DOCSLIB.ORG

Barney Basin, Oregon *

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Barney Basin, Oregon * UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Water-Supply Paper 841 GEOLOGY AND GROUND-WATEB RESOURCES OF THE BARNEY BASIN, OREGON ,x_ BY CS A. M. PIPER, T. W. ROBINSON, AND 0 *£ *~ C. F. PARK, JR. ^ % 3 *^ f 0 ^~ o >->, ,. * * i*u- O WITH A STATEMENT ON fii ® PRECIPITATION AND TREE GROWTH ^ ^ ^ BvL. T. JESSUP C ^ C> * a $ ._____ '">«« CU * en f - Prepared in cooperation with the ' '^, ^o c OREGON AGRICULTURAL EXPERIMENT STATI^ ^ C« W. A. Schoenfeld, Director ,"! » . « DEPARTMENT OF SOILS ^ «} ^j W. L. Powers, Head ""^ -rH ^?- ""*" <^ n. ,^ o co ^s JGQi cr*< r^i ^ »> 5>- ^ ^f" "*, i> -*" ^ <$ -< UNITED STATES 'GOVERNMENT PRINTING OFFICE WASHINGTON i 1939 For eale by the Superintendent of Documents, Washington, D. C, | i ^ i | Prico $1.00 (Papw) CONTENTS Pasre Abstract-_______________ .-___--_____-__-.-_---__-_--_________-_.-_ 1 Introduction. _ _______.____.._..__..____.___..___...._.____.______. 3 Location and extent of the area.__--_._-_____-__--___-_-______-_ 3 Scope of the investigation.______________________________________ 3 Previous investigations.____._---______-_____-_--___________-___ 4 Acknowledgments. ____________________________________________ 4 Climate._________________________________________________________ 5 Precipitation and tree growth in the Haraey Basin, by L. T. Jessup. _.___. 10 Land forms.._____________________________________________________ 13 Drainage system_________.____-__.__-_--_---__--_-___-________-__- 18 Streams ______________________________________________________ 18 Lakes..-______---___-_----_---------_--_------_---_---_------ 20 Geology------_-__------_----------------------------------------- 23 Sequence and general features of the rocks._______________________ 23 Summary of geologic history _____________________________________ 26 Physical character and water-bearing properties of the strata- _ ______ 29 Valley fill ---_----_----_-------------_-_-_--------__--_ 29 Physical character and thickness._______________________ 29 Water-bearing properties. __--_______-_--____--____----_ 33 Late basalt and basaltic ejectamenta______________-___--___-_ 36 Harney formation, _______..____.___.____-.___-________.___ 38 Fanglomerate near Coffeepot Creek-_________________________ 41 Danforth formation.-__._..-_________-._________-_____-_--_ 43 Physical character.____________________________________ 43 Stratigraphic relations, thickness, and age___-_--_________ 47 Water-bearing properties. ______________________________ 49 Steens basalt_-____-.__.__.------___._________-_-_______-__ 49 Older siliceous extrusive rocks.__________.___________________ 51 Pre-Tertiary rocks, undifferentiated._.___-_-_______-____-_--_ 52 Geologic structure______________________________________________ 53 General features_______.__----_______.____.___________ _-__ 53 Faults___-_-_-_-__._.._._______...._._._.__..__.._-_ 54 Folds. _____ . _.._...._.._._ ._.... -. .........._. 56 Epochs of deformation and mechanics of faulting._____________ 56 Water in the valley fill___...__.__.....-______._._.________.___.__.. 58 Unconfined water in the shallow pervious beds.___-____-____- _--- 58 Form, depth, and fluctuations of the water table_-__.__._____. 58 Source and disposal of the unconfined ground water.__________ 63 Confined water in the deep pervious beds._________________________ 65 Form and depth of the piezometric surface.___________________ 65 Fluctuations of the piezometric surface---____-_______--_-__-_ 66 Source and disposal of the confined water_.___________________ 69 in IV CONTENTS Water in the valley fill Continued. Page Subdivisions of the alluvial plain________________________________ 72 Silvies subarea__.___________________________._____________ 72 General hydrologic features.____________________________ 72 Recharge of the valley fill_____-________________________ 74 Estimates based on ground-water storage.____________ 74 Estimates based on ground-water discharge ___________ 76 Estimates based on source and disposal of soil water. __ 78 Summary of estimates of recharge ___________________ 82 Recovery of ground water._____________________________ 82 Economic requirements___________________________ 82 Recovery of water from the shallow pervious beds. _ _ _ _ 83 Recovery of water from the deep perviour beds_______ 85 Pumpage, 1927 to 1931_______________________ 85 Permeability and transmission capacity of the deep pervious beds_______________________________ 87 Safe yield of the valley fill in the Silvies subare^.. __________ 89 Flowing wells in the Silvies subarea._____________________ 90 Minor subareas north of Malheur Lake_____________________ 90 Donner und Blitzen Valley_________________________________ 92 Warm Spring VaUey_____________________________ 93 Water in the bedrock______________________________________________ 94 General features.______________________________________________ 94 Slightly thermal water near Burns.______________________________ 97 Occurrence _______________________________________________ 97 Recovery by pumping from wells____________________________ 98 Slightly thermal water in the southern part of the basin.____________ 100 Thermal water of intermediate temperature.______________________ 102 Hot water.___________________________________________________ 105 Relation of the thermal water to geologic structure._______________ 106 Recovery of thermal water from springs and wells _________________ 108 Chemical character of the ground water in relation to use for irrigation.___ 111 Appendix_____________-_____--____---_-_--_-__-___-_-__-___----- 114 Chemical constituents of representative waters from the Harney Basin ______________________________________________________ 114 Records of discharge by streams in the Harney Basin, 1903-32_______ 120 Monthly run-off, in acre-feet, of streams in the Harney Basin________ 121 Staff gages in Malheur Lake---.__-_--_-_----_-____-____-------_- 128 Altitude of water surface at staff gages in Malheur Lake, 1903-32____ 129 Altitude of water surface in Harney Lake, 1912-18-_______________ 131 Altitude of water surface at staff gages on streams ir the Harney Basin, 1930-32_____________---_--_ ___ _ __-- 132 Drillers' records of wells in the Harney Basin______________________ 133 Hydrologic data for representative wells in the Harney Basin._______ 137 Measurements of depth to water in observation wells in the Harney Basin, 1928-32.__._____________________________ 152 Hydrologic data for springs in the Harney Basin__________________ 181 Records of discharge from major springs in the Harney Basin, 1902-32. 184 ___-______.____________--_---_.__---_-_-__-__-_-_----_---- 187 ILLUSTRATIONS Page PLATE 1. Map of part of southeastern Oregon showing extent of the Harney Basin..____--__---___..__--_---_-----__-_---_--- 2 2. Geologic map of the Harney Basin, Harney County, Oreo;,- In pocket 3. A, Harney Playa, view southeastward from lot 3, s^c. 28, T. 26 S., R. 30 E.; B, Shingled beaches along the southern ,edge of Harney Lake-___-__________-__________..______-_ 14 4. A, Portal of Malheur Cave; B, Erosion trench on tongue of Voltage lava field-______--________--_-__-_____-___-__-- 14 5. A, Glaciated valley of upper Kiger Creek; B, Malheur Gap viewed from the central alluvial plain east of Malheur Lake 14 6. Area and capacity curves for Malheur, Mud, and Harney Lakes.,..______________________________________ 22 7. Altitude of water surface of Malheur and Harney Lakes, 1903 to 1931________-_____________-____-__-___ 22 8. A, Exposure of 10-inch layer of volcanic ash in the valley fill in east bank of Newman Slough; B, Stratified sediments under­ lying the tuff-breccia member of the Danforth formation..-. 42 9. A, Exposure of basaltic-breccia member of the Danforth forma­ tion in the NW# sec. 23, T. 28 S., R. 30 E.; B, Bluff exposing lacustrine and alluvial sediments east of Harney Lake_-_-_- 43 10. East face of the "high" Steens Mountain, an eroded fault scarp. 58 11. Hydrographs showing fluctuations of the water surface in the Silvies River near Burns and in four shallow wells in the valley fill, 1930-31 and 1931-32_________._____________________ 58 12. Map showing approximate change in ground-water levelf in the central part of the Harney Basin from October 1931 to May 1932_________________________________________________ 66 13. Map showing approximate difference in head between the uncon- fined water and the confined water in the valley fill in the central part of the Harney Basin in October 1931 and. May 1932_ _________ ..... _________________________ 66 14. Hydrographs showing fluctuations of the water level in three pairs of companion wel's in the valley fill, 1930-31 and 1931-32.____________________________________________ 66 15. Hydrographs showing effect of pumping from wel] 94 on the static level in three deep wells and one shallow well in the valley fill__-______________________________________ 66 16. Diagrammatic summary of operation of the 87-foot well at the Harney Branch Experiment Station, 1931_______________ 90 17. Map of the northwestern lobe of the central alluvial plain, showing contours on the piezometric surface for the water in the deep valley fill, 1931-_________._____________________ 90 V VI ILLUSTRATIONS Fag« PLATE 18. Diagrammatic summary of operation of the 218-foot well at the Harney Branch Experiment Station, 1931- ___-___-.____ 106 19. A, Sodhouse Spring, near the south margin of Malheur Lake; B, Crane Creek, or Hughet Spring_____-_________________ 106 20. A, "Sulphur" spring
Load more

Recommended publications
  • The Geological Newsletter
    JAN 90 THE GEOLOGICAL NEWSLETTER ·• GEOLOGICAL SOCIETY OF THE OREGON COUNTRY GEOLOGICAL SOCIETY Non-Profit Org. U.S. POSTAGE OF THE OREGON COUNTRY PAID P.O. BOX ?a 7- Portland, Oregon PORTLAND, OR 97207- -:· ·--~··, Permit No. 999 - -- '~ Dr. Frank Boersma 120 W. 33~d Street Vancouver, WA 98660 GEOLOGICAL SOCIETY OF THE OREGOt\ COllNTRY 1989-1990 ADMINISTRATION BOARD OF DIRECTORS President Directors Rosemary Kenney 221-0757 Peter E. Baer (3 years) 661-7995 4211 S\-1 Condor Charlene Holzwarth (2 years) 284-3444 Portland, OR 97201 Esther Kennedy (1 year) 287-3091 Vice President Margaret L. Steere 246-1670 Immediate Past Presidents Joline Robustelli 223-2852 6929 SW 34 Ave. ~ Portland, OR 97219 R.E. (Andy) Corcoran 244-5605 Secretary Alta B. Fosback 641-6323 THE GEOLOGICAL NEWSLETTER 8942 SW Fairview Place Tigard, OR 97223 Editor: Sandra Anderson 775-5538 Treasurer Calendar: Margaret Steere 246-1670 Braden Pillow 659-6318 Business Manager: Carol Cole 220-0078 19562 SE Cottonwood St. Assist: Cecelia Crater 235-5158 Milwaukie, OR 97267 ACTIVITIES CHAIRS Calligrapher Properties and PA System Wallace R.· McClung 637-3834 (Luncheon) Donald Botteron 245-6251 Field Trips (Evening) Walter A. Sunderland 625-6840 Charlene Holzwarth 284-3444 Publications Alta B. Fosback 641-6323 Geneva E. Reddekopp 654-9818 Geology Seminars Publicity Donald D. Barr 246-2785 Roberta L. Walter 235-3579 Historian Refreshments Phyllis G. Bonebrake 289-8597 (Friday Evening) Hospitality David and Marvel Gillespie 246-2368 254-0135 (Luncheon) Margaret Fink 289-0188 Harold and Patricia Gay Moore (Evening) Maxine Harrington 297-ll86 (Geology Seminars) Catherine Evenson 654-2636 Library: Esther Kennedy 287-3091 ' ' Betty Turner 246-3192 Telephone n Past Presidents Panel Jean L.
    [Show full text]
  • Diamond Craters Oregon's Geologic
    Text by Ellen M. Benedict, 1985 Features at stops correspond to points on a clock ago, a huge mass of hot gases, volcanic ashes, bits face. Imagine that you are standing in the middle of a of pumice and other pyroclastics (fire-broken rock) Travel And Hiking Hints clock face. Twelve o’clock is the road in front of you violently erupted. The blast – greater than the May and 6 o’clock the road behind. If you always align the 18, 1980, eruption of Mt. St. Helens – deposited a Diamond Craters is located in the high desert country clock face with the road, you should be able to locate layer of pyroclastics 30 to 130 feet thick over an area about 55 miles southeast of Burns, Oregon. It’s an the features. almost 7,000 square miles! isolated place and some precautions should be taken . when traveling in the area. Start Tour. Mileage begins halfway Pyroclastics are between milepost 40 and 41 on State normal behavior Diamond Craters has no tourist facilities. The nearest Highway 205 at the junction to Diamond. for magmas place where gasoline is sold is at Frenchglen. Turn left. (subsurface That’s the opinion held by scores of molten rocks) Keep your scientists and educators who have visited Diamond, Oregon, a small ranching community, was of rhyolitic (a vehicle on named in 1874 for Mace McCoy’s Diamond brand. volcanic material and studied the area. It has the “best and hard-packed The nearby craters soon became known as Diamond related to granite) most diverse basaltic volcanic features in the road surfaces Craters.
    [Show full text]
  • Diamond Pond, Harney County, Oregon: Vegetation History and Water Table in the Eastern Oregon Desert
    Great Basin Naturalist Volume 47 Number 3 Article 7 7-31-1987 Diamond Pond, Harney County, Oregon: vegetation history and water table in the eastern Oregon desert Peter Ernest Wigand Washington State University, Pullman, Washington Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Wigand, Peter Ernest (1987) "Diamond Pond, Harney County, Oregon: vegetation history and water table in the eastern Oregon desert," Great Basin Naturalist: Vol. 47 : No. 3 , Article 7. Available at: https://scholarsarchive.byu.edu/gbn/vol47/iss3/7 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. DIAMOND POND, HARNEY COUNTY, OREGON VEGETATION HISTORY AND WATER TABLE IN THE EASTERN OREGON DESERT Peter Ernest Wigand' Abstract —Cores obtained in 1978 from Diamond Pond, Diamond Craters, Harney County, Oregon, as part of the Steens Mountain Prehistory Project, provide a record of vegetation change on the sagebrush/shadscale ecotone and of local and perhaps regional water tables. Pollen, macrofossils, sediments, and charcoal from these radiocarbon-dated cores were analyzed. Varying abundance ofjuniper, grass, sagebrush, and greasewood pollen, and of aquatic to littoral plant macrofossils reflects changing regional effective moisture and local water table since 6000 B. P. Eleven dates spanning 5200 radiocarbon years and four regionally correlated volcanic ashes establish the dating of seven periods of diflferent moisture regimes; 1. Greasewood and saltbush pollen dominance before 5400 B.P.
    [Show full text]
  • PDF Linkchapter
    Index [Italic page numbers indicate major references] Abajo Mountains, 382, 388 Amargosa River, 285, 309, 311, 322, Arkansas River, 443, 456, 461, 515, Abort Lake, 283 337, 341, 342 516, 521, 540, 541, 550, 556, Abies, 21, 25 Amarillo, Texas, 482 559, 560, 561 Abra, 587 Amarillo-Wichita uplift, 504, 507, Arkansas River valley, 512, 531, 540 Absaroka Range, 409 508 Arlington volcanic field, 358 Acer, 21, 23, 24 Amasas Back, 387 Aromas dune field, 181 Acoma-Zuni scction, 374, 379, 391 Ambrose tenace, 522, 523 Aromas Red Sand, 180 stream evolution patterns, 391 Ambrosia, 21, 24 Arroyo Colorado, 395 Aden Crater, 368 American Falls Lava Beds, 275, 276 Arroyo Seco unit, 176 Afton Canyon, 334, 341 American Falls Reservoir, 275, 276 Artemisia, 21, 24 Afton interglacial age, 29 American River, 36, 165, 173 Ascension Parish, Louisana, 567 aggradation, 167, 176, 182, 226, 237, amino acid ash, 81, 118, 134, 244, 430 323, 336, 355, 357, 390, 413, geochronology, 65, 68 basaltic, 85 443, 451, 552, 613 ratios, 65 beds, 127,129 glaciofluvial, 423 aminostratigraphy, 66 clays, 451 Piedmont, 345 Amity area, 162 clouds, 95 aggregate, 181 Anadara, 587 flows, 75, 121 discharge, 277 Anastasia Formation, 602, 642, 647 layer, 10, 117 Agua Fria Peak area, 489 Anastasia Island, 602 rhyolitic, 170 Agua Fria River, 357 Anchor Silt, 188, 198, 199 volcanic, 54, 85, 98, 117, 129, Airport bench, 421, 423 Anderson coal, 448 243, 276, 295, 396, 409, 412, Alabama coastal plain, 594 Anderson Pond, 617, 618 509, 520 Alamosa Basin, 366 andesite, 75, 80, 489 Ash Flat, 364 Alamosa
    [Show full text]
  • STATE of OREGON DEPARTMENT of GEOLOGY and MINERAL INDUSTRIES • the Ore Bin •
    Volume 26, No. 9 September, 1964 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES • The Ore Bin • Published Monthly By STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Head Office: 1069 State Office Bldg., Portland, Oregon - 97201 Telephone: 226 - 2161, Ext. 488 Field Offices 2033 First Street 239 S. E. "H" Street Baker Grants Pass Effective January 1, 1964 Subscription rate $1.00 per year. Available back issues 10 cents each. * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * Second class postage paid at Portland, Oregon * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * GOVERNING BOARD Frank C. McColloch, Chairman, Portland Fayette I. Bristol, Grants Pass Harold Banta, Baker STATE GEOLOGIST Hollis M. Dole GEOLOGISTS IN CHARGE OF FIELD OFFICES Norman S. Wagner, Baker Len Ramp, Grants Pass * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * Permission is granted to reprint information contained herein. Any credit given the Oregon State Department of Geology and Mineral Industries for compiling this information will be appreciated. The ORE BIN Volume 26, No. 9 September, 1964 OREGON'S MINERAL INDUSTRY ZOOMS UPWARD By Ralph S. Mason* With a 19.4 percent increase in the value of minerals produced compared to 1962, Oregon mineral production rocketed to an all-time high of $62, 700,000 in 1963. As usual, industrial minerals accounted for the bulk of the state's mineral wealth, with stone and sand and gravel representing near- ly 69 percent of the total. The vast increase in production value resulted primarily from the mining of increased quantities of raw matrials, plussmall increases in the unit values of the commodities. The low values placed on stone ($1.20 per to_ n)and sand and gravel ($1.22 per ton) in the U.S.
    [Show full text]
  • Morphology and Dynamics of Inflated Subaqueous Basaltic Lava Flows
    Morphology and dynamics of inflated subaqueous basaltic lava flows Anne Deschamps, C´ecileGrign´e,Morgane Le Saout, Samuel Adam Soule, Pascal Allemand, Brigitte Van Vliet Lanoe, France Floc'H To cite this version: Anne Deschamps, C´ecileGrign´e,Morgane Le Saout, Samuel Adam Soule, Pascal Allemand, et al.. Morphology and dynamics of inflated subaqueous basaltic lava flows. Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2014, 15 (6), pp.2128-2150. <10.1002/2014GC005274>. <insu-01003996> HAL Id: insu-01003996 https://hal-insu.archives-ouvertes.fr/insu-01003996 Submitted on 9 Dec 2014 HAL is a multi-disciplinary open access L'archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destin´eeau d´ep^otet `ala diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publi´esou non, lished or not. The documents may come from ´emanant des ´etablissements d'enseignement et de teaching and research institutions in France or recherche fran¸caisou ´etrangers,des laboratoires abroad, or from public or private research centers. publics ou priv´es. PUBLICATIONS Geochemistry, Geophysics, Geosystems RESEARCH ARTICLE Morphology and dynamics of inflated subaqueous basaltic lava 10.1002/2014GC005274 flows Key Points: Anne Deschamps1,Cecile Grigne1, Morgane Le Saout1, Samuel Adam Soule2, Pascal Allemand3, Inflated lava flows are reported in Brigitte Van Vliet Lanoe1, and France Floc’h1 aerial and subaqueous environments The presence of water during flow 1Universite de Brest, UMR CNRS-6538 Domaines Oceaniques, Institut Universitaire Europeen de la Mer, Plouzane, France, inflation influences its final 2 morphology Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA, 3 € In water, more efficient cooling and Laboratoire de Geologie de Lyon-OSU de Lyon, Universite Lyon 1 et ENS-Lyon, 2 rue Raphael Dubois, Villeurbanne, buoyancy enhances lava inflation France Correspondence to: A.
    [Show full text]
  • Canada and Western U.S.A
    Appendix B – Region 12 Country and regional profiles of volcanic hazard and risk: Canada and Western U.S.A. S.K. Brown1, R.S.J. Sparks1, K. Mee2, C. Vye-Brown2, E.Ilyinskaya2, S.F. Jenkins1, S.C. Loughlin2* 1University of Bristol, UK; 2British Geological Survey, UK, * Full contributor list available in Appendix B Full Download This download comprises the profiles for Region 12: Canada and Western U.S.A. only. For the full report and all regions see Appendix B Full Download. Page numbers reflect position in the full report. The following countries are profiled here: Region 12 Canada and Western USA Pg.491 Canada 499 USA – Contiguous States 507 Brown, S.K., Sparks, R.S.J., Mee, K., Vye-Brown, C., Ilyinskaya, E., Jenkins, S.F., and Loughlin, S.C. (2015) Country and regional profiles of volcanic hazard and risk. In: S.C. Loughlin, R.S.J. Sparks, S.K. Brown, S.F. Jenkins & C. Vye-Brown (eds) Global Volcanic Hazards and Risk, Cambridge: Cambridge University Press. This profile and the data therein should not be used in place of focussed assessments and information provided by local monitoring and research institutions. Region 12: Canada and Western USA Description Region 12: Canada and Western USA comprises volcanoes throughout Canada and the contiguous states of the USA. Country Number of volcanoes Canada 22 USA 48 Table 12.1 The countries represented in this region and the number of volcanoes. Volcanoes located on the borders between countries are included in the profiles of all countries involved. Note that countries may be represented in more than one region, as overseas territories may be widespread.
    [Show full text]
  • Trends in Maar Crater Size and Shape Using the Global Maar Volcano Location and 1 Shape
    1 Title: Trends in maar crater size and shape using the global Maar Volcano Location and 2 Shape (MaarVLS) database 3 Authors: Graettinger, A.H. 1 4 Affiliation: 1Department of Geosciences, 5110 Rockhill Road, Flarsheim Hall 420, University of 5 Missouri Kansas City, Kansas City, Missouri, 64110, USA 6 [email protected] 7 8 Abstract 9 A maar crater is the top of a much larger subsurface diatreme structure produced by 10 phreatomagmatic explosions and the size and shape of the crater reflects the growth history of 11 that structure during an eruption. Recent experimental and geophysical research has shown 12 that crater complexity can reflect subsurface complexity. Morphometry provides a means of 13 characterizing a global population of maar craters in order to establish the typical size and 14 shape of features. A global database of Quaternary maar crater planform morphometry 15 indicates that maar craters are typically not circular and frequently have compound shapes 16 resembling overlapping circles. Maar craters occur in volcanic fields that contain both small 17 volume and complex volcanoes. The global perspective provided by the database shows that 18 maars are common in many volcanic and tectonic settings producing a similar diversity of size 19 and shape within and between volcanic fields. A few exceptional populations of maars were 20 revealed by the database, highlighting directions of future research to improve our 21 understanding on the geometry and spacing of subsurface explosions that produce maars. 22 These outlying populations, such as anomalously large craters (> 3000 m), chains of maars, 23 and volcanic fields composed of mostly maar craters each represent a small portion of the 24 database, but provide opportunities to reinvestigate fundamental questions on maar formation.
    [Show full text]
  • Harney Area Cultural Resources Class I Inventory
    Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1980 Harney area cultural resources class I inventory Ruth McGilvra Bright Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Archaeological Anthropology Commons, Cultural Resource Management and Policy Analysis Commons, and the Geography Commons Let us know how access to this document benefits ou.y Recommended Citation McGilvra Bright, Ruth, "Harney area cultural resources class I inventory" (1980). Dissertations and Theses. Paper 3264. https://doi.org/10.15760/etd.3255 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. AN ABSTRACT OF THE THESIS OF Ruth McGilvra Bright for the Master of Arts in Anthropology presented August 7, 1980. Title: Harney Area Cultural Resources Class I Inventory. APPROVED BY MEMBERS OF THE THESIS COMMITTEE: Daniel Scheans Gordon ;OoB ~i ,_,,I This document presents the Cultural Resources Overview for the Harney Area in southeastern Oregon. The Harney Area combines three of the four planning units in the Burns Bureau of Land Management District. Most of the land in the Harney Area is located in Harney County, although a few parcels are just outside the county line in Lake and Malheur Counties. Almost all of Harney County is included. There are approximately 3,320,000 acres of Bureau administered public land within the Harney Area, as well as other public and private lands.
    [Show full text]
  • STATE of OREGON DEPARTMENT of GEOLOGY and MINERAL INDUSTRIES • the Ore Bin •
    Vol. 28, No. 7 July, 1966 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES • The Ore Bin • Published Monthly By STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Head Office: 1069State Office Bldg., Portland, Oregon - 97201 Telephone: 226 - 2161, Ext. 488 Field Offices 2033 First Street 239 S. E. "H" Street Baker Grants Pass Effective January 1, 1964 Subscription rate $1.00 per year. Available back issues 10 cents each. * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * Second class postage paid at Portland, Oregon * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * GOVERNING BOARD Frank C. McColloch, Chairman, Portland Fayette I. Bristol, Grants Pass Harold Banta, Baker STATE GEOLOGIST Hollis M. Dole GEOLOGISTS IN CHARGE OF FIELD OFFICES Norman S. Wagner, Baker Len Ramp, Grants Pass * * * * ** * * * * * * ** * ** * * * * * * * ** * * * * ** ** * * * * * * * * ** * ** * Permission is granted to reprint information contained herein. Any credit given the Oregon State Department of Geology and Mineral Industries for compiling this information will be appreciated. The ORE BIN Volume 28, No. 7 July, 1966 ENERGY AND POWER OF GEOTHERMAL RESOURCES By Gunnar Bodvarsson* Department of Mathematics and Department of Oceanography Oregon State University, Corvallis, Oregon Introduction Geothermal resources are now being utilized for power generation and building heating in a number of locations in the world (see companion ar- ticle by Groh). This industry is of a rather recent origin and has not yet been developed to its full capacity. A great number of undeveloped geo- thermal areas are found in various locations, mainly in the Circum-Pacific Belt. The State of Oregon obviously has a number of geothermal prospects. The geothermal industry has many procedures and principles in com- mon with the petroleum industry, although there are, as a matter of course, a number of peculiarities resulting from the special thermal processes in- volved.
    [Show full text]
  • Crack in the Ground Reports
    Volume 26, No. 9 September, 1964 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES CRACK-IN-THE-GROUND, LAKE COUNTY, OREGON By Norman V. Peterson* and Edward A. Groh** Open cracks or fissures in the earth's surface are notuncommon; they occur fairly often as a result of earthquakes or volcanic activity, but they usual­ ly become filled with rock rubble or lava and disappear in a very short ti me. A large fissure that stays open for hundreds of years is, therefore, a rare feature. Such a fissure occurs in a remote part of central Oregon. It is a deep, narrow rift about 2 miles long, and it has remained open for perhaps a thousand years. For lack of any official name for it, the feature is referred to simply as "Crack-in-the-Ground. 11 Location and History Crack-in-the-Ground is situated in northern LakeCounty in T.26 S., R. 17 E. As shown on the accompanying geologic sketch map (plate l), it can be traced from the southwest edge of the Four Craters lava field diagonally to the southeast until it disappears in lake sediments that mark the north shoreline of prehistoric Christmas Lake. The feature can be reached by road, but the last few miles are not suitable for cars with low road clearance. The route starts from the east side of Sil ver Lake on Oregon Highway 31. From this point the course leads 19 miles northeast on a paved road to Christmas Valley Lodge, then east on a graveled road l mile and north on a graded dirt road 4 miles.
    [Show full text]
  • Volcano Type: Stratovolcano Composition: Andesite Most Recent Eruption: 6,700 Years Ago Threat Potential: High Glacier Peak
    High to Very High Threat Potential Low to Very Low Threat Potential WASHINGTON Mount Jefferson Mount Baker Belknap Glacier Peak Black Butte Crater Lava Field Mount Rainier Blue Lake Crater Mount St. Helens Cinnamon Butte Mount Adams Craters of the Moon Volcanic Field OREGON Davis Lake Volcanic Field Mount Hood Devils Garden Lava Field Three Sisters Diamond Craters Volcanic Field Newberry Volcano Four Craters Lava Field Crater Lake Hell's Half Acre Lava Field CALIFORNIA Indian Heaven Volcanic Field Medicine Lake Volcanno Jordan Craters Volcanic Field Mount Shasta Lava Mountain Lava Field Lassen Peak Sand Mountain Volcanic Field Moderate Threat Potential Wapi Lava Field Mount Bachelor West Crater Volcanic Field Mount Baker Location: Washington, Whatcom County Latitude: 48.777° N Longitude: 121.813° W Elevation: 3,286 (m) 10,781 (f) Volcano type: Stratovolcano Composition: Andesite Most recent eruption: 6,700 years ago Threat Potential: High Glacier Peak Location: Washington, Snohomish County Latitude: 48.112° N Longitude: 121.113° W Elevation: 3,213 (m) 10,541 (f) Volcano type: Stratovolcano Composition: Dacite Most recent eruption: 1,100 years ago Threat Potential: High * Mount Rainier Location: Washington, Pierce County Latitude: 46.853° N Longitude: 121.76° W Elevation: 4,392 (m) 14,410 (f) Volcano type: Stratovolcano Composition: Andesite to Dacite Most recent eruption: ∼1,000 years ago Nearby towns: Orting, Seattle, Tacoma, Yakima Threat Potential: High Mount St. Helens Location: Washington, Skamania County Latitude: 46.2° N Longitude:
    [Show full text]