl 170 tc 190 and J43 to )63 hee, and en. ",e11 ~a an o~.n hal. troal 304 co 388 hee. Depehs to :01) and boteom of the fonue1on. are .uthor'l eltimat••. Z.SBa 16,063 O. t 7 B.) eCL DS! 6 recownd 2'!.0 fut () barrels) of J."Y. SUlnc.1y 011 and ",aur-cut !IUd ...nd ~.176 fee' (11.9 barrels) at ,a••y aNd-cut "'at.r.

~o 134,100 209,019

108 ... 5 .8 1,350 t02 94 30 3.0jO 7.6 CS Analysi. inc Iud•• 1 . .i. IJ~ boron and 2.3 IJ~ fluorld.e .

:,JJO Z,110 18 '7.350 1.110 606 H 29 10,400 7.6 GS Reported "'el1 depth, "1..5 t.ac. AAAiys;"1 tnclud•• C.l.,} ;J~ boron and D.) P~ fluor1cia 256 taz.ooo 292,557 .l)4 5.4 eeL OST 5: :lU1G co surface afcar 1 ':tour ..nd "J 1Il1nuc••• con.l.c:z.nc at ,al and oil-cut !!IUd ior 20 "'Ionute...nd ••It "'aCar "'lth a I~UIll of all tor dur.C10n ot c.st. Flow dUf':z.ns i.ut ~ allau'•• at e.ti.:B&tad r ..t. :Jf l. ~arr.is p.r hour, 95 percent .alt ·.Iater and 5 oarcene 011. ~: .9.3 ':')8 156 61 l..0 728 i.o GS A.na1~si. loclud.' a.d PpUl fluoride.

III 948 823 1.0,526 417 -2.21 1 1 SO OIe11 dn11ed !'larch 1957. lO,070 feet dup, 9 5/8·inch cu1nl c ...nted ae 365 fut. lJaeer sand. loned frOlll .:.45 co 535 feu. and 918 co 1,040 f.et P'roduc::inl tOC"\!UI" tions 11.ted are .author' 5 lnt.erpree..tlon. l)a~th co eOfl at the Nav«jo S.nd.cona is ..uenor' $ 8tcimace • ~ 10 2,389 2.; S 1.5 Ct ..:.~~ tetit ~nlle

I. 1.1 5J4 105 c;s Analysis ~nclude. l,O ppa fluoride.

085 3,550 21b 93 ..0 5,J90 GS An.lvlis ~nclud.s 0." p~ fluoride.

~ • b 70 54 1.5 1.890 117 95 31 ),930 • GS "na1"1'1.1 inclu!1&:11 1..7 "'"" fluoride.

.,t70 L53,OOO 2'-; ,:..48 .05 6 9 eet OST) racovl!l"ed .:.50 te.e of salC ",.ter-cuc. IIlUd and 540 het of ~~cuc sale ..,ater.

,,':' 5 ~ 38 .•)00 1'-3,&67 .07 6. ~ ShO CS!' recovered 90 i.ee of "'e'ary i.a.. -cut ftNd and ),094 fue of 11. iahUy muci ..nd i.u-cut salt ..,ater, v.1"y Ibant t-:~ce oi oil .. 9.235 :5 0 eGt 057 .. re(:ov'!red ",B60 feet (b6 barf'e!.) of sli.iht1v l!lUd·cut, n....viLY gu-cut ·~.ter 1. .':'tlO 10 z,na - es "ater sample trom-Horag. tanK .. t "'elL "n«ly.1.5 incLude' La P!JlIl- tluond.

15.100 1l.j83 .251.0 CGL OST 2 recovered ~OO feet n'::.6 barrals) of tl1.gi'ltly lIUdd~ carbon d1oxideC'1} ga.­ ~ut .£lc vatar and ),600 faet 07,3 barreis)of carbon dioxlde(") la.·cut s«lt ..,acer .

~ 9, ~6;' 19,369 . ~9 . .5 Cl,. OS:;' r~covered itoO ieat 0:: careon d:z.olUde e...·cut cir:z.l.l.l.na !!Iud .and ... 2:5 t.et ~t :.arbon ::!1011ade ;el·cuc $.lt ..,ater

.0 ).9 ISb 150 17 10 /.8 CS 'field .:f .cr1ng iess tnan i ij)ftl 1'1 ••' than }i. ')vod) AnelVllll indudes 0.02 pom 3:81 ')or:-OT'l. L70 J22 9 GS An.aiV'lI includ•• O. U ptmI Doran ana 0 ... fluor:z.ae.

;:.0 .9 t29 ; U: .1 :24 · ~ CS Analylu l:'lciudc. (LO;: ppm boron .nd 0.;: i'P'"l tluotld•.

63 10 J,J40 ~.J40 49 3.970 GS Ur.anHufl ex.,lorat:z.on borehole. 191 teet d••p. O.pth to wac.er ..,a. 17-" feet: on 12·12·51. An.iy.it lnclud., 0.4 ~prlI fluonde.

18 ~ , Ii 10 772 2 •.200 CS Uran1UJft e~lor .. tion 'orehole. 169 het da.p. Depth to ",acer "'as ooio ~.ec on d·24·5i Anal ys:z.. inc ludes 1.1 Cptrl f luorld•. \...:. .b (\40 300 ~, .120 GS Analyns l.nc:.i.udc. 0.6 p~ fluorid•.

~. 19Q 1.390 1,190 986 20 1. 7 2.J20 os 00.

::. .:lC 3.290 1,070 ~,570 JJ .... 0 3,640 7.:' GS Analysu ~nclud.. 0.J5 ppm boron and l.J PPfI ftuoricic.

l,520 55 2,.550 1 •.:.aO i.,310 20 l.9 :: .640 8.0 GS Repot'ced y1eld. te•• then 10 gpnl neu than )toO bvpd). Anelysis tnclud'!l 0.-; ppm ~luorid•.

•• 910 ).070 l,910 1,:'.50 l<:l 2.0 3,280 7.0 GS A.nalysu incl...da. 0.25 PPCS ooron and 0.7 PP'lI fluot'1da.

j[ ::)5 69 3.j 36.:. • GS A.nalylil lncluae. 0.2 Pl"& fluoride.

50,000 53.9... 0 10 0.0 eeL OST b recovered .:.50 teet ~f ...... c.r-eut mud, .:..50 ie.c ::f sl.l.iht.ly I'ftYddy v .. car. and ~,)UC feet oi \later WU;:1 ul:z.nie,,· of i8.40C ppm ot JOdlou."'lI chloC"lode. Hue:: b.fore te.t CO"ta1ncd ~.3:'O PpIlI ot 104iwn chloride. d6 59 I.' 388 es AnalySiS l.nd\.&

10 21 226 l24 20 31 ~ .a J59 • GS AnalYl1s lncludu 0./ Pl'll fluor1d•. I - 65 - Table 3. - Continued

?arts ,eC"

tocat1~n ?rodUC1tlll ! !'~nnatl,.OIl u • ~, -u '-' , 0 "

~lS 2lE 14 'oJ Bunau

:.25 2J! SIll:S!l1fIll: 2 0 do lAadvUle LJI. 1.611 .,045 I,d,,­ ilSl' 5 6- ·54 5,on 1.043 S,390 '-15 26£ toI'W~W~.t: J2 0 Phi-UilJ. Is..,. Zone ot 5,650 5,i98 ~,;&4.';o :.- ·64 5, JOL 2, i2a 35,718 }OO ?u:rol.~ p.. nciox ~1II. Co) • :')5 2t S'ol~-tsW.\: 11 'J Clan C~ayon. 12 u6 53 53 tac:o :')$ 2! 3W~ti\l1: II 'J 10 do ;0 .JS :H 55

do do 3J :., lOJ

ilO do lO- '-oj 66 9.J l5 [5 25("Hl )2 :")$ 4E SE\:!lE1: 'J Sur.au oJc ;1. flow JJl co ll!!clarnat".."n ~ :.JS ,,-e SIl'SIll::illl: J4 , c.... tie a.oc:k :10 i •• 12- ;·;a 52 It.. S;2Ci,4 11 Remarks :., l4 ':')5 :it ~-249 li.&vaJo Sill. L.i22. do 50(E} 7 S 8ur••u.;)t U-lll :.to [90 l3 tnd1&Q 5':17i) Atla.i.C'.

:..)s 14£ do o. Chdly 5 •• lll!1 [6 LJ Mbr. ,,( CU.CLH Remerk"

io 3K-SIO do [6 [4

,30 ,7 lSl 'J' l4E SEl::illl:SE~ l6 '. do ilC-4lZ C.dar 1'1:u. s•. :ibr. ':Jt Cucl.r :1ft . ... JS ~6E !3 do Orl&n il.Qck :i.. :"L,.... ~. 3-;4 '0 17 :0 ll. }lJ r~n~ ~t Remark' :; ..u::L.r ~:n. '0 !A.. 260 o. C:t.Uy i •. •.:.0 do JJ LJ '66 :-tbr. :Jc Cachr :m ?'2.

:")$ ZOr: ;0 do u· ':'·54 "l 17 19

:.JS 1!.£ C ~\::'fW~ t9 a Tu~o. taC. l.U: Leadvtll. 1...1. ,3LO 6,292 ~ HQ·lO lJ& 5, Sa2 ~62 ~4, 506 .), , i 3ux-.au li '.... lnl&~. s•. 56 It.. !l .. , ::tc(l,.,ul .:"!£41U lK-ll9 ~1."'V&Jo .is. :. 13- 508 i. .J ::: I::: Ie H.llr.nOS.a Gr. 5,310 5, JJO 3,)80· DSl' 5 3,37'- ':i.51& 5, ~'18

':')5 ZJE J2 !u&..u JC 1"(-17 !ndi.an. Ut'.l.i,rs :.)5 ~r..E C 3.J.jfElc. 5 a Z:l L;'U' and. Ak.ail Zon. of 6,614 ;,~OO· JSl' Z i,.:380 2.~oJ Jannaoarc ?aradox :$. 6,580 <)f.l ''::.::1. :..]$ 24£ C SE~ll: , a Shall 011 c.;,. 6,308 ;.255­ :>ST 5 ·\5 1a 300 J, 340 0; ,J9O Ouray 1.... &,903 ;.305­ " ••;'5 ,:'75 t,PO ElO.co:. :llI.. '),n~ .:.JS !c..c:: 1 '.1 ih,l.I;' ••u. ~ i :.l'l:\~ae. 5., SiO·'n 'i6 17 2.J L.J !,;"di..n .u;!.airs :')5 2t..E C ~OC':::NEk 2,5 l) <:hamuli,;" Oesare Creak 5,')4;: J,-.:.a ·SJ l, i?1It:rolet..aa :an. '" 0:0. !?aradox Fill.

:..JS Z5! C St.i\:Sw~ t~ 0 t .. UO hlfta"f 4on. ot 5, ':'04 , ." 79 5.389­ O'T 3, ':00 5)4 J2.5S4 '0 !aradox ::11.. 3,51)) '0 I·UO ;0 5,J'H ,.,1:: 5,504·4' JS!' 36,193 :-teetHC· 1,.08·';00 ~ 5 :.eo :'1Jlll,~d J- l-·H 17 ~ 1 i ;9 C~.aOdl.n J.nd l.JJ5(~) i<::lc: C,J'~.

- 68 - call1ion

., ; ~ . .c ·. ~. • .I !

2i 298 185 JO lo2 50.

J8 1.6 210 Jl 82 5.2 os 00.

1,)78 6.851 1.5 6.0 (29) Cauns ue at .:.37 teee.

8. )) ~ 1 I,. .8 4.6 679

\4 lJ 2.':' 236 26 2b ., J84

214 :.15 .26 1,7)5 91 i,a OM Analysu lnc.ludu 1.1 pplll .. iuminwa. J.05 ?pal u ..nic, 1.'- ?~ boroa, 1.2 ?~ ~luor:Lde, 0.01 ppa hydroxlde, .. nd 1.4 ppw. pncuphaU .

~. 750 \4.600 94,J90 . 10 6.J CCL OST 5 recontact ~,UO tee' of -.Addy ..,..ur.

5,086 )7,400 68.512 .13 ~.8 eeL DST I) :-aco"'crad 1,018 f••e of ....y, l!IUddy ",.en and 990 f••t of aalt waUl'. t •.:,)O 650 loo 3,'-10 155 5,1..0 8.1 GS 16 • 6.5 21. 64 354 GS Analyul i.nclud.1 0.4 !''PIlI fluoride.

.)7 • (JO) the u\ccrv&l tucad "'.. tram 1.598 to 1,799 t••t i.n the De Ch.. l1y Sand.c~ne and. oval''' 1yins Cueler FOJ:m.acion; how.ver, ehe Oeehelly ·"e. ehe rlpore.d producin, fo~c.1oft. OST 1: flo_d.t rata of tl.l berrels of .11,hC.1.y ..lty ",ecer per hour on SiS iDCb. bott:os ehoke and 1 inch co, choke. Recovered 2,560 het ot 111&hcly .alcy water

559 JO\ 2,1.59 0.6 30) Yald an 5~27-58 "" .. 1,000 bvod ()O Spal) by OaUU tut.

~ , 580 ~),d90 co

3Q" II lOZ 52 J. 0 ~, 0)0

581 J,815 99 1.28 1.S 01) S.Vtn-lnch eU1.n1 lee .c 1,106 t••t, d.pch of "'ell 1.1 1.122 f.et, pertoraced "'.lov 822 f ••t.. Depths co col' and bot.t~ of the fonaacion are .. utbor's e.ci.aa.c.,. 18 1.2 1,180 J6 '8 57 J,UIO . os O.,eh ot ..,.U il 300 fe.c, c...d co ::j~ t.ec. Analyst. inciud•• 3.9 P1* fluort.de.

1.640 3.490 2.\ 8.f>40 5.' 10 90 5'" 1:.000 7.9 GS Oepeh at w-ll II t,lo) h.t, ca••d to 328 het Analylis includ•• 0.1 ppc fluorlde.

~. )00 2,810 .2 ',080 J19 9) 56 11.100 7.9 -cs Pulll~d yu1d on 6-:15-64 "'a. U7 gpte (5.340 bvpd). "'t.eh H8 tuc of drawovn. AnalvllS lnc:1udcl O. J pplll t~uorlda. . ,280 ;:, '160 .1 J ,~50 n 52 Ii ,jOO 8 CS PuIll.CMld :'lelci on )-11-0. we. 1~5 ,pm ('-.250 b",~d). "'lcn H8 t ..c of dreWdovn. An.ai"·SlS I.nC~Ude5 a.1.. ?pm ~~uorlde H. JOO ~Z.187 1'- 9 eeL OS!; flo....d .. l-lncn IrreaJ:l o! saghcly u1ty "'aear In S5 manuees.

19b [9 ).1 11J 58 1.4 - GS Analyst.. include. 0,0 Pp8 fiuonde .

.. tol ,0.000 .088.0 eGL OST 1 recovered lBO i.et .jf saic w.cer-cut 2ld, 180 t.ee of m.lO-cut ,a.i.t "'ater, ..nd '-50 teet ~t ..It water H!(' ~Q, ':!4Q l)l.btl':' ~1~5 5.S C:' DST : :,ecoverec 1&0 :ue ~f ";"4 .. nd j ...-cut ::Dud lone 315 f.et of g••-cut .... 1.: ",ater.

Ij 204 22.:. 14 .2 4)J as AndYlis i.nciudes 0.2·poe tluot"1.de

.9 219 192 . 2 J7J GS 00 .

.8 JOO J29 GS Oc.

II 4.2 ll,i. :'1':" !l .J as Yield on 7-29-54 "'es leu than 0.1 gpg ne.s than ) b~d) Ana1yu. lncl.l.Ide. O.t, ?p1lI fluon.d•. ].1 ':'60 2.J 6B J2 1.5 712 as AnaJ.vsu lnclude. 0.4 I'JM tluor1de.

\5 •• 2 298 ., 4\0 os 00.

19 b.l J2 \8 .1 5)8 os 00.

~ ,670 20 2.5 :.490 :,!lOO ... 310 i) J Z, 760 as AnalYSi' include. a 7 ppm ~luClride

.: ,':'75 ), 19~ 11.2&0 2,:80 ],,;;!78 7.4 ShO DS1' 2 recovered .. 70 f••c ('- barrel..) of .ulfuroul "'ater. Analyah includes ,,,,. • .-oniulII. 10 ~". boron. And 12 ppat. sulfida. -. J 287 t4 ~ I., 467 as An.1.~t11 lnciudu 0.7 ppm fluoride.

JO 46 ., Z7J GS Ana1y,u lnc1.ud.1 0.6 PPII !luori.dll,

.:.;: .000 L2 7 1 CG"...

'00 ll':',310 186,35] 11/0SS.SCL DST Z r-ecoVOIred 1.5 feet of ".avily ,aa-cue. :nod, 90 f ••c of ".avily o:ll .nd la.~c\lC lIlUd, 100 fe.t of oil-cue mud, and 710 f ••t ar salt water.

- 67 • 11 Ot.••olveo soU.d. CalClJ.L.&cad. fro-. dec.rattiaa ~Q~cic.u-nc.. tXc.~c .&& neead. I/ .-'nalys". :'y: 3R, '1 . .3. 3ur...1,l ~f !t.ci~ci.Cln CCI.. Ch-..i.c.al I.n4 leoi.o~i.C&L t..loor.car1••• C.u~r, ·Jyo. C!.. CQre t..&boracort••• Uu; •• :J.aJ.UII. :.X. CO. C.:.nc1nen.u! Oil Co). crt.. C... lilorni.a r ••n.ft1 [..&00 C'&CO C"1. ••• ::ftc •• !.Qa ..ul~.l ••• C... .1.1.1. Jov. JoveLl 01vU1oft at :n.. 'Jaw Ch_i.cal CoJ. JK, utah Hace Oe,arOMnc ., t a..len :So U.3. c.olcliul .i1.u."'V." ?A. ?I.ft AJMrtcan i'lltrole..... CCt1l!. n. ?.e.anon uooC'&CotlU. 5.111: ;'.1" Clcy, '':c"ft ~. ;tacky Moua.c.ai.tl ~n,,1n••r1nc C"., '::cand ';unCt.10ft. Colo. ihO. Sh.Ll 011 Co. 50. ilJ.~r1oC' Oil CoJ. SU. UCMl icace Uni.versi.cy aCt Utah :ieac. Ch..1sc 3/ :t.••i..Ic1v1.ty :':lIe ..uC'a4 I.e S7·". ~I R••isci.vHy ....urad I.e jO·!. 51 (ron pr••eac ~uc ..ounc ~oc d.t.ra~cL ;/ il..i.ac1vicy raeuuce4 .ae. ~·T. II t\tlAlyst.:iI jup,Lieci oy C:'Ct... .i.-nice 0t.l ':Q. dl ,\t\alyst.,s sU~'Pli..ad. )y usarve au .utd C... Ca. ~I 1a.utivtty ::l•••u.rI4 ~e '!1-? 101 ~'SUt1.Vl::'y ::WSJluC'ad ..It 39-:. Til a••ut1Vlty :M••ured J.t as-: ITI ..uu..Lysi.. lu,pJ.Ud 'Jv ?acl.iic ~.cur• .L ':.lS ~x~lou.t1cn C~. ~I a••1.Jt1vi,cy ma••ured .at '-O-!'. "'V:I tron ~n solution ~( 1:1JM

- 70 - :1'111 lion .:: o

o ~ -e • 0 "",,, ~ ~ ~ : 8'"" ""

;0 16 0." 97 :1 565 • GS Analyns lnclude. 0.3 p,,:r. tluond•.

~arre~s) ~,.)l7 3,800 "3.310 71,66618,100 116.107.6 ShO aS! l recover.d l80 feet (: :11 IJut!ry Tald and tUt (14 . .5 aarnl.) of shgnCly ~ddy, s11;nt.l" ~ ...v ,&It 13 18 ZJ6 ~J6 24 H 1.0 )S4 _ GS Andy.is inc1l.uiu 0.$ ppm fluoride.

4,790 n,100 • 3,002 .18 8.0 Cel Perfout.d L..68S·.... 1S0. 5,108-5,282, .and 5,)7i.-5,"80 f ..c •

~z, 000 i1.,St48 12 7.1 cet OS! e recovered J50 ieet ':If g.say w.t.eroy :lIUd, 270 t.et of I ••'''' IINQdy ...&t.r, and 600 :e.e of ~l.ck Julfur ..... e.r. .1 12 \00 " 31 9.0 GS Analysu Lnclud., 'J.6 r'0aI Huon.d•.

50,000 84,516 .106.9Cel OST 5 h.d a flow of inil.nmacle la...nd recov.".d ",085 f •• e: ot w.eu' ,

763 73.000 tl8,567 .08 7.1 Cel '.loiter sG'lopie obtained (-rom. 011 ....ell SCOCK tanK; s.ual)le 101.' 1iSht ':trovn .and cen­ t.lncd a cl• .er filtrace

208 .1 ]i.8 2.2 1,060 .6 GS ~.pora.d .... li. :i.pc~ tilC' ~I!et. r'e::'~orated )20·':'~2 fnt. :Jpen hole 4tl-610 fut Analy.t. includ•• 0.5 ppm nuorl.ci•. 118 .9 428 l81 )J 2.0 i ,180 J GS Iteoorted ..... ll deptn 67; holt, ooen hoi._ ... 0·075 teet. An.ly.t. inchute. 0.) :'TJtll fluot'lde. ,; 238 100 1.1 400 166 )c 2.2 l,UO 8.5 GS Reporad .... 11 .3C'PCh, 600 fut. Anaiyns l.ndud.. 0 ppm ::luonci•.

71 16 .3 292 98 61 3.1 "77 7 ... .:;S 3"/ 27/ - 'S~.5 -l.UO 96 13.8 t.690 8.3 B'R. R.ported weii. deoeh. 598 feet, ooen hole S~598 feet.

;. J I 00 37S 8 .• CS Sorl:1; ~~'- ....'.:;i,,"S ;;cor.- u,~ to \0 iptn (i"7 ':;; )4,) b'Jcd) Analy.is l.ncludc. 0.10 "pm iluaride .0 i..9 166 "7.; CS Analysts incl.ud.! 0.; ;)~ Uuand•.

102 ':'18 • CS Analysi. include. 0.: :tpT:\ ~luot1,d•.

6.0 J.2 lLJ GS Yield en 9· )O~ 5':' IJe- less :h.n 0.1 ,pm (less thaa ) 'ovpd).

10 3.' 98 315 - GS

:28 3' i.:' 616 221 60 Io.~ 1.030 7.6 GS Analysts includu 1.0 ~::~ ~lUorld•.

110 10 l08 B6 13 i. ,470 CS Held on ~-Q·5i. wu le., ::.han 0.1 !!:Pftl (\eu than ) ~d) An.al.ySLs l.ncludes l.~ .,pm fluarLQe

597 • GS An.alvSls ltlciudes O.!:l' ilptT: tluot'lde

12 10 3.5 u.• ) 78 31 .9 220 - CS Do. 28/ l,':'80 56.500 1/ 12 ','1-

-; C l. j i)) 11 .5 206 ~ CS Analvsl.S lnclwde. 0.2 opm fluot"l,ci.a .

5.0 l ... III :'.f:I 2i4 -; CS Anal"'sLJ l:1cluCleS O,C ",pm fluorlCle

., .. ,JOO .06 .:' Cc.;, OS1.i <"ecOVot ..ed .,C fe",c. ~f muc 5L2 f.",c of sl:q;nt.~v 'lIUdd ... ~~t.e':'. }jO :! siq:ntl\' mudd~' ~lac:k sultur~u. ~.. cet"

5.5 ).0 105 :28 • GS

: ,060 b":'.965 108,68i n,lOO .087.2 ShC OS! 2 recovered .,200 feet .:If sulfur \,IAur.

3,876 95,000 156,534 .077.9 CC OST 5 ,ecoyer.d l,ilO i •• t of s1.i1htly ouddy sulfur ,.It 'Jolter Sd\ple t.Ken .IlC tool, cl.ar ...ater, nydres.n sylf1ae ;lr.,.nt 1,., l83 5,500 90,623 .11 7.1 em OST? r.covered lo,l85 feee of llWoJddy water ''''Lcn slLght sulfur odor. Clear water s~le .... l.cn oreciptc.atll!d loron ~x'Ld•. 1.5 5.0 ... ':' ..04 661 - CS Arl.l~SLS includeJ ~.C pom ~1.uoride.

100 ~2..;40 87,099 11'.097.0 Cl. OS1 1 recovered ~29 i.et o~ wate"-cut ~d. verv slilhtl\' oi.l .and @:a. cut; and 5ge :eet of salt 'Joleer Wlth sulfur odor,

250 S6,800 9),~6 12.!L2 8.0 Ci.. DS! : recowred 5.094 teet Jf oi~ ,1uU:ed wLtn 101', )O~ feet of ,alt l.laCer .-nd !,U­ .:ut oil .•nd 186 feet of .&It ...&ter ~. 000 .0:)0 tOB.9f>4 12:'10 tl 5 CL ~st 1 acovere-d ':'65 :eet ~f :!IUdd ..... slLihtlv i&.I.ty .... &ter ·.Iith Julfur odor .nd Z.704 ~e.t :Jf siq:htl\' S&l'::y ·.Iatu· witt': sulfur odot'. :80 138 3i6 ~90 108, ·.I e U is ilOO feet dee~

- 69 - Table 4. - Selected hydrogeologic data from springs,' water well:

toc.aU.oa: idl::..&u ) .... anet MeidL". 3oJuree: ~. %line 1:~.1; O. ,JU, or ! •• 1,14U; 5, J~r1n,; T. o: ••c. ~ol.; './, ",aUt '".lL. O~.r.cor .,t. ~Vft.r: ~ .... ~r: )l"IC'&c:Jr ,Jl;' .Jvner at 1:1JM lIacar sMlai.a '..I•• col,l..ccad ~or c.h••1c.al lnaLy,i.s. t..Lm..c~n.; J.d~ac ~ny f;:l~C1on ~.'PO('c.d ?roduci,n, :;)nt.ec1on: :'31.., :ormaci.oft: !.a •• :-tbr., :-!emaar; ,ad., ..ry; Sh. o .ih.aL.. ; is., 5U1dscona, n...... C'. La records:l[ ;,1.1 ud J•• '::::lcqani.....n4 '}caca and :-.ctaraL 1.~.nC:'•• do :'\OC "'t.c: ••••rt.l·, "'lira. !JLCt\ Co:':. ~d..nci.:i::.cion.

~e ~ .2. § ,. , . c_ O~racor ?rOducin( =i~ ~ ., .. u or """,.r :ormacton .:: )­ =2 ;l ~ ~ ~ -~~ " 0 ,- ; " 0 ;. S.cc1on

20S zy N'!\:::ft~Jc J4 " Sc:q.:n.a trn· Noren iioen rill. ~o ,000 0,00 H ).1 ;aC1on C.:l. ,OO(E) 225 LW SW%:Klt:sE': 32 iJ SC£nciard. OU i3 ,197 OST 2 :.- ·57 7.120 t. JJ~ 3.384 Co. "t C.dilot'ni.a 59 41 l~oo 1).4 LO l.1 II us Zll SlfjfWt:sWJc]6 S To,,", ~t Gha.- Glenwood. !arC1aC'Y i.~a· 1.5) 000 i-l'-H ·.,rood AlI4 31'ctnll oua roc:iu 4, jOO(R) Uc&b. Sue. Fl.h 'd.accn... or? ZJS JW N~ts\l-\:!l!:~ !6 Cley ot 1liGb.... Ric.htield. Cnrr :;0110'1 ~ <0 7-JO-H 'id 14 J8 ~2 :~.Ld. 51!)C'1a.1 :m. 1,:.oO(R) W4:tRl4::tftlJc 1% tow of ~o.eb.rry Tnet.ary 1.ip'l.... .L.lQ£ ,- JO-17 II "'l ,.; :0 l]' Jo••,a .i9rinC ou. cocu '"J(R)

I" LII 26 S Towa. at Sur· Burr S9'C'tlll do dO 1.1 vtlh ~ liS lV :ats.ttsE~ La S Hoec-CM liac do l !..DO T-ZJ-17 112 S4 182 )4 ~62 Spril\1 ti(Ei BiS ]V :a:\::SW":SE~ l3 S elCY rlt l1.oa.... CoLd Sortn" do 10 :'"J41 SllJcKltM!-t 1) S Souch 3en!i Joseph. f{oc do 3, .:.00 10 )6 1• .:.4£1 !rr1pcton 59r1nJ tiJO(E) Co. l~o Z5S 4W :itf:.tfW~.t!: 29 1,J aeft O.I:'t'1.a.Jer do '5 At lOO 8'50 32: lLI lO 5.

Z7S ;W N!~\::SW.t!: !'f Mnte t..aurta do .l2Q... J9 ,",ei Coa.o lid... c-.4 LOO(E) GoLd :-tin.. s;,j.\:SEidW~ do do lJ, .,00 <0 61 '.1 ;.] :'000:) 19S 111 p~ l4l C..nyOft do 1,l'JO a,0 LL S~rtn. 270(H) 295 .:ow SW\:SII'cllh lL !ovn Jt S""""1.lL do do :..S \.0 ~07 Junectoa 50rtall lOS )II '1II'cII!l::fEl: I. S !ovn ot K1.npcon do 510 do lio. Z5 1.4 20 2.1 !Clnpc:oft )p'nlli TI(iij lOS 4!J NII'cII!~ 1.6 r""", "Jf C1.rcbvt.U. do .L.12Q do l2- 3-02 9.6 1./ 0.0 ClrcL.v1.U. ,)!ilr1ns ;0(:<) ~!1 0 C.d1.tom1a l 2.385 1.'96- :lST t L56 J] 616 l5 659 Oil Co. J,J.44 llS ." NIIl::fII.\: L Tewa .Jt rerct.ary 1.-9\•• jj 4) 1.5 l7. Ant1lllcny "1oU ::,ocic._ llS r~ S.\:S!.\: C.AH!ocni..a '0 vU. C.2. lIS :. I S£\:SIl

iSS ~ '!!.ct."'~cU' ... l· Z7 l.ih1n~r'.:mo ~~r .,,507 ?,58!i ",H2-~~ :0"J{~) J ,'HO U\'o. _oJ. 1~ ;:l1nt. ::ft. , " 365 ]I.l ~.t1.0nA1. oar C.&lloo.l1 -:.n~ WU\'I.I••o and 330 51 11) J.' i .. rv\.c. j £011. .iolt'1.n1 5tr.J.-9\c T"i'(ii) <:1.L.tts 51. )6S i'.J •....r1oWII ·....c.r H.aaottJ. ·,.I....echo ::11. !..O 20 :0 '.J,.I4lrs ipr1.n1 )75 t.JJ S!l:s!\:S!.\: L' ., ~.ciona1 lark : do 500 270-]00 ~. ·59 1.i l6 i.nice 'Jahv.a'!l Uld 600 <0 I.C l6 ). Scni.~c Calts SI. <0 ;00 <0 7,7 j] " ZJI.. do ;00 do 10 l- 5-

l7S .W 19 II J.J 16 271

~J J7S loW S K.c1onal ?.a.clt Sh4l.p Cre.k Y.hv..eo .and. 1 Kl 1.3 :.a2 S.,rv1e4l 5prull 5t::d;i\C C1.it:!3 SI. J]S 6W c :iEl:s'~ L6 o Pht1.1 i.pa :.A !rou1C ill. J.I.l .,n0I',6l2-)5 './1,1' l l] 188 ?acrohua ~o.

O.aic.oca SI. '-,32' ",39l '-,326­ Wlnlor t". :.. ,393 :",H] }7S 6W ~~J.: ]J V.r101JA w.c.co Lower .\...y Y.....cch ::ll. ) ~I ?lov 3- J-54 50 it LJ :! .0 :.u.. n ~~rtn1 1.3 .'JOQ(M) NlldEtstl: 2 0 Philli.... U Ouoc.& $,. '-.311 .,94l :lST ] 10- ·6) l] LO III PecroJ.eloa Wln.or till. (.,941 Co. l7S 9W SW.lt:SlttN~ t1 S Hac1.onal hn. 1-14-

- 72 • - 71 - Table 4. - Continued

':fA .. <

?t'odUC1tl1 ; (o.nu,ci,OQ ,=­.

t .~" : ., .. '"

7_ ] .. .,) 1.05 0 •.3 0,04 38 ]0 J .) ]83 "" ~ Z~O(lt) I :ryO .09 10 J95 SIl '0 I01'Rf '0 Jl II 195 Slol dO :am150 do 5 '-10 do J4 7.1.0 395 6W' t65W j9$ &W st\:llll~t~ 11 j ~IJO '0 16 l4 LlO(E)

~o ~OO do 9-23-63 :..4 5.3 JOO(E) do )"'l J4 II TO([') '0 11 '0 7-20-6J 57 5.6 .0. JO (2 o:TW' l~os 10 ]')! lOW SU:Loc Z2 30 ~ do 29 t.J J8(R) TrOllLC: Sh.. LOO "0 3-21-0) :so ).1 .04 70 JI :J i""W"

~oo do 36 J9 l(o) mrtOO do L17 51 C~l : •• mr\10 do I-ll-'l 58 12 119 59 .;.os lOW ~lt )) S :{ac1on.a.l ?..rk do '.3 0) l6 [1 :.0 165 Service :..JS llll :n:....-':!Il:~ II 0 McC.lloch OU Paieoz:oi,c lu.­ "'l0 (3) LlO 10 C.Jqlo u:on.

C.ar3ll1 Fill. ;"0 nov i.4) H mT 7-Jt-~2 .:.i.S 9W ?N-tsEttNJc 10 :.I Nat1ona'" ?ark 86S.. 0f24 310 !.u.te4 .,d II .00 6l tJ :86 ';;ervt.C4 1(11) HS lOW Z 3 ::to do 5.. flOW' J. 7-63 9,J. .02 l2 lJ LO a--.rk.

~ts LOW do do do do J.. 7-03 do; .01 \9 8.3 t.S t.J 9.

L7 Uld 20 ) do do .10 io 3." \4 1.0.0 :'0 139

~lS t2\l sY~~.t tJ J Ucm hr... 6l2-'J6 3,aL Led 3· -)0 ), ;05 L,':'02 17. )80 ?eCI':]leua Cori'o :'15 lJW' t..lWu1n.n ~oc l62,tJOO .00 590 1."00 i8) 'i~H·1.n~. r., fbv(R) '-lS SW I'(""&JO ) •• 350 io ~-,"~ .. oJ S1 5, 7 '2 l4 liO Z~(E} c Sil~k 16 0 Superior OU )2. L6 '-.201 ~,648 4.590­ CST 2. t6Q 194 10,758 4,604 ;J 8ur••u ~t :fa"aJo S•• 550·';00 IS L.aQd !iAn.~­ ~.nc

~ 15 n.: i"''!ct'on :iI, ~br'. ,Z'-2 ',p i ,:'00. 2 ~111)(~) 5wolo :uc L. :;ai. Jf ~.anc.ot .ih. ;05 :oJ ~o,-:t\ :lorn ::a.. tOO 'ilow 1/'J0 27 1.5 ll' lW ll.S 7! Pt'ic.a itive, r•• =;30 ='0 1J J.' lOI Th('E) l~S 5! Nt~..lcfNJc 12 'J Ut:.ah. Paw4lr C.;)i.co" 'Jall ~onh Kern ;1'1. i6Q l,U' 5.. i •• I.l 'I JOt ..nd LLpc :ia. Z R...rk, It_ark, Co. US n: S£tJakSEt 2.7 S CLty ot Price C(deon i9r1n n ..... catf u. S.. do 7_ Ll-6I 48 7.) .00 17 II 7.6 214j -...,," ! I I US dE :fE~~E~.3 eo. ~el .. on do 0 ~o 3.. tJ-ft2 1.4 3.0 Z9 )7,i ~JS it C it: tsW"': L.3 i c..no Unci 011 t.r'C':In Sis. :1.b'C', '!l, ~l9 6, 19S.. H Ac: !l..re l2- ·5... (3) '. >601 and. C:.. ':~. of M.&ft.c.o. 5h. lin. 6,412­ JST) 12· -34 (8) L,it31 2,)50 ~, j02 1":'~duc.e:1.0" ~J ~.JS 7! SWf;sEkSW..le: ti 'J ~oune:uo. :....:.. l do J,3J~ "',!.~O 1.865- :'.. JO .. (1I.) lO 1121 SU9Ply Co. '", ISO .....ca, eto 1.0,204 4.227 .. .10 1.0 .. )0·63 [1 LO Z, iTS lJS iE: ~~~'" l jo I 4,J9O l.JS 7! do '-,J). "',)42 .. [S :')9 116 !. ,3U

.0 r., "08­ "'-lO·oJ (llJ (8) ~,1l0 J·ll-04 L4 ~O ~. no 40 4,067 ~.H4 ~,oJ70.. do .... )0-0) (ll) L) LO 169 4,1002 s•• 40 ll- 5-64 I.. 5.a b.atk..l 'J Cley of :dr· :tordl Kom , •• [14-J8l .10 1·2l-\2 \9 .05 62 19 :l nz '1t.."

- i4 - nd oil and gas wells In bedrock In the High Plateaus section

i..lei: ~~. o~rt".l. of ..,atar P41r d..av; ~pm, ~~ll.Jn. 1M' m1.tluta; (E), asti.:llo&tad; (!i). :wa.urad; (ll), rC'P0rted .. t o::ioc ..,.car IUl9". wu collected for cn..ical analyll,.•. The (!), (M). or (I.) los oe.i.da -:0. l1.v.n u.Dlt. !he otna't' 'Uloit i.s c.~lcul&c.d:m che ~.i.s .:If 1 &plII equ.al. J~ b\lpd .Ind 1 ~d aqu.als O.OJ ~. attlOd or point ~f coilectlon: FIO\ol. lndi.c.atas collect1.on at ...prini :)r flovinljJ ",aU; DST, :iril14,c.em ta,t !or Cli..l ::Jr ;.as; "1.I. loI'1.ra .. Una cast ior oil or .... • .,..rk..: OS1'. cirill-lIcCfIl tast daca, and WI.::, \O'1.ra-l.i.ne ta.t Qae.- rcoerced bv at.l :It' ~. cO!ll'P.n.... .'ullion

, . ~ .. · ~ . - < .• = , ~ · =3. . " • ~i·. . ! '"

i 5 2.0 238 12 o. • GS aeoorted nel.: .J1'l >1:-5; IoIU ....00 !;j:lm (4a,OOO owtld) and .In 6·2.5·6) vu 290 gprtI (10.0000wod) .",-"alvSls .. nc~uQu O.l P?fIl fluot'lde. ~"lt C~oudv ,761. 30.000 so, Ltd 0.:5 0 9 CCil. OST 1 :."ecov*ro!c 7.5:2 feet "i ..... ter wae..r 1oI\el1 .l lUln or...nic con· ten::; unablE :c cot"-roci.,HI' .ae (f'llS ':l!lIe ~ue 6e11eved t~ ~ fot1llAcicn water,

3.1 13 ll9 II o 1S .3 :)2 je.u G:: Ana.i.vslS l..ncluc•• C.C ;:'p1II .li~1nUrn, J.00 ;;1lT', cOtloer. J.: ?'PftI fluot'lde, Q.J ?p1II ~:..tl".1u:ll. v.ao ;:.om ~ngan.u.;.: ?p:l1 ?neSplae.., .lnd 0.00 p.".. ~lnc:

27 20 ., J ~ 0 .J 548 ~ GS Ao"i,·sl.$ l:'lcludes C.: ?om .l!.L:...··::nnull'.. ,j,OO ?P"lfl ccpper. :1.';: :lpU'l iluOr1Qe, D·S ~i.:h1\J.fll. 'J.Ol '::lOt'll manlll.ne,•. ' .;, :l0':ll ena,enae.a . .lnd 0.00 pp-m ~inc. 19 135 ~ 59 .J J71 1 G5 "n~~'ISl5 ~ncluQe~ 'j.e: ppa: .lium1:nnl:. ::'.OC ?PO l;opper, D.': ;:;.mt iluOClO•• 0.0 ?'P'IIl :ittllu1':l. 0.01 opm man~anese, 0.13 ?I'~ cho,pnac.., .lnd a 00 ~par l.1.nc

5.0 ~ 19 1: l58 5 GS "n.lvsls ~nl;lude5 0.,)2 ;:pm bot'on olnd O.J O'Or.! fluorl,de.

898 oJO .0 2.700 64" 3.':' ':',100 . .;, (;$ A.rtaL\'5l1 ~:H:i.:JCU 0.:' p~ ~L.Cllnuc:. S.GO :Jptt '::o'P~.r, :.0 ?1JIII fluorica, .O?;nn ~':.r::ur.: ~.'~::l~ :'ll.&~~01:-:""Si., .:.J ~'Cr.: ;:Ihc$;:,nace. 4.nd ~.a1 ;;It)t:'! nne ],5 ~ 19 76 :> G~ A:·I.L·.·S~$ ~;-,C~' ... af!1 0.: ?P"l' 3 l.ur.:. nu:n , 0.00 ~'C:':". ::q:ocr, J.~ ;::m fiuortde, 0 :- .. } .,om :Mr:% .. r:cJ~ -.: ;:IC~. ~h;:)s?hac.., ~nd G.OO J;r.'t ll:'\e ~ • .:'.70 ,750 5, 150 a~2 22 .790 ~ 9 GS AnOl!\'Sls ~nctud.s 0.~ ,:m I. HP:'::':-Ull'I. 0.00 ::l'On C:;'~;:1.:'". :.- :cm ~luorlcll. d 0 ?~ .~:h:.,... ::'l. r:. .. ~ .,?:f: ::1 .. ns.nc~•. : .• :;OPT.'. ;::ncsohat", . .inc (;.00 ?P'! L:':,\C '1lI!l.o.Hac.ur'f' ol;culter :::iu:-. ~)OoF. : .2'-0 .1 790 ~. ZBO 1.250 j "i C:: Anoll:'515 ;.nciucots _.~ ;:lDnl ol~ur.'IlnWll. 0.00 p~ ~ccoer, J.9 :l:.iorHla, :.0 porn Ilt.hl.u:ll., o.S ppm mansanc.. , 0.0 ??m pnO'ilh~ee, .lnd 0.00 =p1II ':lnc,

6.2 2.S .] l50 lto o l4 B GS ~1ne ~un:1.i caved ",nd .aoandoned.

~. <) .'.;: ~ !:: I I .2 .0 " lest ., '8 o Jj ·les I .0 J3 1.275 108 2, S93 :I::L :-ST ~ recovered )00 tut =~ r.\uc!, :..00 feet :d water-cut ~Q, )00 fut of mudd\' w.;\ter, HlQ • ,::J53 :eet d 5:i..hr.":. ~.uddy 'Jatn 5.mp~f: tram bottom. 8.0 . b 1.26 J 20 Anal\'h.s l:lcludes 0.08 ,,:on: ccror. "'no O.J ;:prlI fluoride,

JOO

255 Tne 5c!':n~ ~~ ~:". J ~.satt : • .)10' orooaol·. ~n :::'Ie ~rl.an aead to~e:..on. Anaiv1:i.s I- I r~' ~ncltJdt' D.~5 :lDTll 001'01'1 and O. i 00"1 ~luo-rolde. I': .~. CS Th", 'Orl:'1;: l5 ~:'1 '" ba".llt fh~.... ~roO.ol'· ~:-. :ne 3r:.oar. Hc.ad f~::r:IA.t:.on. An.alY1:1.s to I I .nc~udI'S ~.0b ?em borol' lind ':.': j:lOTl', fluot"lde. " \7 \0 An.ai.vSl! ~n.:~udl's 0.02 ;);)l!: borc1'1 .an

•. J •. 0 12" '0 '1 Li 180 :, CS An .. I",", :nl; ludell 0.0~ ::10m boron .lnd I).l tluorlde.

560 C~, ~S: r~c:)I,'E:n·(l: ~3c :t"t :r '.. ~tet: ""ten. fe...· ,p"CI(.5 v: rio!""" dead :rude oll l.'" :., I' j I I =.n@:~c.. t~ S,H.r.• :'.:: '.... 1'1'1' :':.";;Im )00 JOO ppm .:ni.::rtoe ,,~, .:. iO t.990 . I . ~oo I \' , G' ::'1 G'

.0 .. 0 ~ .... 70 o p .. GS S:lons ::: .. scha=~e ~easurements: Aon.l 19~7, ~OO lI'Pa: OO,bOO ~od) ~unl' lq5i '"' 1 L11.00C ~pm ('- ~lO,OOO owo.:.!) '.0 ::52 9 GS \,loiter sampl<' :ol~ectl:c "-Irnilf ~rl1lln~ w.ll. l;a.ln.i .ae. Z70 fe1!t.

J' S.,; 1&0 ~ JO (. )0 .3 GS "~d c,ned ~. J')u ieet, ;)crfo~ac.d trom 1, Si) 1.92C ... nd ~,.,6Z t= 1.974 :eet.

9l J .0 3tS .J SiG 7.9 GS .... ll c",sed ::l Z. 000 tll!'ct. ,.-rotoraCed frCl'nl 1.268 1;C ., "174 ieee. . .365 0.0 870 i~2 33:' ._ ~ .210 b OS well c ••ed to Z.OOO f ••t, oerfot'u,ed frOftl 860 co B90, ~.268 to :.132. ~.87J to ~.92'J, .nd •. 962 tc :.97.. iut. s.":) •. 0 :1J 6. i G$ AnatvS1S lnl;luQeS G.O~ opn: ::>ot"Otl ",nd J. ~ OQtll t:iuorllJe

.:. a J!!4 ~ , 1bO ~ GS

.:.. b 7 7 eGl. '.n.! l :."ec::Ivered lO,Z~O l;C \cUbLC l;enC1JtI.eers) (5.~ ~&llon.) of 'W .. ter .nd Z50 ~c (tes. chan ~ cubic foot) 01' s.nd. 'Jatar sMIIllle ."'•• f:"O'r.l '" 'and 1n the Lower ;:tart tne Iro01': Shal...... tll::!", lola. io§~ed tr~ ':'.'-JJ' tc ... 326 !i!e.t A.rul"5is l{1cl·..Ioes pam l.tniurr. . .8 l" uo . 231 ::'.0 8 7 eCL DS. recovereo ~.250 ~I!et of ,11~ht:~·. l!tUd-cut 'raclt15h "",.ter Analy'l.S lncludes J.') Opr,l ',:O'1:"U::'. 2.5 o '0 .j 'I GS 100 :lST ) :-ecovered 682 feet ~f l'lNd-cu: water Analv5is 'lncludes j:ltlm Lithlum. , 5 GGel l.; 1.:. l!!) ~ 79 192 I8.' GS Analys15 Lncludes 0.01 ppm ooron and 0.2 ~p!l fluot'ide.

- 73 - Tobie 4. Continued

:'.Jc&cion OliMracor ?t"OdW:i"~ ; )'t' J'Vnolr :~C'llI.ac1.on . =­, . ..,, , -..:.a. ,.~ , 0 " Q , , 5eeClon "

~ ..,) 5£ S£b.E\:$l-l!: L5 ',J 3Lrch C= ..k E::Dery it!. ~br. 5.318 5-18-59 tJJ J5 6.1 l29 :rr1.~Cicn Jt ~cos :in. CQ. J MOunCAut Fuel lO r.rroft 5s. ~bC'. "'.622 !o .578­ t't'aduCc.Lon :'-·)O--o.l (11) 510 188 i

jo "',J6J­ Jo 17 ZQ '.7 1.170 2.070 :".041 do ':'.09l­ :... )0·63 1.252 l. JJO :.. .:.)9 Pacdic K..ayenc..a ':':1\. J .J65 ~. 500 J , .. :0­ )S1 ~ ~ 5 . :.16 1.250 ~. ~.j3S :oJ ••eern 01.1 r,.;'1.a'i&u is. }, JOO ':140 1 C.J"t''I'.

SE::a.\::'sW-t 30 0 KoW\c.ai.A Fuel Ferron i •. :-tbr. ].,06 ~.719- Produccl,on 4. )0 ... ,<;) Z5 1.1~1 6 1, jJ7 i~Dplf Cu. Jl :iaa.c:o. 5h.. '" ,J49 '.... e.r SE.t:lW.lcSW.Ic J2 a ':he.. ieu.. do :'.!o.9' 1..,3n 4 •.516-71 DST 1 .:.- 4·56 l8 l1 ll7 )05 ~.cural G.&. Co. ~-'lSc:t,o(E~ t6 I) renneco Oil 3,202 ~,L50 8,i09·50 )51 :.. 1957 1.011 C,) • '0 8,969-04 )5t 1 lH7 :.D7 ~,i"l 1f,351 ~,776. .JS1 :0 l~57 !J) t6. ';]!o. J.352 :.35 .,E :N.ir:.i;';~.\o; t7 'J Thr•• ieu.. turon is, :-tbC'. ,,:)90 t':''Jduc::: L~n .. - t2·,6 ~87 ~J4 ::... cural .;""" Ji ~cos ih. .tattr ~v • ~55 6£ S-.J.\:SEt:N.Ic ~O <,) Tenneco ·)tl -10 6,095 5,710- 5.. i'll!" ll- 1-~4 21 l2 l.]f)(] 1,350 C,J. 60. 348 R.m.ar:k~ :t.m4rks

Cr.a::v :!.o1.t~ H-2'JO ;0 -100 lal 12 l5 eM. HO(l1.) 5;';-I:::~.l6loi.lc lJ 0 Thr.. :ieun Emecy is. Mbr. J,d10 1,668-19 )5T l LJ 529 l,ll0 ~1&cur.l C...... ,t ~cos 5h.. Co. O....oc. 3 •• 3,,jO,S S,:05·t2 JST 'J u-tJ->4 11 l. :.48 2,.540

Fecron i,. :-tht. ",0001 '1.110 Se. J. ·)4 1.755 JC ~nCo. Sh. hmarks do :',:'90 4,"80 i .. ). _)4 L.J13 l,J5C ur:u.ru Duae.. S•• ;.290 5.4l0 5.)08-18 JST 2 J-Z9-54 14 2,180 20,12'" Cr...,\ '!i'/er ~:!l. ~jO i.e .W19. nov ;' ·27·.;y )J 17 O. I.e. 41 l2 ,9 l04 a"'rks '1(11)

~'.3 ~~ 15..·\;S.Ei:; C~C..,. .Jf ';0 l~ :'0 21 La c:.,nri.AIII !:; .....::s!':5E~ ::s J 1.::.ln 3.)uc::e~7: r .. rt'~n is. :-tbr. ). laO ; .d80 HI ;:,J. Jt ~.anc:os ih. ~3S l:: I~!\ol'ldiEl:Sc;! t~ !,:,W'n Jt F1~ee,=. n.;J.~St..if t ... ,,5 1)00 now Ll :ay.tt. S!'rt.n" t, JOO(M) :35 ~E: 1't1J~~~ :0 Cicy JC ~l:.i ~oC'c:;" aarn ,'11. do i-,S-57 :'1 5.5 , .0 Hli :15 ,~ ~£'tN!'::SE! 5 Clt.Y.Jf .E'u,cock Cnen. ill'/er ~l1I.. 10 3·27·5d ,,7 13 J.d HO '::"=i,on 5.r1-,.

5E1::SE\:SC:~ ro 'i !.)Vft Jt 5panuard. jo do .J9 ;4 66 l.7 450 '::; .. nClr':iaici 39unll SOl~.1::'l'!l:':O .) C... li,forni.a rer:,on S~. :1.br. i,381 d.8l0-90 )ST :. lO- ·6t to 19 J. lJ8 l. l10 I

5.12S-n 1ST I' 2-iO- 50 d4 ) .:i60 Ouac.a 3~. .,.U2 ';,:80 S,~~". )51 LJ !-Z4· ;0 l,'J42 21,JtO o),':'l2 C..d.r :-towtCa.Lll ';,.2.30 ~.J92 o,J7l1­ . iT II .1. l-56 2S0 .:~. Uld ~."'j4 :-!oC'risan :11I.

!:S 5£ r .. rron Ss. :1.br. l,242 1.775 1.)05-19 :'lov 1·l9... 53 109 2,JP 195 ~ i :ianco~ Sh. l,J9's- ..1.lQ... os! L-22-33 2:1 ~. J97 452 1.<08 H(R) 1.-2)-l6 ·)51 ) 1-,4.;) t, HQ·)O J5T ; :·23- iJ ~ .J ~ 7 SkcU:, JU Jo L,170 1.i30 ~, :..i:"· .L..i22 'l.lw ~. 1-';.2. " ~, 000 ::.,J. 1..':05 ~S(~) C1c:; Jf [.i.:::h t..JSt r.trti... r:{ qne- )i SOO do .; La 1.0 5a1 l;\.a C:ceK ;~C':';'\~ ,,,CllS ~. L·)O(R) To"," JC 3r~ SOC'l.nl "1,, .; ;Of) Jo 55 ~9 7.5 :<.:Josh.a"em ~'JO(t:) do :0 1)00 jo 37 ZS , 1 I.) t 19 lDD(E) ,:ij 15 t1c~n :Lsh .lnd L.:I. FL,n 10 ~53 1)00 do 40 ~ ) 14 U6 G4lDlI ;)I9c ;:~c:h.,.., 4, JlJO(E) :iPC'UUj

- 76 - 10 l/V7 171 ue

7J 462 ]76 ue

19 l/332 304 ue

1.1 28J ue

I.J 10 JJ 281 178 ue

~o 10 J..! .. 16 :'i4 ue

30 JOI ue

6.1 124 ue

3.5 1.6 12 0.2 240 7.2 cs -'t\alyulinc;lud.1 0.02 ?'PftI bo~on. 0.2 .,pm fluor1dc, .nd 0.0 ppaa _ac.n•••.

328 ue

:"/ lJ2 10 127 li3 ue

196 l/690 527 ue 1 258 l~ 1 809 540 ue

,-.9 4 .~ . ~ ~J8 .1 16J .6 GS Spring Juppb.•• Tesple ot 51n.were wacer system. Malylu include. C.O!- PP"l boron, '1,: ~1)m !luoride. and 0.00 ppal mans_nan. 579 "hi. ~e.st C1t"1.11cd bv Io1.r-ro'a,t"..: method. ~.t.r w•• encountered .e. ';"1.') fece, with estimated :-,uld ot 2 i?ftl (70'!Jw'Pd) .Ie. HO t ..t. :~ g;no (850 bvpd) at 1,200 fuc., ~.:.O ilPftl (~,800 ovpd) at ~."70 hac, ana )00 i'Pftl (l0.20G O"oIpd) at ~.600 f ..c. Sdt Water at 5,000 feet.

19 610 - ue

56 10 .J 254 1,,91 .4 421 5 CS AndYlis l,.nclude. O.J Pl)ftl t'll,l.Qride.

16 la .7 169 1)4 296 .0 COS Sprlnl .uppll•• waur to Grotto "'.tar system. Reported ::

! ,J50 J ,olD 3.2 9.J90 2.080 1.600 1 ;0 \J.500 7,4 CS Samllled (low of enurt sprlnl .are. at old hloghw.v on.d.;. AnalYlu lnc:ll.lde. ~.O P1'G boron ..nd Z. 1. ppa fluorid•. i8 : .0 182 l/U9 - ue s ,000 ~32 19,149 110.498.0 CL OST: rltcoveud 196 hac of 'ul.fur w.car.

210 e.l (10)

~ 1 ;0 ~ cs "OS! frOftl 7,1.000 to 7,761 feat r.covered 3.78) f.et of vcr)' h••vl..ly l! ••-cut ""atar.

s. ~ _. 19 7. i CS

1.0 267 260 .1 484 7 7 GS

Il t~ 7.2 11 lIO 246 21 I. OH Althaulh eh. wall 1-1 Perforatad trom 1,290 ::0 1,948 f ••t, 01'1l0s1-(. tne ?t'loce River f"onlAttan, only the Ndrch Horn FQ~tloon re'Oorcsdly Ylelded \i.c.r Reported '!1«ld. in 1962: floved ::.70 SP. (9,~OO b.",d) and ol.llftped 1,"00 &pm (5~,OOO b~1Id) 209 194 369 8.1 CS Th. Colton Sartne il po,ubly a tault .prin, that ~uue. ~rOlS the Colton FOnllAcion, 1Jh1.eh overU•• eM ~.ur-be.rtnl Fbpcatf LiJDe.stone. '!i.ld ftOft! Colton Spring locah. 1.ft elUtion, of ...Uona: 394 (9.4 m.illion ~.rnl.) l.ft ).961 and 691 O&,l. lllillion barrels) 1.1\ 1957 (I•• Cordova. 1963. pl. ).6).

\0 1.8 336 324 603 8~9 3.272 733 3,335 ::::1 ::6 ::

311 ~ 9.5 b. J CC: The ..... t.r ..... clOUdy oranle, vitn preClopitl{ • 1.r,on oX1de, A,nd it i.· bellev.d t.o be lIl&lonly concten.ad wacar. 1..700 L' 6 eCl

(8) ~7C j .25 6.9 eCl ••ter is slIllillr in Chamlc..al cOatOOlition to \i .. ter frOft! che ferron Sandscone !'\e'lllaer u:ceot ~n..t it 11 ftlUen. mora dilute. The v.ter :..s beiieved tc ':I.... !lIlxture ot condensad and fot"lUotion "'.ter.

6J 95.0 l.9 eCl ":he water was cloudy orange, w1.ch precipitAced lron OX1-l:]e, conden••d water. (3) l., :50 •.:5" 62 ) 3 CCl Iotater va. ch.r .nd sO"'PY. o 392 987 6.1.00 tI.4 eCl :.Jatar "'., clOUd':" ye tlow , "'ith prectpl..t.. ted iron oX1.da, and 1.-:: lS be11eved t.:l be an eQuai mixture ot" condans.d ",.ter .nd foralecloo" ....ter. 2)0 .1 91 16 1.110 6.5 CS Producina .a, veLl, yhld w•• 1... than 1 ,pm (lou. tnan J.'. 1N1'd) .

16 7.9 11 )44 271 ~ OM Reporced Yleld 1n 1952; £lov, 50 1lJ'll (1,700 b"'~d); pumped, 700 11'G (24,000 bv-pd). Analy.ts includU 0 ..:. ppm £luot'tda.

- 75 - Table 4. Continued

! ~ ~ 0 ~ '" 0 ]~~ ~-:- ., >- -:; ; Loc.acion ')p- , Q ~ '" if ~ - ~- ~ Q 0 • 0 -:; Q ~ z 5..c.cion

us 2! JJ r.r~i.&ry 1.~.- ~S JOO nov 10- 20· 54 J8 0.00 Z2 5.i,. LJ J,' ,... r;oc;c.a .:.50(E) " 27S JE 'EI::fU:":~ L9 C• .Ubnchc '0 SO laO '0 4-Z~· i9 ;0 J2 )11 ;5 :..9 177 ~8S I.E JO Forese Illnpc. S•• oJ JI. ~·24·59 ;1. 22 Yo J5 to 211 i.rvtc_ LIt) '0 2SS 5E SIl

365 l£ SEts£ttI!t: 11 a tenneco 011 Kai.oaa U. ;.on ;,92J 6,060-70 Prod.uc:ti.on a.lS.. 63 l."O l70 1.97J 2,:14" Co. ::esc Coconi.ao :is .. 6,92J ~. ~90· lOO(O) do 0-62 t.iJ-.Q ll.6 !,O49 2.782 7.011 ) .- L1.i.b..o u. &,,620 6,954 6.660-81 S.. Production 5-l0-65 18 551 !23 )."'60 2.1OC l ...C'ks ·".cae Cocon.LQO S•• T ,31' 7,345 S•• i,,. l2-12·';) '40 ZI. 2.5'13 t,2:1e 3•• !t....C'k. J....rk. ' ....ck.

Cadar :u. ... s•. T.500 d ,.530 7,305·90 ~~O $WaD ':I.C ~ - :0 ~.; .. 7)6 US 252 t •.iH: :1.bC' • ,/ ~u.clar )(Ri'

1"~:~l"l 9 ,ZlS A' ~ ,t.24 S.. S.. Z-L?-;;4 lt2 Sl J, ;0' Jr.;: sed. rock.•• laa ilell\ark, ~ernat'k:ll

')'L,sol\ild Jol1.d.s ':Alcl.llAtlet ~:~'lll d.atat":lli.neci ~~n.c.:.c.l.:enc,J "xc.oc: 1.1 :10eld. 1/ .UtalysLS ~y~ CeL. :hlan,c.al J.nd C.olo.1.c.al !.~bo('&conl', C~.o.t'. "I~o. II CL. Con I...&oot'&C;~t'... QaU~•.•ax_ OK. IJeah. Stau O.~.rt::Mnc .It !i.eden GS. (J.3. (do 10tj:1.c:..al 5",ney :-te, !lAUi.bu.r't~n Co •• 0kl£h08l& Ci~, Old.... ac. (leah Hue Ch_1n . JI !.Jcal L:on. ri ~ron 1.L1 ,olutiQn at :.t.m• .It £GalySli•• Ii ."naiys:'. 'l.£lt1'lbd ~y Collitorn1.& ot.! co). ~/ C... lc:ul... ,ad ~~ aud1oC' trout. pare. ~er ~l.llion ,t J.l..k.ah.nLCY (u c... lc.i.... carbonaca). 7/ ;tau.dla "n. IvapoC'aClon. 3' Tuee. ~I 1.si..C1.VlCY :Ma.u.rad

- 78 . nUllan .. ~~ ~~

".... > ~ ~ . Raaarlu 0. -. ~ i1• 0 .. ., o ~l ..

0,0 a.o 0 . .2 ; ,;

~28 1., Z~J 5.5 7.J ec:r.. Y.C&r- \J •• cloudy oran,., lJith pr-aCl,pic.ced u-on oX1de, ..nd it L' b4:l1eved to tMI a mutcur-a of approxtaately 2~-~0 p.n::enc tona.totion ....".r ",ith the rlmloaJ,nln, be1nl conden••d "'atar .... i L,~80 22 ... ':"':'0 '0 38 81 7.110 8.0 CS PToduc:.Lnl la. loIeU thae ylelded leu than 1 liM (te•• tnan}4 bvl:Jd).

(8) ~, ZOO ), L31 2.12 8.2 eeL

... .;,)9 2J,500 .. l,7l0 16 6.5 eeL.

'50 2.27,'CCL

20 )86

: .008 100 .2,7S6 5.2 8.0 eeL OST :. r-ecover-&d e, 700 taet ot tr.sh loIaCar-. 597 ;'20 3, .. 55 5 8 ... CCr.. OST i recovered 500 teee of lIIUd-cut fre.,.. "'at.r. ~ ~S. 700 i6 Ii ~ C::;:' OS! 10 recovered 210 ~e.t of mud, )00 ~eet of .... It 1oI ..t.llr very sl~lnt.ly , ...-cue "1.ch • t.int trac:e of dead oil on top, anc )~2 ieee ~f mud. 48 L5 7.2 eeL :.IateT LS ~.llevlII!d :0 be condensed loIater Ole 11 d.epened :0 Oall:ot.. S.ndstone ~n !. 958

24 Z ,060 7.:" 5,050 200 96 bO 8,150 7.8 C;S Iolater lola. pUlItl)ad fraft tu01.nl In. ide loIeLl a. I.' lola. ?roduc:.d trom ""ell C: ••lnt: dun.nS loIeli produc:t~ol'l ta.t. Yield "'.. a leu than 1 Itm (1 ••• than )4 ~"d).

In Loa 26 616 128 2~ 7.3 CS Reportad yuld on LO-27·55 101" l.L60 iP'" ()9,400 !)vod).

55 ;0 ,)0'0

))0 ) .069 " .... 9.5 CG~ OST 9 t'f!covered J80 ieet of ~ud, 920 t •• t of l

66 1,150 3,:'7... 7.8 eGL DS'T 2 r.covered 2..0 fut :Jt Ija.-cut mud ..nd 10,008 te.t of i ....cut ",ater. 6. 12 )75 276 Z9 20 ,3 640 8.0 CS ',",eli. lS )50 hee ::i.eo .and 15 "ertor.ced fra. 127 to 1100 h.t in .. Lluvum; now.ver, tne ..., .. tar enters tne ""ell I'IlOltlv i'ro!ll tn. eeet!n R.iver for:nae10n from the ~e:."f:)t·­ .acad :ont! .at 115-280 :eu And tiUOu!h tne "'al.l bott"'" .t 350 teat. Analysis includes 0.09 PP"! ooron .nd 0.4 PP'"I tluor1m!.

~. 3 .0 '::.0 t99 J76 8.1 GS Analysis includu O.t pl'ftl fluond••nd J.OO PP"I ",.ng.nese.

: ,.;oe :",S"i 5B :; .) cer..

4) laO \0 ,0;:0 ": GS Analv.LS lnc:lude. 0.) ppr.:a fluor1d• .and 0.00 ;:Ipnl lfI.&n'.a•••.

7.9 GS An.l.v~lls 1nc:ludes 0.2 1'01'11 flUot'lde and 0.00 1'1'1'11 :Yr..ne.neu, e.) es Sprlni lS In. £"u;'t :.:Jne .at :he Caul <:If o:t1t! ~.aatch Monoelln., .and :ne w.ateT ':0"­ ".ains hydrogen iulflde. Analysu: 1ncl;Jdel ~ ! pam fluor-ida .anti D.02 ~pm m

i.O~ ); III 3; l,O 978 7.5 CS An.alyslt 1nciude. 0.3 ~pm fluonde and 0,00 pplll man,&neu.

• ,_2_ .. ~')o .• :.:.0 so ~. ~ eel.. DS! _ recovered 7)0 ieee vi 'll~ntiy muddy ..... t.r .nd i09 feet of :;l~.aC:j( or,lclC.1,Sn "'att'r , 0 :.:.5 '..n~l..: ::rl:;'~l"!l: .. ~., ~·~s~ In :'~52, .an .rteSl.r. lio...... i; encounCe:'

,>J, '.':'S 50 7 'J eGt ;'51 ) recovared 80C feet vf s.ait' .... ater "':"IC= 40 fee, ot :l'lu~. Organlc mactaT ::Iresent :.n water sCllo1.e J ,'JoG 25.'Dt ~~ ~ ~~~l DS7 6 racovered 180 f.et vt mudd .... ult ..ater. :.:'6.3 580 3.598 ; i)S1 ?! racovaree iO i.ee of ,.It loIater and ",....c. OrlJanic m.tter pr••ent ln "'lIter :>"mOlf: . ~ j ,50 .. ',2 OST [1 r.cov.red J,400 teat of oracl('1sh sulfur w.ter .nd )0 f •• t ~t lId "'1. ?O~ ,.:j'a 6 :) e::tcell as,; ~) recovered 00 :uc )f ::tuci .Inc 06G te4t of ult ..&tee Cle.r ....t.r uDl~i.e.

d6i. J: .OOG 3],361 .113 6.5 eGL OS1 U racoverad 1.l0 feet ot mud and 240 f ••c oi s.lt wat.r. Or".n1C: ..ccat' ::Ir\sene ~n wacer s&Jftvle.

7,)70 GS AneSlan flo""" encountered .... hile drl1l1nl iilS tast. i~) a.'J1S es OST! ~lo"".d L,l"0 idlon. of ..... cel" ::Ier hour (710 bw~d OT 21 ipm) ':hrough .. 5/S-1.ncr: openlnj. ll) GS D$7) r.c~vered 750 tut of fresh muddy "'ater ")7 GS ;)ST;' r~cover@d :,260 f.at c{ [resh ...ter, llIuddy Ot1 :00. . ::)0 )0' c'i:~i; _.J:!.'.) .,~iO ~l Jl I~c ;00 2 CS Ar:eSlan flo"" C!l'Icountcrl!!d .... hUe .iri.1.1.i.nl sa. ta,t An.ly.is I.ncluce, t 9 pPftI boron .

; ) ; .. 0 .0-'0 3 GS An .. LVS1S lnc1u4.' 0.0 oam "lumt.n1Jm, 0.00 Dp!fI C0l:lp.r, 0.2 Pp!ll tluor1.de. J.l ;:10m :~::hlum. 0.': 01"'" ohosonatt!, 0.00 po:n man,."es•.•nci 0.00 PP"' t.1.nc. • 1'J b CS Anaivs1.s ~nC:u4es 0.1. ;;'pnI C'uorlde .

, ,a ~ 60 '::)i

20 :3; 7 ) CS An .. l vus lnduct.. 0.03 j)pnl boron and 0 ;IPftl fluoride.

- 77 - PUBLICATIONS OF THE UTAH STATE ENGINEER'S OFfICE ( ,,) - Out of Print

TECHNICAL PUBLlCAT10NS

No. L Underground leakage from artesian wells in the Flowell area, near Fillmore, Utah, by Penn Livingston and G. B. Ma.xey, U.S. Geological Survey, 1944. No. 2. The Ogden Valley artesian reservoir. Weber County, Utah, by H. E. Thomas, U.S. Geological Survey, 1945. "No. 3. Ground 'water in Pavant Valley, Millard County, Utah, by P. E. Dennis, G. B. Maxey, and H. E. Thomas, U.S. Geological Survey, 1946. "No. 4. Ground water in Tooele Valley, Tooele County, Utah, by H. E. Thomas, U.S. Geo­ logical Survey, in Utah State Eng. 25th Bienn. Rept., p. 91-238, pIs. 1-6, 1946.

"No. ;). Ground water in the East Shore area, Ctah: Part r. Bountiful District. Davis County, Utah, by H. E. Thomas and W. B. Nelson, U.S. Geological Survey, in Utah State Eng. 26th Bienn. Rept., p. 53-206, pls. 1-2, 1948. "No.6. Ground water in the Escalante Valley, Beaver, Iron, and Washington Counties, Utah, by P. F. Fix, W. B. Nelson, B. E. Lofgren, and R. G. Butler, U.S. Geological Survey, in Utah State Eng. 27th Bienn. Rept., p. 107-210, pIs. 1-10, 1950. No. 7. Status of development of selected ground-water basins in Utah, by H. E. Thomas, W. B. Nelson, B. E. Lofgren, and R. G. Butler, U.S. Geological Survey, 1952. "No. 8. Conswnptive use of water and irrigation requirements of crops in Utah, by C. O. Roskelly and Wayne D. Criddle, 1952. No. 8. (Revised) Consumptive use and water requirements for Utah, by W. D. Criddle, K. Harris, and L. S. Willardson, 1962. No. 9. Progress report on selected ground water basins in Utah. by H. A. Waite, W. B. Nelson, and others, U.S. Geological Survey, 1954. No. 10. A compilation of chemical quality data for ground and surface waters in Utah, by J. G. Connor, C. G. :YIitchell, and others, U.S. Geological Survey, 1958. ='fa. 11. Ground water in northern Gtah Valley, Ctah: A progress l'eport for the pet'iod 1948­ 1963, by R. Nr. Cordova and Seymour Subitzky, U.S. Geological Survey, 1965. No. 12. Reevaluation of the ground-water resources of Tooele Valley, Utah, by Joseph S. Gates, U.S. Geological Survey, 1965. No. 13. Ground-water resources of selected basins in southwestern Utah, by G. W. Sand­ berg, U.S. Geological Survey, 1966. No. 14. Water-resources appraisal of the Snake Valley area, Utah and Nevada. by::. W. Hood and F. E. Rush,' U.S. Geological Survey, 1966.

• 80 • :1I;,111.0n . f .. c ~~ 0 N} ...... ~ , - <; ~. ~ -. R_rIu . ~ '; ~~ ~ i i~ u 0 2- ~~ " f n• 0 " .:i c: -. " lU . § I .< .. ., i~ ~ 0 ~~ ~

1.1 5.5 2.1 l50 76 26 0.6 212 7.8 CS Analyu.' inc Lucie. 0.1 Pl'" fluoride. l,110 )0 5.2 1.760 1,240 .6 1,990 7.3 GS Well de"e.h, 285 hllle.. An.aly.i' include. 0.1 .... fluoride. 167 7.5 .5 44(J 151 11>4 .2 665 9 OS Sun••t ?ark a< Du.rh_ C.&tIYOD, Andy.i. includ•• 0.05 p~ boron and 0,1 .... !luor1d•. 187 16 .6 1,510 166 87 18 2.270 8.2 CS '!1.III14 ""at la•• chan l 8... (leu chan 3'0 bv1>d) . Analy.i' inc luGe. 0.76 .... boron and 1.0 .... fluoric1c, 2,475 .:. ,178 12.344 ~..59 (1) Water j:lroduC~10D attar .ncount.rin, dn111nl br.a'" &< ",84)-87 fe.c; yilllld ,.- 3,450 crea••a tTO'IIl 0 '0 10 bural. of ..,.tar .er nour IInile drill1.nl wuh cubit 9~ ..... c.r ot'odu(;: 1.on faee 0' ur .or hour. Aft.r dritl1.n l oreaJ(' &< ", 987· feac., c __ inerea.cd '0 .. •• t~ead 10 barre i. • 0: ..... t.r hour SUltli.e t.att.en "'1.l:h pre••or shutdovn a.d wall. b10\11.nC :1:I1.t a.d h••."d. of "'ater 240 4,970 11, )75 li~ 57 7 5 CL li~b4 160 ),692 9,869 7 .5 CL S"abbtld 130.8 ':l.rreJ.. of fluid 'n 19 hour.; no .how of oil or la•.

2, 970 3.540 1.1 11,800 1,290 569 Jl 16 ,~OO 7 Des Well ;,roducclon 1. o\4)ril 1965 w.. 82 barr.l. of "'ater '0 24 day. , w1.th lot ,002 barrel. " of oil. 4. ,000 1,931 10,&30 ll~ 7) 6 5 CL Watar !CII.~h co Uacted wh1le dri:Unl with ur bec"".en e,565 (bOt:.JlD of coUlng) and 7,170 f ..t. r'Jt1UC1on. lIX'De.ed 1. :lV·n noll! lncluda r ilBpo\ol'.ap ~mo.r of .'1o.. nKopl FoM1.&c ion. K.alb.b LiM.tene, !orovll.1' Formation, Ceconlno S.ndsc;ona. a.d Orian Roc. Ionau4 of Cutler Format 1.on_ 1,.. 00 :48 ",752 ll{ .1 6.0 CL

1,140 5,112 lO,494 ll/68 6.2 CL Dt-lll1nl with au a.d blO\led ...11 9,424 fe.t, weU IIIo&kinl , '0 C.5 barrels of water ." hour. 09.n hole '<"" 9,267" '0 9,42"- [e.t _

- 79 - No. 4. Ground water investigations in Utah in 1960 and reports published by the United States Geological Surveyor the Utah State Engineer prior to 1960, by H. D. Goode, United States Geological Survey, 1960. No. 5. Developing ground water in the central Sevier Valley, Utah. by R. A. Young and C. H. Carpenter, United States Geological Survey, 1961. *No. 6. Work outline and report outline for Sevier River basin survey, (Sec. 6, P.L. 566), United States' Department of Agriculture. 1961. No. 7. Relation of the deep and shallow artesian aquifers near Lynndyl. Utah, by R. W. Mower, United States Geological SurVey, 1961. No. 8. Projected 1975 municipal water use requirements. Davis County, Utah, by Utah State Engineer's Office, 1962. No. 9. Projected 1975 municipal water use requirements, Weber County, Utah, by Utah State Engineer's Office, 1962. No. 10. Effects on the shallow artesian aquifer or withdrawing water from the deep artesian aquifer near Sugarville, :Ylillard County, Utah, by R. W. Mower, United States Geo­ logical Survey, 1963. No. 11. Amendments to plan of work and work outline for the Sevier River basin (Sec. 6, PL. 566), United States Department of Agriculture, 1964. No. 12. Test drilling in the upper Sevier River drainage basin, Garfield and Piute Counties, Utah, by R. D. Feltis and G. B. Robinson, Jr., United States Geological Survey, 1963. No. 13. Water requirements of lower Jordan River, Utah, by Karl Harris, Irrigation En­ gineer, Agricultural Research Service, Phoenix, Arizona, prepared under informal cooperation approved by Mr. William W. Donnan, Chief. Southwest Branch (River­ side, California) Soil and Water Conservation Research Division. Agricultural R~ search Service, U.S.D.A. and by Wayne D. Criddle, State Engineer, State of Utah, Salt Lake City, Gtah, 1964. No. 14. Consumptive use of water by native vegetation and irrigated crops in the Virgin River area of Utah. by Wayne D. Criddle. Jay M. Bagley, R. Keith Higginson. and David W. Hendricks. through cooperation of Utah Agricultural Experiment Station. Agricultural Research Service. Soil and Water Conservation Branch, Western Soil and Water Management Section, Utah Water and Power Board, and Utah State Engineer, Salt Lake City, Gtah, 1964. No. 15. Ground-water conditions and related water administration problems in Cedar City Valley, Iron County, Gtah, February, 1966. by Jack A. Barnett and Francis T. :'Iayo, Utah State Engineer's Office. No. 16. Summary of water well drilling activities in Utah. 1960 through 1965. compiled by Utah State Engineer's Office. 1966. No. 17. Bibliography of G. S. Geological Survey Water Resources Reports for Utah. com­ piled by Olive A. Keller, G. S. Geological Survey, 1966.

- 82 - WATER CIRCULAR

No. 1. Ground water in the Jordan Valley, Salt Lake County, Utah, by Ted Arnow, U. S. Geological Survey, 1965.

BASIC-DATA REPORTS

No. 1. Records and water-level measurements of selected wells and chemical analyses of ground water. East Shore area, Davis, Weber, and Box Elder Counties, Utah, by R. E. Smith, U.S. Geological Survey, 1961. No.2. Records of selected wells and springs. selected drillers' logs of wells, and chemical analyses of ground and surface waters, northern Utah Valley, Utah County, Utah, by Seymour Subitzky, U. S. Geological Survey, 1962. No. 3. Ground-water data, central Sevier Valley, parts of Sanpete, Sevier, and Piute Counties, Utah, by C. H. Carpenter and R. A. Young, C. S. Geological Survey, 1963. No. 4. Selected hydrologic data. Jordan Valley, Salt Lake County, Utah, by 1. W. Marine and Don Price, U.S. Geological Survey, 1963.

No. ;:l. Selected hydrologic data, Pavant Valley, Millard County, Utah, by R. W. Mower, U.S. Geological Survey, 1963. No. 6. Ground-water data, parts of Washington, Iron, Beaver, and Millard Counties, Utah, by G. W. Sandberg, U.S. Geological Survey, 1963. No. 7. Selected hydrologic data, Tooele Valley, Tooele County, Utah, by J. S. Gates, U.S. Geological Survey, 1963. No. 8. Selected hydrologic data. upper Sevier River basin, Utah, by C. H. Carpenter, G. B. Robinson, Jr., and L. J. Bjorklund, U.S. Geological Survey, 1964. No. 9. Ground-water data, Sevier Desert, Utah, by R. W. Mower and R. D. Feltis, U.S. Geological Survey, 1964. No. 10. Quality of surface water in the Sevier Lake basin, Utah, by D. C. Hahl and R. E. Cabell, U.S. Geological Survey, 1965. No. 11. Hydrologic and climatologic data, collected through 1964, Salt Lake County, Utah, by W. V. Toms, R. W. Mower, and C. A. Horr, U.S. Geological Survey, 1966.

INFORMATION BULLETINS

*No. 1. Plan of work for the Sevier River Basin (Sec. 6, P.L. 566), United States Depart­ ment of Agriculture, 1960. No.2. Water production from oil wells in Utah, by Jerry Tuttle, Utah State Engineer's Office, 1960. No.3. Ground water areas and well logs. central Sevier Valley, Utah, by R. "A. Young, United States Geological Survey, 1960.

- 81 - OF UTAH TECHNICAL PUBLICATION NO. 15 ENGI NEER FIGURE 2-A 1966

w y o M H G

'I I

o ••

Fiqu"~ z- B UNITED STATES DEPARTMENT OF THE INTERIOR S' GEOLOGICAL SURVEY S1

EXPLANATION ------.­ Isohyet Shows normal annual precipitation. Interval, in inches, is variable

,..

"

'f

--~ J~_.A.~:"_ " A R Base from U.S. Geological Survey State Base Map, 1959; scale 1:500.000 o 10 I I ~i'l .. r£ z- C,;.

ISOHYETAL lVIAP OF THE

=

---",. \'"

,f-13. 0

I. i I ~/ ...... / I C-.-.__---t",

, b' ~'./ .,-.

o N Isohyetal analysis prepared by the Water Supply Forecast 30 ~o MILES Unit and Office of the State CI imatologist. U.S. Weather I I Bureau. Salt Lake City. Utah. using adjusted cl imatolog­ ical data (1931-60) and values derived by correlation with physiographic factors. F''f'H~ z: - D

LORADO PLATEAU IN UTAH

TE OF UTAH T~CHNICAL fE ENGINEER PUBLICATION NO. 15 FIGURE 9-A 1966

./-----" j fL , {:!'/ .~. , I, I ~-~}- ~' ", "1 15·..:'.'~.od_,! ..s#!rlJr.:"r 1 I 1 1 I I I I /" ". I I 1 \ " I, ...... ---.., c:=.___ I

o' : --t- .• !-­ w " v ~'·"·o·· \ I . ';. p ...... ~" I· - , •5 .•. •5 ,) ___ --t- f

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',4.

'j. •~ . I " I I ~,. "~~.".'" •5 , ...... 1 I o

F'9 ..... r C.C(·6 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY

,-­ ('I ......

EXPLANATION Well symbOl i

"4olas FormatIon .."d rocks of MisSIssIppian aqe ~ j ROCkS of MissISSIPPIan age • Leaavl] Ie Limestone

Number " ....r !ymool Indicates classificatIon of ""ater "amgle (s.e 9. 81. I. fresh: 2. Sllghtl y sal in,,: 3. moderately s.l ine; ll.. 'Iery sal ine; 5. br',ny

"r·:: 1 .~,"~

-. 1 - --·1

,,""-.' .---

--:---~----~------~ .. . ~ ..._"""- --'-..:" '. -", r

, ) "'U'" "..-;"~"a.,~ I .... ' .; _'~..t:-.--~~-__----~------.'.~l--L--=--~~·<-'4.-:-~""..'~-":=:·~--~:"-=-~~:----~:--:---- .. ~ .. :. ,~ '. I ,. I j I ~ . -i,.j~~ .'" " '~:?:r- ~ ~ ~ ~ ~ - -:-2 J ' o " ,:,y~: ' ." ,., r--~ ~~-~ ~~-~: " , , \ - . 0.;, •.•".• '~""-L; .. , -c- . ",,. .... __-+_-~~J__.. - ---'--'

/,"

"" A",' ",,,...., c .- ~ " ." . " L..... ,

\ -'j,

.. \1 1 _ ...... "'. ]70 ...... ----~-.....-_...._~..L.. _"'_ __' ~ I 30

Bot. from U. S GfoloOicol Survey Stoh A Ba .. Map, 19~9; leal. ',~OO,OOO 10

MAP SHOWING LOCATIONS OF WELLS IN ROCKS 0 F;4urcq-~ THE CANYON LANDS AND HIGH PLATEA

!'" ~ .,.

" , '" \ >- \ I I

' .. I

I • l~O 0

.~, _.~ ". ! .:...

J o •3 / .' '. 0 , 'l~o, ',~' ", ". 1 ,; .... \ I i -' I

~

~., ...... on :,< _,~"" ",,"~ ..~T /7>

'. I" L A 5 r" ~H:l ," I

,', .. ' ~~. "f" .. .:.:..:o:.,.... ·.:~r,- .. '. "

z o A

~o 40 MILES

CAlVIBRIAN, DEVONIAN, AND lVIISSISSIPPIAN AGE IN S SECTIONS, COLORADO PLATEAU, UTAH F"yLLrGq- 0

ITE OF UTAH TECHNICAL PUBLICATION NO. 15 TE ENGINEER FI GURE 10 A 1966

~ ,."f- -.-: =::-::---:-~, ••• .r-' .... 1 j I .'~'.-., 1I I j'" , I

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/" \

~-. _."- .,~. , r ;"...,. , ,,· ··,~'r ". _'-s-5. ~~.'

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~,,-----r ~1 \-'\ ~ ~. p \ 7' ''!' p- --_._._-~ o

-01 ., ... ,~ ..._., "I - =-:-.- --: -_~ - r-::.- - .J~_ -,~ ~ . ..;" -";;."'; .~ .;~-'-.'"

1='"'90.41"<::- 10 - B UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY

, ~ 2° EXPLANATION ---., r I '... ~ --' - f__.- ~..... ~ Pattern of well 5prt nq ':;;~;~:1,Jj;r outcrop 'ltater-b••rIl19 unl t .iymDO I symbol /:",

~m-llms~1l, MoenkopI FormatIon. Sinbad Limestone ~ember ~ of "'oenkopi FormatIon. and Kalbab llmeston~

PI< X:a. bab Limestone 0 0- i Pt Toroweag Fonutiot' 9 Peo Co con I no Sandstone -0- Pe Cut1 Sf FOrnlatlon • Pew White Rim S.andstone /l4eft1ber of Cutler 6 e-- FOflfl.t i on - ~ Ped De Chell y Sandstone Member of Cutl er () C>- Formation Peor Org~ Rock Tongue of Cutler Formation O 0- '. ~.~ ·-1" Pee Cedar fo4esa SMldstone Member of Cut I er I!l @- ~" .. f-" Format j on • ...... --.• ~-'to. ...,,~.-ji-- ,'/ u .. ,.<-··...... i Pell Haloal to Tongue of Cutler Formation 0 0- .r ,I" '. (L.-/'. .

1\ ~

__ 5.,,~_ ; -;.... ­ ; , ~ f / .~; ...... ~.- I .~

4 ---.­ --·;-~1 /' . ., ._..~ ,i~·"'·~""·

-.; ...

--!--~-----~------;.

--'.. ~." :

"

"

,£ ··r- .'

00,

3°_~"'O'"

H-__----...~.._:...:!..3-----ccc:----~---"

~., ,.

.. ..:.....------~------_..:..------C'I ~ ...... ~ (_.- .,

.. :

, ----- E

" .-...... i.

'., , il ,-~.. '-:- ----._------­'0

Bas. from U. S G.oloqical Sur •• y Staf. A R 30lt Mop, 19~9; 1«:.He 1500,000 o 10 !

MAP SHOWING LOCATIONS OF 'VELLS AND SPRIN FiilLr~O-c., IN THE CANYON LANDS AND HIGH PLAr

\? -'.'i, '.'

-....-"-, ,~~- ._--.--

:3"~ 0

-r

J. "''''''-' e j 3 ,! ".-..- o - ''- - ...... :.... - - " ._0..-- ""1 " i

'lD "', 5 " s . J. -; r

"

":-OW£L:l ,~ () ~ ,

A pAr 0 7'

z o A Geology from Stokes (196~). Hydroloqy by R. O. Fel tl s. ~o 40 MILES

: IN ROCKS OF PENNSYLVANIAN AND PERMIAN AGE AUS SECTIONS, COLORADO PLATEAU, UTAH Pq~r-c: 10 - D

"E OF UTAH TECHNICAL PUBLICATION NO. IS E ENGINEER FIGURE II_A 1966

,0 ,o· 1 i

..-...... ' '" , '1 -'.. I I I

'. I." ~. ;'( .Jr'l/ r.r

~:,1

.... n;...... ~_ I

o

.,-

,,"'

o

. " , .~, '" , , .; y -- -.-£ ...... ; ~ ...... e i

FiqurL t 1- B UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY

,2° __ (.-' - ~1boo_ ,,,;..c '.~",,"" -.:".-'et!

EXPLANATION

Pattern of Well !l4i ne Sprl ng outcroQ Water-bear, n9 un, t s)'mba I symbQl symbOl

Moss Back ~etnber of Cl'unle Format i on ~. SI''lInan.lmp M01ftber of Chinle o Formation , I Chinle Formation • I -; .J Sinbad Limestone Member of e j MoenkOPI rormatlon - ~oenkotJ I For"'iot t on ., '! lIm-~m$ MoenkopI Formation and Sinb.td -

Numbe,. near symbol Indicates classification of water silIIlple (see p. 81. I, fr,,": 2. sliQhtly saline: 3. moderately SIllne: ~. "ery salIne: S. briny

• I' 'f':'" '.

...... ~'..-I,

I .• .'.' , "

".) - ,~;. ------

~ , -...... '"

II /£ R /{ -.t' ~,', ,- ,I -,-~ ..,-

1 -} 'I'

i 0 ,E

,', ;.. ..f ~\:, o N .' G '';! .,\ - '" fo..· I .....u ':l~"l!,) _"'t_H.,,1

~ ~I -I / 1i " '-.-

--~...

N

.-;...... 1.,.':'1_. I.~(.

Be1. from U. S G.oloqical Survey State A R Ba .. Map, 1959; scalt "500,000 o \0 1

MAP SHO"VING LOCATIONS OF "VELLS, SPRINGS, TE: THE lVIOENKOPI AND CHINLE FORlVIATIONS IN THJ FiqtLr~ I J - c. COLORADO P

, ~.~- ~l "

------,.--,·-:.-.--~--~:r/'7~2f"\l'i..7t~~n'VP..... \ ;>.."?,, ; .. , , " I, .180 0 I

-"-. ". U -A "'N ~~~~- / o ~~f~, I , ,- .f ... • l~ ~. ''\. ('_.~- t._ '\.. I • ,.

,"

, .'4 D r A_I'j..., I 0 ~ ~J . ..,.r- 1 ~-_ _=._.w- ~·_ ~-.-~L~;~~_.~ ~ ~~~: ______~ • j ~__ ~~. 4)70 Ii 0 __ , 10·

Z 0 N A Geoloqy froll StOlees (196~1. ttydroIQ~' by It O. Feltls. 30 40 MILES I

HOLES, AND WATER·YIELDING MINE TUNNELS IN ~ANYON LANDS AND HIGH PLATEAUS SECTIONS, .TEAU, UTAH i=';qu.r<::- U - 0

HE OF UTAH ITE ENGINEER TECHN I CAL PUBL J CAT ION NO. 15 FIGURE 12 -A 1966

, o I 5)' I ~,. I -=\c~ j .~; i , ,

---~- ; , ~'

~'1u,....c I~- 6 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY

EXPLANATION Pat tern 0 f "'ell Spr I"g Water-bear I nq \,In It outcroo i_mbal symbol

[.QC GI en c..".,.on Grau 0 e E",q~1 J"n M.\/ .. ;o S.nastone 0 c>- "k 1(,"'8nt. For"'atlon "" Wi "gAte S.nastone • - "k-"w Kayen ta Format I on ano wingate S"nastone v -

Jb-J

Je-J"n E,.trada and Navajo S~dstones

Je-J"n-.w Entrada. ..." .. jo. ana Wlnqate Sandstones ¢

o W.ll used to construct geol091c uctions

Numaer ne.,. symbol Indicates clauification of lOIahr 'oUIole (s•• p. 8). I I, fres,.: 2. sl,gfttly ,,alIne: 3. tftOder.tel.,. uill".: ~. very ull"": S brIny / 3

Sections shown on fi 9U"" 3. 14. 8. and 16

(2)

._.-­./ \ ; :"","""""; .. ~ '=--­ " ::.~-.¢:- ,\ ~ - ~--...... '- \ Y "--"\ " '1\ >~--"""""'+---- L/"

'--"- -*~=---,. -~

,,, .. ,, ...... _,.,>C .... T :,0 "4'" L

"

LAI

Ba .. f.om U.S G.olaqical Su ..., 5tat. A R Ba .. MOp, 19~9; .col. I'~OO.OOO o 10 I 1

MAP SHOWING LOCATIONS OF WELLS AND SPRINGS F;<1 u r<:.I2,-C- PLATEAU

~ .. ,r..." ,(- ----J--

~ ~ 0 f N

I ~ I i t- ~~

o

z o H A Geoloq, frOlll StOIl'!$ (196'" Hyd ... oloq, by iii. O. F@ttlS o 10 40 MIllS I I

IN THE GLEN CANYON GROUP IN THE COLORADO N UTAH hC1ur.c /2- D

TE OF UTAH rE ENGINEER TECHNICAL PUBLICATION NO. 15 FIGURE 13-A 1966

!,.,!'(,"oH'''. '

> r1 U---:...--:----::-:-::---:-:--:1 ,~. ....,-,'-. I / .~ "'j I ,., , ~.'. '1, I j 1 ,I

~ ...."._--- - -<0.:- J ~1- , /', \ I

,-

o

,.. . 1 '- ~~\J--:~ ( ....

i="i/:iu....c 13- 8 UNITED STATES DEPARTMENT OF THE INTERIOR S GEOLOGICAL SURVEY S'

EXPLANATION Pattern 0 f outcrOQ

Kd-Jw Dakota S.andstone and WInsor Format I on Kdbc-Jm Dakota Sandstone and Burro Canyon and Iobr'" son ~o"".llons Cedar Mountain and Mar!"1 son FOf"matlons

Jm ~rrl son Formation o --< JmO BrUShy BUln Shale ""ember of e Horrl son Formation Jm. lIIestwUer Canyon SanClSlone Memoer at Horrl son Format Ion

Jmr Re<:apture Shal e /l4emOer of Mor'" I son Format I on Jms S.l t W'un SoIlldstOt'le Member vf ~ --< ~ Marr! son FormatIon J. Winsor FormUlon Jb !Ii utf Sandstone e &- J. Entr'df. S~dstone • Jc. Carmel Formd I on ~ - Jm-Jb Morrl son FO("lll.l.tlon and 31utf - Sandstone " Jb..Je 8luff Sandstone and Entrada S~dstone + Jb-Je-J,,"" Bluff. :ntrada. and Nil\lajo $ Sandstones Je-J~n Entr..da and Hav-iojo Sandstones ... Je-J"-n-q Entrada. Navajo. and '141 "9ate S~dstones 4-

"UMaer near symbol Indicates cl.usification of wder $oltllole (s" p. 8). I. fresh: 2. slIghtly saline: J. mOderately sal1fH!:~. "ery saline: S. brIny

A

;.; -

,E cf .' .'. }" o IN E \~ ."I

B01. from U. S G.otoQicol Survty Statt A R Ba .. Map, 19~9; Icat. I~OO,OOO o 10 I I I

MAP SHOWING LOCATIONS OF WELLS, SPRINGS, AND WAT. ENTRADA AND BLUFF SANDSTONES, AND 1.\ F;-qu.rc.13-~ CANYON LANDS AND HIGH PLATEAUS

I ;!~O a ! ~ I

o

GeologJ f'"", Stoke. (196~). z o N A Hydroloqy by R. O. Fel tiS.

30 40 MILES II

~R-YIELDING MINE TUNNELS lL~ THE CARlVIEL FORMATION, ORRISON AND WINSOR FORMATIONS IN THE SECTIONS, COLORADO PLATEAU, UTAH Fi ct l.l.r<:..13- D

fE OF UTAH TECHN I CAL PUBLI CATION NO. 15 °E ENGINEER FIGURE I~-A 1966

, •-< -...

'~ .. ' ...:...... _--.,; - .., -. l<.~.~ , '. , , ~'" .'.- C A N .... y o ," ~c"" o

hqurc I If- 6 UNITED STATES DEPARTMENT OF THE INTERIOR ST GEOLOGICAL SURVEY STI

EXPLANATION Pattern of --'--~-- "ater-bearlng lInl t au tcrop , :j ms Mancos Sl'lal e o ~ " • t ,') .. ~ <.1 'me Etneq S~dstone Member of Mancos Stud e o .". I 8 KIflIII-l(me ,",&lull. Shal e Memoe,. 3nd Emery Sanostone -+- . ~\-. [ Member of Mancos Shal e 'm, Tununk Snale "'Moe,.- of Mancos Shale J'~ S'td Traolc Shale and r)akota SMldstone

'd O&koU Sanastone o 0­ ~ Kdbc Dakota. Sancutone lnd Surro Canyon FormatIon ~ Kbe Burro CoInyon FcrmatLon • [ 'il @- 'em Cedar t40unh.ln 1'=0,.III.tlon ­

Oakotil Sandstone and .'nsor FOl'"matlon

Kdbc-Jm Dakota S.anastof'le and Burro Canyon ano Mar r! son Format I on s

kcm-Jm Cedar MountaIn and Mar,. I son ,Cormatlons

Hum.,.,. neu symbol Indicates Clul,ficatlon of \Olater umoJe (s.. p. 81. 1. fres": 2. 5119"tl., Solilne: 3. moderahlv saline: ~."ery s.ltne: S. brIny

113"

A

I ~ " ~, ".[,:-'-0'"", ...... ',-,. I 'I- C.

":'"":"1-.

~,.

<, . , '- ,,' , . ~-'-l:""'-

0;.""0..... -. 18" ..~~1 _ ~ ------t ~.; t ." . 1 0 ; i ,8 L .. flle 4' S4. :~... •" '1'- .. .- ;- , ; l:. ---<; - " G E ~." '. i '-l -,. ''\I , - . - '" - " r~"" ,"t " -- "

; \"... !

) /

" :.... E

v--. o

Bo .. from U.S, G.ololjieo' Sur .., Sfal. A R 80.. 101011,19'9; leal. I~OO,OOO o 10 I I

MAP SHOWING LOCATIONS OF 'VELLS AND SPRINC FORMATIONS, DAKOTA SANDSTONE, AND l\'IANCO h

L. o

Geol09Y Ir"", Stoke. (196ij). z o N A HydrolOQ1 b, ~. O. Feltl'

30 40 "" ILES , I !

S IN THE CEDAR MOUNTAIN AND BURRO CANYON ; SHALE (EXCEPT FERRON SANDSTONE IHEIHBER) US SECTIONS, COLORADO PLATEAU, UTAH F;c,yfL 1~- D

E OF UTAH TECHH I CAL PUBL I CAT I ON NO. 15 ENGINEER FIGURE IS~A 1966

.3"."""'" "'.).... _-- =2!-

o !,~'. " M' .... , R

;, ...... :...- - ~ . .; -,

-'_f

. l . _-'-~';' , " .' ',."' . ·c A N T"'Y o

A

h'1U"~ 15-0 UNITED STATES DEPARTMENT OF THE INTERIOR STA' GEOLOGI CAL SURVEY STA1

EXPLANATION Pattern of Well tiline outcrop water-oe.r1nq IJni t sy"'bol s'flllbol

~ Kf Ferron Sandstone tolMb.' of Mancos Shal It • -<

Numeer near symbol indIcates c!uaificatlon ot ....ter saJI~l. (se. p. e). I. fresn: 2. slightly saline: 3. IftOderately saline: 14. ¥er'J sali"e; S. briny

.--~-. ..,." -.- _.,' :...,~ ... .. , I --.--tl , 'i~7,~,,(AJl ;- ¥_-;.~ ;...

"._-'.

"I

,-~ ,,;. ''-'~' --;---=-:::----1------:- __ i -" 1 ;1 -'f I --I.

/. .' i A .C \~-- R_ "-r'~'" :'

t··' 1/ ..., -I fl.'''._ :;,.tor Cr_ 1'--"- 'cl...""'iO ...... ,,, .~ ....,.",,_r ;~, ::_~_L __ :~",-·~-=-.:.. ,.~~-':~~~ __ ~._=_~-:< /~-~,.~,L7---- " •• ~. .;;, ',;:: i ~ ..... > ~... ~'r ~-<':: .-11_-- A ",- . • _,,:... ',

< j ~

"" \. •. ,..... 0"'".... Ja o

.E ..j ..""

o N G '.

'~I ., , E ., ,.-,

aalt from U. S. G.aloqical Sur••y Stat. A R Bolt Map, 19~9; Ical. 1500,000 o 10

MAP SHOWING LOCATIONS OF "VELLS AND A " SANDSTONE MEl\'IBER OF THE lVIANCOS SHALE riC/LH"C 15-c.. SECTIONS, COLOR..

-- .-1....- .--:- o

- 0 . . ~-

'-, {"t~ " .. ir I:'",,; ~ Z, - ~" .,. "IO~" --,--_.. _-_ ... -'_." '"" .... ~. " 1. /" " j L t 5 --t"-';'"r", r - i J,

"-" --~.", A :.._---' ~.,,, "' , :'\' ~., .••" .- , , t. ~ ...._~~_,: ..""l ~ :'..., .~>::::'~; ,....: ./ 0. s'" ":., - .i:.' . 7 •• ,., 1\ .-,.. ••' ,~. ..· L.'·' ., .. ," .. :.,; -.. , ....."...,., ... J' ~.~...... ,,' . , ".: ~

z o A

30 40 "'llfS I

\.TER-YIELDING l\'IINE TUNNEL IN THE FERRON IN THE CANYON LANDS AND HIGH PLATEAUS DO PLATEAU, UTAH P'qu.re 15- [)

UNITED STATES DEPARTMENT OF THE INTERIOR STATE OF UTAH TECHN I CAL PUBLI CATION NO. 15 GEOLOGICAL SURVEY SlATE ENGINEER FIGURE 17- A 1966

Ill" 117 0 r~,";,!,' "',"~"Jr, T.'1~, I 11,1 N"r A H I, \ II ,I :,,1i I' '0', ItI c ') "'I 1 1 ',. . " EXPLANATION , ~ r,lll .. , n n! "1 W!"ll ~I n~ ,'1/ I' 1" '..,..,,,, W"lp'-b"", tnQ IHlIt Sp' '''9 ,.',." ' 'I "I r~ n·d<:, no ~ f I lJl A N. r"'bo t ,>,"'!:lol ,;y"'bal u, " Ii'j 'I "".,1 I I, ,>'( I',' , lk,.,h 'I, , ,cp, .f" , [~n:J No' 11', Horn lorma\ 'on 0 0- ! 'I\': ,I 1..,;.,; .. 9, r· .,l J ,I I '<:.1 f ~ , '! " r" rf' Ai I,IPI rt')/ ;T\ilt '0" &-- ~ ~, ~ ~- i_._ ", l' J : 'e: "\ "; [' _.1.',_'__ 8t"l"~h,,~ lormal '0'\ / ;'1~'(, E~ kb -{ ," . I ',a· ,,.., 'I) kb-k .. p h Fn,m~tfon <> ,\ •\I,,' j'" 8lilck awl< ilnd Star POtrl! ~' Sandston" " - \ ,'i I \;I"J': - ./ t"RI l' ;1, II, r-- ~,I- . -0' WKu Aorks of Cr~t"cPOIlS "9" l;nd'Vidf'd I,:: l '\ I I, ,) '--~~':.: ~4,;"L I. J "','" kaIparowits FOtl!\ilt,on ....,:;;\ r-~" -J n 0-:. •• r' \ 1 ' .. 1 ... L_Jl:c'c.._ ' IL b- ---~----t-. ~ I __ 8 u Iropi ( Shal e 0 '~" ~a~~~~0.' ' \i' ,I . ".. ; ~'lrl T'oplc Shalf' and Dakola Sandstont" - , ",- I ,...'~~t:S::~~,~" ." h // M'J"'bl"r ne<1' ~,"'bol indicates classification of waler sample (see p. 8). Iresh: 7. .,1 i9~dly sal ine: 3. modelate!y sal ine: II. very sal ine: S briny I/r·~( i; "~~1tl':"":,C '." A" ! R i ",'" '-; ,>\.. ~i~·f.re,1 ~ j ,: '; '\V ~'Jl.'~\ I ( )~ ~~ ~Ii " ..,r.", ' ,;: . "'" ,,~, ,!.~,. ' -J: ',. , ). I 1130 r,~·~,d "',', ~_~,~~'" J.-~--~"""~.. ,.l~\l:( --,-'~l'-l ''\- ..L 'TKnh , --- "; -..,-,.:::h,.- >';UAP/~?{{f%1!-" ',,11 ~~ ._.", !., , ,.l',h ~ l ",: /..r.l 5'! ',;',' \' J'>" '::nc), I', 'II', . '- i,,'.o:r' 'r "'. ( 'i ~~;\ 'CA-.--' 'i t t ,- ~ ',' , I' l i :,,-. " \ y'-.", ...... ·..,··1,. J.,.l.-~ I. I 'f,. nl".'I,,\1

~ ....; t ~ ~. Q .c r

. ,­ , -

------,. o ~.. . ~ =.... ,,,;.- ti ~ JJ..

~ ~ ! i.,~ • .,)~. '""I,,, II ri',.'. ,~,\ ,j ,., :','1" '~ ~I' ""'.'~~.,~I' • 'f II: , r,q.\7 I. - < I' 1/ • J I{w~, \ ] I +-----.""t '.' - to""'I . ,- _. r .-"',.....- .~ "",. ' -,...... I' .." r,,'I~1 ('trw. .• ' \, "'. ~ / t", ( .• ~ ..;>. - Rr1f1j;mI~fP ,1 ~~ ~ ... ·f... ..,.t,Il

,.::: ;'::. \d II J~ y--, , ...... '''--- _'-111 IJ\: . ._~;,. JJ~lIj\llm,,'i,~

J, \\ ~Ir-~ :-I?f:Mi~~~I;it%f~ I . '~,......

' ,I ,,\ \;' I '!~ ~~J! ' l 1 kws \1 ('1?{') 1\ I\ t" I \ '.I}:; , I (·q\~l'" t I j' ,,\ : 0 II ~ ,~ \' . :'1 ~'J .~~.;..' 'i~.: ;;;'i"'~ kt ,. I. j) 1 I:;' , ...it \ !.(,:r .... r ....I,r/ } I '1.", I Ijt, j , ~. ~ I ~Ifl"" T I I I _ ..... r I' J • \ l_...,M.,j.... *, "'1;'1 {I".. } ( ..4k'tr~Wf , ,. .. :....,:." Lf 'l~::i:l J"" 1 ,( \ "~;,' \ I' \ ,...... ,': \ ~ f I' , 'I l ,,I,.,".,.... 'I .' I'I, I r ...... 1 .' .j, 'J \ ,! t'l J, Jlo·~_I....:...--__.....t.:..:-L1 j_L.I.-_--1- __ ~- 0 1 t 1 0 111 0 - 37 'II '" Bolt hom US G,oloQicol Su,vly S'at. Bolt Mop, 19~9i ,call 1'!500,OOO A R z o N A Geology fro", Sloll~s (196~), HydrohllH by R. D. Felti~. o 10 20 30 40 MILES L_ I .1 II

MAP SHOWING LOCATIONS OF WELLS AND SPRINGS IN ROCKS OF LATE CRETACEOUS AGE (EXCEl DAI{OTA SANDSTONE AND MANCOS SHALE) IN THE HIGH PLATEAUS SECTION, COLORADO PLATEAU, UTAH

UHITED STATES DEPARTMEHT OF THE IHTERIOR STATE OF UTAH TECHHICAL PUBLICATIOH HO. 15 GEOLOGICAL SURVEY STATE ENGINEER FIGURE 18-A 1966

111" Ill" I' If [ r~ f ~ H "' I" 1\\ \f';I J:',,: r)~('" D '. IJ c I '\. '" "'In i ~'.'!. i I ",." !,p, il" ~ .,tH,"t' EXPLANATION ,\." ?: \-RIlVP; "., Pat t e. no' w,'ll 104,1l(> Spr 1"9 Walf'T - b,.". '''Q un' I f ;~ ,• > )), f\ j I r~ [j'1 A N. out crop "'~mb(ll '>.'"t-o I symbnl , U, I '.-, , , ,. i h;",,", ''I' I~ t '" ! ! F I .. r T, IgJlCo',<, 'r:>'~" of l~rt 'ilr. _lQ" .- . ,f'·' G • " ,~" .•.";>'/( 'k'" ,I ' • ,oJ,. I ", , \",:...,. I/:' ",\"'V J'", ,-" J." Ie (rat, Hn Il('w f('. ",,,lion I!TIill .. f'l- l_~;.. \ \,"\ 1//":: .:L<~ I . rf\"'. T. G'ef>n R,vf" r fl' mal, nfl Co' .,..... fig=J I" ,~... '0" I, .\10" 8"~n Hf'ilrf anr1 WA ....lt,h fOHn",t '(H", 0- ,Ihw... 1 S('""101 W""'ill"h formal. ('In 0- "" "j" [lliill " f I "9<,t "If L ""1'<' In'll' (>- i. /.1·_~.. I~ "_t, j ..... (j" ",~ 8 Tl(n'" Norlh Hc"" Fo,m",t,on 0 0-

N1Jl'lhpl np;u .. ,mhol ,nd"-,,,tp<, ,1i1'io<,r11catlon 0' w'II,., <;: t.,

"

f\ R B ri o,-,,; Ii 1\ .. " \. [ '. J. ..;r•• ' \~ I'" / , ','.. i' .,.~, J ", ·.'t ' 1 113 0 ._ ,,,.°,-"0.· " ~_'·~~L ~'L- . ~ -[ . -1 '~r~;:,' h I ,/J "ry:.;~;,;;., C-'1 ",,r '.. i ' ;".:;," "'" r '1'11 .I' '.,c .., ,; .1 I' : .;'j -l.... 1 ~ - t rY.--' , . I( "'" ...... ".1 • <",,', r '. 1 • i ''''.1.-\ 7 '?' ~f -, _~ ':1>. ~ O , /} i -r""'l , f ' oj: !. _ (. ! n,,~ "." ",,), I \ ,~/' ':'.~ '·l ,Il.) r~ ~A. \ ", " \' ./'""..-".,.';... ";1". ."···i ..·0". ; \. \'..'0 ..".:..J1 Ir II J"~l ~ l'.:,'"~. '~--~7"-r/v,llT~' \ j' I [' '" :r I ;"1';.:J , ~'" '."", J W~9714'H. ,,/ ~ (;'), -'-I,A' 'r:- f J'\ ."~i ',".' .J ,.~. •• i" c' '! I'J! I . \, ..' ' :!,' I

;'1 ~ ~ ~ :... . . oa I VJ

r - ~-- ~

, -f . i: 1 ~ K .. ~ ; o -'- .., ./~~;~- " ...... -..~~.: .... -..>. '- ~.. ~,

..

-.3: •• -< -....., , ; . " -, !' <.. . ..-. .:) -J --:.t"~ ..... ';::'. .i ,; -- 1, ~. ~

\, t'i \ "I I, I' I~'~~ 'I, I '!(" ~. ~\q. I"~ \ ,(" ,II 'J. 1 ' :I,~....I II r,Ii,;".' "_,, IJ·'1\t",", •. j.,,' ' .. r;, •. ~ -,'~ , " ';.' , ., ...., ". , :.' - I' ,I '0 n , r _.1 \ L "r "~t6rAI "',,~__ •\'k. I ." •. '- " ',....,.. ", i, I I -' . I 1~,' . I i y ~,_/, t - 'I ~ . I ". , , ". i ,) j '" ./ ... ',', j'lI. '" .( 0' .. ~ J ". . 1: '' :' r." ,,! ( i, ,"" p 'l ' n "'I .....·f·"I 'i. ..;. '! .i, '. ~!. ,\ ." 1 .. I J;~" ',. L,_~ J. .... I',\'j "",iI . t",_ , "I 1 n lll,. Ji'} \, .".. \,;. >" " /1 \ \ '. { $, • i '\ l,.,,', .:! 1,,' i'l/; ' Il!!~~\ .. ! ' ...... '~ ;t.~:. \ I .....' "" ."' ,,' ' 1\ ii, .. ~<:'A,y-; 1-" \ ", l 'R N "~O~"Y_'"'~~_"'( " Ell "0 'f- r· '", " 1" : . ~~~, \' .'~ .... 0' • ~ !,.J.' • '. '1 ! l,0, ," , .• ' I 'j! " i ." i ~' .', \ I'.,. ji ,,' ,\ "'~ .... \ ,' I I :t: r Y'''''' ' \ ~~.r,':" ~. f. , I i '.

11°'

Bo" hom U.S G,oloOicol SurvIY Stat, A R N A Grolo9Y frOIll Stokl!S (196Itl. B... "'.P. 19~9; Icoll t~OO.OOO z o Hydrology by R. O. Ft"1 tis. o 10 20 30 ~O MILE! II -.L_._L J

MAP SHOWING LOCATIONS OF WELLS, SPRINGS, AND WATEn-YIELDING MINE TUNNELS IN ROC OF TERTIARY AGE IN THE HIGH PLATEAUS SECTION, COLORADO PLATEAU, UTAH