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Preliminary Geologic of the Ruidoso Quadrangle Tad - Andesite/diorite dike, undivided (Oligocene) NOTES AND ACKOWLEDGEMENTS

A DIVISION OF NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY within Mescalero Tribal lands north of the Rio Ruidoso in the northwest NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES OF-GM-93 Tmz - Monzonite (?) dike (Oligocene) NMBGMR Open-file Map Series 105°45'0"W 105°42'30"W 105°40'0"W 105°37'30"W corner of the quadrangle was compiled from Moore et al (1988b). Geology within OFGM 93 430000 431000 432000 433000 434000 435000 436000 437000 438000 439000 440000 441000 442000 Mapped and compiled by Geoffrey Rawling Mescalero Tribal lands south of US 70 and east of Fence Canyon was compiled from Cenozoic Sedimentary Rocks Moore et al (1988a). Last Modified 26 April 2006

3693000 3693000 EXPLANATION OF MAP UNITS Tcm - Cub Mountain Formation (Eocene) I thank Thora Padilla of the Mescalero Apache Tribe for granting access to tribal 33°22'30"N 23 lands and Ernest Kadayso for escorting me. Dan Abercrombie of the US Department of Tsv- Tsv-tf Qg A 15 Kd@sr 33°22'30"N (for detailed unit descriptions, see accompanying report) tp 10 12 Pg Pg D Mesozoic Sedimentary Rocks Agriculture facilitated the access to the Mescalero Lands. Doug Rappuhn of the New 16 Kmv Qg Kmv - Cretaceous Mesa Verde Group, undivided (upper Cretaceous) Tsv 32 Pg Mexico State Engineer’s Office kindly provided lithologic logs of water wells in the Kd 28 Pg Kmv Km 32 Ruidoso area. 21 @sr Anthropogenic Deposits 22 H 0505S Km - Mancos Shale (middle to upper Cretaceous) 83 85 Qvf 14 af Artificial fill 32 Pg 86 25 Kd - Dakota Sandstone (lower to middle Cretaceous) REFERENCES CITED AND SELECTED REFERENCES Qvf H 02925 daf Heavily disturbed land and/or artificial fill. 7 11 Km 88 Psa PERTINENT TO THE STUDY AREA 3692000 13 3692000 @sr - Santa Rosa Formation (upper Triassic) Kmv 28 88 D' Ash, S. R., and Davis, L. V., 1964, Guidebook of the Ruidoso Country: New Mexico 10 Quaternary and Tertiary Surficial Deposits Tsv H 01635 Tmz 82 Psa 81 Geological Society, Guidebook 15, 189 p. 70 18 23 10 15 Kmv QHa - Alluvium (Holocene to Historic) Paleozoic Sedimentary Rocks Barker, J. M., Kues, B. S., Austin, G. S., and Lucas, S. G., 1991, Geology of the Sierra Psa Kmv 10 6 Qvf Pg - Grayburg Formation (upper Permian) Blanca, Sacramento, and Capitan Ranges: New Mexico Geological Society, 9 Qvf 83 16 78 20 Qvf - Valley fill (upper Pleistocene to Holocene) Guidebook 42, 362 p. 86 Psa 73 19 Psa - San Andres Formation (middle to upper Permian) Cather, S. M., 1991, and provenance of Upper Cretaceous and Paleogene Qvf Kd Pg Qrt3 - Lowest terrace deposit of Rio Ruidoso (Holocene) strata of the western Sierra Balca Basin, New Mexico, in Barker, J. M., Kues, B. Qvf Tsv Py - Yeso Formation (middle Permian) S., Austin, G. S., and Lucas, S. G., eds., Geology of the Sierra Blanca, 3691000 18 16 Psa 3691000 Qrt2 - Middle terrace deposit of Rio Ruidoso (upper Pleistocene) Sacramento, and Capitan Ranges: New Mexico Geological Society, Guidebook H 03388 15 75 20 P\u - Permian to Proterozoic rocks 42, p. 265-275. 58 11 Qvf Qrt1 - Upper terrace deposit of Rio Ruidoso (middle Pleistocene) Kelley, V. C., 1971, Geology of the Pecos Country, Southeastern New Mexico: New 20 90 20 @sr 15 Psa Mexico Bureau of Mines and Mineral Resources Memoir 24, 75 p. Psa 4 Qaf - Alluvial fan deposits (middle to upper Pleistocene) MAP AND CROSS SECTION SYMBOLS Moore, S. L., Foord, E. E., and Meyer, G. A., 1988a, Geologic and aeromagnetic map of H 02178 25 15 23 A A Location of geologic cross section a part of the Mescalero Apache Indian Reservation, Otero County, New Mexico: 80 Qls - Landslide deposits (lower to middle Pleistocene?) 9 27 U. S. Miscellaneous Investigations Series Map I-1775, 57 Geologic contact, solid where exposed, dashed where approximately H 02096 Psa ? 1:50000 scale. Kmv 17 000 000 Qg - Stream gravel deposits (lower to middle (?) Pleistocene) located, dotted where concealed, queried where inferred 3690 24 23 30 3690 Moore, S. L., Foord, E. E., Meyer, G. A., and Smith, G. W., 1988b, Geologic Map of the Km northwestern part of the Mescalero Apache Indian Reservation, Otero County, 56 21 16 H 01518 Qvf ? Normal , arrow shows dip and dip direction of fault plane where Tsv 15 10 17 15 QTg - Pediment gravel deposits (Pliocene (?) – lower Pleistocene) New Mexico: U. S. Geological Survey Miscellaneous Investigations Series Map 26 H 02623 Pg measured, ball and bar on downthrown side, dashed where 15 25 34 approximately located, dotted where concealed. Fault tip is queried I-1895, scale 1:24000. 17 9 QTgg - Glacial outwash gravel (Pliocene (?) to lowest (?) Pleistocene) 24 Qvf 4 Mourant, W. A., 1963, Water resources and geology of the Rio Hondo drainage basin, 17 10 where the termination of fault is unknown. 11 82 19 11 20 77 Chaves, Lincoln, and Otero Counties, New Mexico: New Mexico Office of the H 03495 33 4 @sr Psa Cenozoic Igneous Rocks , trace of axial plane, dashed where approximately located 22 17 Kd QTg 12 5 State Engineer Technical Report 28, 85 p. 20 Tsv 82 Qvf Kmv 17 61 Tad 11 24 Tsv - Sierra Blanca volcanic rocks, undivided (upper Eocene to Oligocene) Syncline, trace of axial plane, dashed where approximately located Sloan, C. S., and Garber, M. S., 1971, Groundwater hydrology of the Mescalero Apache 16 Qvf 86 Tsv Qvf Tmz Kd Indian Reservation, south-central New Mexico: U.S. Geologic Survey Hydrologic 000 16 25 Tmz 000 3689 31 12 9 23 3689 Dip and dip direction of bedding, dashed where compiled from Moore et 14 30 3 Tsv-tp Investigations HA-349, scale 1:125000. Kmv 20 7 10 6 14 - Trachyphonolite porphyry flows . 13 Qvf 14 82 12 39 88 8 20 295 al (1998a) Qvf Qaf Thompson, T. B., 1966, Geology of the Sierra Blanca, Lincoln and Otero Counties, New Qvf 77 B Qvf Qvf Qaf 10 16 Qvf Qvf Qvf Qvf 21 Qvf . Dip and dip direction of eutaxitic foliation in welded ash-flow tuff, dashed Mexico: PhD Dissertation, University of New Mexico, 146 p. Qvf Qvf Qvf Tcm Tcm @sr 10 17 Tsv-tf - Trachybasalt flows 20 000 Qvf 10 Qvf Qaf Qvf Qvf Qvf Pg where compiled from Moore et al (1998b) Thompson, T. B., 1972, Sierra Blanca Igneous Complex, New Mexico: Geological @sr 6 12 . Qaf 17 Pg 27 20 295 Society of America Bulletin, v. 83, p. 2341-2356. Qvf Kmv Qvf Qvf @sr Dip and dip direction of joints 24 24 Py 10 Qvf 14 Wasiolek, M., 1991, The hydrogeology of the Permian Yeso formation within the upper 33°20'0"N Kmv Qvf Qvf Kd Psa . Tsv Qvf Tmz 3 C'' 40 295 Dip and dip direction of plane of small fault 10 Qvf Qaf 4 Qaf 33°20'0"N Rio Hondo Basin and the Eastern Mescalero Apache Indian Reservation, Lincoln QTgg Qvf Tcm 16 7 12 Pg 13 . Trend and plunge of slickenside striae and Otero Counties, New Mexico, in Barker, J. M., Kues, B. S., Austin, G. S., and 7 15 295 40 3688000 6 Qrt1 3 3688000 Lucas, S. G., eds., Geology of the Sierra Blanca, Sacramento, and Capitan 6 @sr 12 85 Qvf 17 Pg and local trace of dike, with dip and dip direction where Qvf 80.295 Ranges: New Mexico Geological Society Guidebook 42, p. 343-351. 74 18 10 measured 67 5 7 9 5 5 16 4 12 21 5 14 9 Kd @sr Water well with NM State Engineer Office W.A.T.E.R.S. database 19 5 21 Pg Psa 18 11 Qg 17 Py 15 H00123 11 13 14 Qaf Qaf reference number 26 @sr daf H 03062 15 5 18 Py Qaf Py Py Qrt3 28 Py Qrt3 12 7 10 Water well projected into cross section 16 Kd 15 Psa Qrt3 Qrt3 Qrt3 Qrt2 Pg 18 Qrt3 H 00031 Py 5 16 24 8 Qrt3 Qrt3 11 89 Qrt2 12 10 82 Py 10 22 8 Qrt1 3687000 Qvf 85 Psa Qls 3687000 Tad daf af Qvf 85 14 28 Qvf 22 8 14 Qg 29 60 Km 35 65 18 Psa 84 4 H 01397 Qg 84 Py 16 8 11 71 12 11 6 10 Qvf 85 90 10 24 90 12 42 11 12 84 16 7 14 68 QTgg 12 14 18 A' 17 11 Qg Qaf 7 QTgg QTgg Qvf Qaf QTgg 26 Km 14 3686000 3686000 Qvf Psa 5 daf Kmv 19 Kd Py 30 Py

Qvf Psa Qg 14 6 Tad Tad Qvf 4 5 Km Kd Qaf Qaf 13 90 Psa Qvf 4 Qvf 15 Tmz 5 13 Qvf 4 7 af Tad af 15 19 7 Qvf Qg 34 Qg 19 Psa Qvf 20 Pg 10 af 18 Py Qvf 3685000 QHa 22 19 3685000 Km Km 24 QTg 10 46 10 Qvf 83 16 20 Qg 7 Qvf 28 38 88 Kd 39 Psa 9 af 58 4 Km Pg Py 7 Kd Qvf Qvf Qaf 23 24 Pg 14 25 28 daf Qvf 40 33 18 Pg 20 QHa Qvf Qaf Psa Kd Qg 23 10 af 23 Py Qvf Psa 18 90 daf 10 daf 5 12 7 17 36 QHa Pg 26 Py 23 QTg Pg 21 22 19 9 000 daf 16 000 3684 22 73 80 3684 85 Kd Psa 88 8 12 14 15 13 Km 17 20 26 Kd Tad 31 Qaf 33°17'30"N 12 Pg @sr Kd Pg Qvf 22 74 33°17'30"N Kd @sr 20 Qaf 10 12 Kd Qaf Kd 4 14 QTg Km Qaf 35 21 Qaf

000 af 000 3683 Qvf 30 3683 Qvf af C' 15 @sr Qaf af Psa Qaf Qvf 18 18 5 Qaf 10 40

Km 22 19 6 Kd 27 Kd Qvf 6 Kmv 27 Qaf Qvf 31 3682000 Pg 3682000 Qvf 15 37 Tmz 5 24 Psa Psa Qvf 8 14 @sr Psa Km Km Qaf 20 Psa 15 22 Qaf Tmz Kd 5 Km Qvf Psa 15 Psa af 22 18 12 20 Pg 11 14

19 3681000 18 Pg 3681000 Km Kmv Psa 7 27 Qaf 11 2 18 Pg 11 Psa 88 Kd 6 3 Qvf Psa Psa 82 12 Kd 9 Psa Km 12 25 B' 16 Km @sr 29 6 Psa 45 Pg Psa 3680000 5 3680000 Psa Pg Psa 15 C 15 80 10 4 Psa Kmv 4 19 27 25 5 15 40 20 29 Pg 22 Psa 38 20 Psa 15 Kd Kmv Km Psa 22 Psa Kd 35 Psa 35 5 Psa Kd @sr 33°15'0"N Psa Pg Psa 3679000 3637390°0105'0"N

430000 431000 432000 433000 434000 435000 436000 437000 438000 439000 440000 441000 442000 105°45'0"W 105°42'30"W 105°40'0"W 105°37'30"W

Base from U.S.Geological Survey 1963, revised 1982. 1927 North American datum, UTM projection -- zone 13N 1000- meter Universal Transverse Mercator grid, zone 13, shown in red Geologic map of the Ruidoso 1:24,000 quadrangle, Lincoln and Otero Counties, New Mexico. NOGAL FORT ANGUS 1 0.5 0 1 MILE PEAK STANTON

NEW MEXICO 1000 0 1000 2000 3000 4000 5000 6000 7000 FEET

SIERRA RUIDOSO BLANCA RUIDOSO May 2004 PEAK RUIDOSO DOWNS 1 0.5 0 1 KILOMETER

Magnetic Declination by CONTOUR INTERVAL 40 FEET May, 2004 1 APACHE MESCALERO WHITETAIL Geoffrey Rawling SUMMIT 9º 37' East NATIONAL GEODETIC VERTICAL DATUM OF 1929 At Map Center

1 New Mexico Bureau of Geology and Mineral Resources NMBGMR, 801 Leroy Pl., Socorro, NM, 87801 QUADRANGLE LOCATION Open-file Map Series OFGM 93 This draft geologic map is preliminary and will undergo revision. It was produced from either scans of hand-drafted originals or from digitally drafted original and figures using a wide variety of software, and is currently in cartographic production. COMMENTS TO MAP USERS It is being distributed in this draft form as part of the bureau's Open-file map series Mapping of this quadrangle was funded by a matching-funds grant from the STATEMAP program (OFGM), due to high demand for current geologic map data in these areas where of the National Cooperative Geologic Mapping Act, administered by the U. S. Geological Survey, A geologic map displays information on the distribution, nature, orientation, and age relationships STATEMAP quadrangles are located, and it is the bureau's policy to disseminate and by the New Mexico Bureau of Geology and Mineral Resources, (Dr. Peter A. Scholle, of and deposits and the occurrence of structural features. Geologic and fault contacts are Director and State Geologist, Dr. J. Michael Timmons, Geologic Mapping Program Manager). geologic data to the public as soon as possible. irregular surfaces that form boundaries between different types or ages of units. Data depicted on this geologic quadrangle map may be based on any of the following: reconnaissance field After this map has undergone scientific peer review, editing, and final cartographic geologic mapping, compilation of published and unpublished work, and photogeologic interpretation. production adhering to bureau map standards, it will be released in our Geologic Map Locations of contacts are not surveyed, but are plotted by interpretation of the position of a given (GM) series. This final version will receive a new GM number and will supercede contact onto a topographic base map; therefore, the accuracy of contact locations depends on the this preliminary open-file geologic map. New Mexico Bureau of Geology and Mineral Resources scale of mapping and the interpretation of the geologist(s). Any enlargement of this map could cause New Mexico Tech misunderstanding in the detail of mapping and may result in erroneous interpretations. Site-specific 801 Leroy Place conditions should be verified by detailed surface mapping or subsurface exploration. Topographic Socorro, New Mexico and cultural changes associated with recent development may not be shown. 87801-4796 DRAFT Cross sections are constructed based upon the interpretations of the author made from geologic mapping, and available geophysical, and subsurface (drillhole) data. Cross-sections should be used as [505] 835-5490 an aid to understanding the general geologic framework of the map area, and not be the sole source http://geoinfo.nmt.edu of information for use in locating or designing wells, buildings, roads, or other man-made structures.

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