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NMBGMR Open-file Geologic Map 207 Last Modified 2013 NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES A DIVISION OF NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY 107°7'30"W ȱȱ 12 27 Qpy Qpa 18 Kca 15 Kcl 10 Kmh 12 12 10 33°10'0"N Qe ȯ ȱ ȱ ȱ ȱ ȱ ȱ ȱ Ȭ¢ȱ ȱ ȱ ȱ ȱ ¢ȱ ȱȱȱȱȱ¡ǯȱȱȱȱŗŖŖȱǻřŖǼȱǯ ȱ ǰȱ ȱ ȯȱ ȱ ȱ ¢ȱ ȱ ȱ ȱ ȱȱȱȱȱȱȱ¢ȱǯȱȬȱȱȱȱ ęȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ǯȱ ȱ ȱ ȱ ȱȱȱȱȱȱȱȱǰȱȱȱĚ ȱǻTbǼǯȱȱȱŜŖȱǻŗŞǼȱǰȱ ȱ ǯ ȱ ȱ ȯȬȱ Ȭ¢ȱ ȱ ȱ ȱ ȱ ȱ ȬȱȱDzȱ¡ȱ¢ȱȱȱȱȱȱȱȱȱȱ ȱȱȱȱǯȱȱȱȱśȱǻŗǯśǼȱȱ¡ǯ ȱȱȯȬȱǰȱȱȱȬȱ ¢ǰȱ ȱ ¢ȱ ȱ ȱ ȱ ǰȱ ȱ ȱ ȱ ȱ ȱ ǰȱ ȱ ȱ ȱ Ȭȱ ȱ ǯȱ ¡ȱ ȱ ¢ȱȱśŖŖȱǻŗśŘǼǯ ȱ ǰȱ ȱ ȱ ȯȱ ȱ ȱ ȱ ȱ ȱ ¢ǰȱ ǰȱ Ȭȱ ȱ ǰȱ ȱ ȱ ȱ ǰȱ Ȭȱ ǯȱ ȱ ȱ ȱ ȱ ȱ ĵȱ ȱ ȱ ȱ Ȭȱ ¢¢ǯȱ ȱ £ȱ ȱ ȱ ȱ ȱ ǯȱ ȱ ȱȱęȱ ȱȱǯȱȱȱŝŝŖȱǻŘřŚǼȱǯ ȱǰȱȱȱȯȱȱ¢ȱǰȱ ǰȱȬǰȱ ǰȱ¢ȱȱȱǰȱ Ȭȱȱȱǯȱȱȱȱȱ ȱȱȱǰȱȱȱȱȱȱȱŗȱǻŖǯȱřǼȱǯȱȱȱȱȱȱ Ȭȱ ¢ǯȱ ȱ ǰȱ ȱ ǰȱ ȱ ęȱ ȱ ȱ ǯȱȱȱȱśśŞȱǻŗŝŖǼȱǯ ȱ ¢ȱ ǰȱ ȱ ¢ȱ ȯ¢ȱ ǰȱ Ȭǰȱ Ȭǰȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ Ȭ¢ȱ ǯȱ Ȭȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ¢ǰȱ ¢ȱȱȱȱȱȱǯȱȱęȱ ǯȱ¡¢ȱŗǰŘŖŖȱǻřŜśǼȱǯ ȱ ¢ȱ ȯ ȱ ȱ ȱ ȱ Ȭ ǰȱ ęȬȱ ȱ Ȭǰȱ ȱȱȱȬȱȱȱǰȱȱ ȱȬ¢ȱ ȱȱǯȱȱȱŞřŖȱǻŗśřǼȱǯ ȱ ȱ ȱ Ȭȱ ȱ ȱ ȱ ǰȱ ěȯTan, massive ȱȱȱȱȱ¢ȱȱȱ¢ǰȱęȱȱǯȱȱȱ ¡ǯȱȱȱŗŖŖȱǻřŖǼȱǯ £Ȭ£ǰȱěȯȬȱ¢ǯȱ 4 4 Ql 2 4 QTp Qpy QTp 15 Map Symbols 4 3 3669000 3 Geologic contact–solid where exposed or well-known, dashed where approximately known. Kmj QTp 2 Ql O 5 3 Normal fault–solid where exposed, dashed were approximately ǰȱĴȱ ȱǯȱȱ ȱǯȱ Bar-ball on down-thrown side. Kca 13 3 Mzu-Pzu Qpa 6 ȱ ǰȱ ȱ ȯ ȱ ȱ Ȭ ȱ ȱ ȱ ǰȱ ȱ¢ȱȱȱȱȱȱ£ȱǰȱȱǰȱȬ¢ȱ ȱ ȱ ȱ ǰȱ ȱ ǯȱ ȱ ¢ȱ ȱ ȱ ȱ ȱ Ȭȱ ȱ ȱ ǯȱ ȱ ȱ ȱ ȱ ǰȱ ȱ ȱ ȱ ȱ ȱȱȱ¢ȱȱȱȱȱȱǰȱȱȱȱȱȱȱǰȱ ȱ ȱ ȱȱ ǯȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ǰȱ¢ȱȱȱȱǯȱȱȱȱŘŖȱǻŜǼȱǯ 10 5 Qpa 4 5 3668000 Tlr Strike-slip fault–arrows show direction of movement. Dashed were approximately known. 14 Tp Qvy Qvy 26 Kmh 12 3668000 5 Ql 8 10 15 10 8 Tb 10 10 10 Kcl Kgd 20 8 5 17 11 10 26 Tbc 10 Qpa 3671000 Kmh 10 20 20 18 7 Kca 10 Qvy 5 30 15 ěȱ¢ȱȱ 3670000 6 20 Tlr 10 5 8 7 14 3672000 20 20 Qvy 5 13 7 5 8 15 Kca 80 20 4 3669000 Kca 7 15 10 10 12 20 Tp 4 7 30 20 3 10 5 4 5 10 Kmh 15 5 17 10 6 3 8 3 10 5 5 3 Qpa 10 62 3 10 17 8 Kmh 12 ȱȬȱȯSand, gravel, silt and silty clay of alluvial fans, erosion surface ȱ ȱ ȱ Ěȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ǯȱ ȱ Ȭȱ ȱ ȱȱ¢¢ȱ ȱȱȱȱȱȱȱȱǯȱȱȱȱŘśȱǻŞǼȱǯ 7 Qvo 4 4 Kmh 3 Kmh Kmj Kmh 6 ȱ Ȭȱ ȯSand, gravel and silt of shallow drainageways, alluvial ǰȱȱȱȱȱȱȱȱ ȱȱȱȱǻQpoǼȱǯȱȱȱ ȱŗŖȱǻřǼȱǯ 10 8 17 15 Kmj 8 13 Kmh 11 7 7 5 4 ¢Ȭȱȯȱȱ¢ȱȱȱĚȱȱ¢ȱǯȱ¢ȱřȱȱŗŖȱǻŗȱȱřǼȱǯ Ql 7 Kmj 7 7 5 8 Kmh Kmh 3673000 6 Qvy Tpp Qe 5 4 Kmj 3 ȱȯSand and loamy-sand ridges, dunes, and mounds that accumulated in the ȱȱ¢ȱǯȱȱȱȱřśȱǻŗŖǼȱǯ Cretaceous Qpo 20 Tlr 5 B' 3674000 10 Kca 7 10 5 Qpo 7 4 Tpp Qpa 13 5 8 4 10 4 5 5 ěȱȱȱ¢ QTp JDC#3 Í Kmj Qpo 10 4 Tp 3675000 35 Qpa 5 15 30 15 8 4 5 7 10 Kmh Kmh 15 Qvo 4 72 6 8 Kmj 15 Kmh 5 4 Kmh Tbc 15 8 4 8 5 8 2 Tb QTp JDC#1 10 20 Qvo 3 QTp Í 15 12 Kca 20 12 4 ȱ¢ȬęȱȯSand, gravel and sandy gravel deposits of arroyos, fans, terraces, ȱȬȱǰȱ ȱȱȱȱȱȱȱȱŗśŖȱǻŚŜǼȱȱȱȱ ȱĚǯȱȱȱ¢¢ȱȱ ȱȱǻȱȱȬȱǼȱȱȱȱ ȱȱȱǯȱȱȱȱŘśȱǻŞǼȱǯ ¢ 9 10 5 15 30 15 33°12'30"N Kca 22 18 4 Qvy Qvo 3 5 20 2 3676000 Ql 12 12 QTp Kca 23 10 15 5 15 Kmj 10 12 10 Kmj 14 7 25 4 3672000 15 Qpg 15 14 20 5 5 10 10 3 Kca 70 14 4 6 Qpa 10 13 4 Kmj 5 2 5 17 13 Kmh 9 25 25 20 21 5 Kmh 4 17 4 7 5 3671000 Qva 6 8 13 Kmj 10 Qvo 3673000 14 12 10 10 15 1 25 12 15 6 5 7 12 Qvo 22 10 10 15 10 13 13 14 22 20 15 15 C' 3677000 7 Kca 10 18 53 14 8 27 13 12 Kmj 13 25 Kca 13 10 13 17 10 10 8 25 27 39 12 30 27 8 20 30 11 10 25 20 45 12 7 Kca 55 Kcl 45 Kmj 18 8 20 40 Kmj 12 10 12 16 17 18 15 25 20 20 13 7 7 Kca 12 5 15 13 15 Tp 10 50 18 25 7 13 14 13 Qvo Kmj 10 33°10'0"N 20 5 15 12 7 8 Tb 7 7 13 17 5 15 Kmj 14 5 B 15 Tb Qvo 14 3675000 15 7 19 12 11 10 10 A 10 15 QTp Kmj Kmj 13 Qpy Qpo Kmj 3 Ql 3678000 Tbc 25 Ql QTp 40 3670000 Kcl 3676000 Tlr QTp 18 10 25 20 20 Kmj 26 35 12 10 3674000 Tp 9 Qpo Kca 15 9 Qe 20 22 26 Kca 23 Kcl 10 10 33°12'30"N Tlr 10 Kmh 15 Kca 7 10 13 15 20 20 2 Ql 18 QTp 23 14 12 10 Qva ȱ¢ȬęȱȯSand and gravelly-sand deposits of arroyos, alluvial fans, and terraces, whose surfaces are graded to within a few feet (meters) of the modern Rio Grande ĚǯȱȱȱȱŗŖȱǻřǼȱǯ 20 16 13 27 13 12 Kmj 5 Qpo Kca 10 15 12 Kca 7 17 20 8 Tp Qpa 7 12 3679000 17 4 9 10 18 20 23 23 25 20 25 20 13 20 21 Kcl 12 Tp 20 20 Kgd 18 3677000 18 10 Qvo A' Kcl Kmj Kmh 20 20 17 20 20 Qvo Tbc Qe 5 20 Qvo 3678000 10 15 12 Qpo 7 3679000 QTp 7 15 Tb Qvy 10 23 Tbc Quaternary 20 20 Kmh 3680000 27 Qpo Kca Tp Kmj 33°15'0"N Tlr Ql Tp 313000 Tb 19 20 12 17 312000 Tb Kca 20 15 311000 310000 12 22 16 Kmh 309000 13 20 3680000 308000 Tlr Tp 21 307000 Tp 8 12 10 107°0'0"W 107°2'30"W 306000 23 32 17 Kmh Kmj 305000 21 10 10 Tb 8 304000 13 10 10 33°15'0"N 107°5'0"W 303000 3 Qpa Tb Tlr Tlr 3 Syncline—showing direction of pluge. Dashed where ¡¢ȱ ǰȱĴȱ ȱǯ p Anticline—showing direction of pluge. Dashed where ¡¢ȱ ǰȱĴȱ ȱǯ 3 z Kca 3667000 Kca 2 302000 303000 304000 107°7'30"W 3667000 33°7'30"N C 305000 306000 307000 308000 309000 107°5'0"W 310000 311000 312000 33°7'30"N 107°0'0"W 313000 107°2'30"W Strike and dip of bedding. 50 Horizontal bedding Base map from U.S. Geological Survey 1970, from photographs taken 1965, field checked in 1970, edited in 1993. 1927 North American datum, UTM projection -- zone 13N 1000-meter Universal Transverse Mercator grid, zone 13, shown in blue JDC#1 1:24,000 1 BLACK BLUFFS FAIRVIEW WELL CROCKER 0.5 1000 0 1000 1 ELEPHANT BUTTE ENGLE ENGLE SHANNON CANYON NW 0 2000 0.5 Geologic Map of the Engle Quadrangle, Sierra County, New Mexico 1 MILE 3000 4000 5000 6000 0 7000 FEET A May 1993 CONTOUR INTERVAL 20 FEET JDC#1—T.D. 500ft mostly in Palm Park Fm. JDC#3—T.D. 300ft mostly in Palm Park Fm.; lowest 30ft maybe rhyolite ǛŘȯǯǯȱśŖŖDzȱȱŜŖȱǻǼDzȱ ȱŚŚŖȱȱȱȱǯ A' Location of geologic cross section ȱȯȱȱȱȱȱȱDZ Palomas Formation; stage IV–V soil carbonate is well developed; the surface is also locally pediment on bedrock units. 1 KILOMETER NEW MEXICO Well name and location NATIONAL GEODETIC VERTICAL DATUM OF 1929 PALOMAS GAP POLECAT TANK CUTTER by Greg Mack 1 and William R. Seager 1 Magnetic Declination August 2012 9º 2' East At Map Center QUADRANGLE LOCATION 1 Dept. of Geological Sciences, New Mexico State University, P.O. Box 30001, Las Cruces, NM 88003 New Mexico Bureau of Geology and Mineral Resources New Mexico Tech 801 Leroy Place Socorro, New Mexico 87801-4796 This and other STATEMAP quadrangles are available for free download in both PDF and ArcGIS formats at: Correlation Diagram Pliocene Pleistocene Hol. http://geoinfo.nmt.edu [575] 835-5490 New Mexico Bureau of Geology and Mineral Resources Mapping of this quadrangle was funded by a matching-funds grant from the STATEMAP program of the National Cooperative Geologic Mapping Act, administered by the U. S. Geological Survey, and by the New Mexico Bureau of Geology and Mineral Resources, (L. Greer Price, Director and State Geologist, Dr. J. Michael Timmons, Assoc. Director for Mapping Programs). Open-file Geologic Map 207 Qvy Qvo Qva Qe Ql Qpy Qpo Qpa unconformity Qpg Tbc Tb Tp Eocene unconformity Tpp Tlr unconformity Kmj Kmh Kmh 4,000' Kmj Kmj Qpa QTp Qpa QTp Kca Qpa Qpa Ql Tlr Kmh Kmj Kmh 4,000' Kmj Kgd Kgd Kcl Kca Kcl 2,000' Kgd Kgd Mzu-Pzu Mzu-Pzu Kcl Kgd 1,000' 1,000' West B 5,000 feet ASL Kmj Kmh Qpo Qpo Qpa Qe Kca Kcl Kgd 4,000' Kmj Kcl Kmj 3,000' Kca Kcl Kca Mzu-Pzu COMMENTS TO MAP USERS 2,000' Kcl Kgd Kcl 1,000' Mzu-Pzu Southwest C (10x vertical exageration) 1,000' Northeast C' 5,000 feet ASL Bend in section 4,900 Jornada Draw fault 4,800 Engle Lake fault Qpa Kca Kmj QTp Kmj Ql Qpa QTp Qe Qpa Tpp 4,900 4,800 Tlr (?) QTp 5,000 feet ASL QTp QTp Qpa Qpa Cedar Lake fault Antelope fault Qpa 4,700 Tlr (?) Kca Tlr Kmj 4,600 Kmh 4,500 A geologic map displays information on the distribution, nature, orientation, and age relationships of rock and deposits and the occurrence of structural features. Geologic and fault contacts are 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 geologic mapping, compilation of published and unpublished work, and photogeologic interpretation. Locations of contacts are not surveyed, but are plotted by interpretation of the position of a given contact onto a topographic base map; therefore, the accuracy of contact locations depends on the scale of mapping and the interpretation of the geologist(s). Any enlargement of this map could cause misunderstanding in the detail of mapping and may result in erroneous interpretations. Site-specific conditions should be verified by detailed surface mapping or subsurface exploration. Topographic and cultural changes associated with recent development may not be shown. 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 an aid to understanding the general geologic framework of the map area, and not be the sole source of information for use in locating or designing wells, buildings, roads, or other man-made structures. 4,700 Kmh Kca 4,600 5,000 feet ASL Kmh Mzu-Pzu Kmj Mzu-Pzu Tlr Kgd 2,000' QTp Tpp QTp Kca 3,000' Kcl Qpa Kmh Kca Kcl Qpo Kca East B' Antelope fault Tlr Kmj Kca Kca Engle Lake fault Kmh Kmj Kmh Kmj 4,000' Water well anticline Kmh Qvo Kmh Central horst Main - central fault Bend in section unconformity Kgd 3,000' Kcl 2,000' 5,000 feet ASL Kmj Kcl Kca Kcl Kca QTp Qpa Qe Kgd Kgd Kca Kmj Kcl Kcl Mzu-Pzu Kca Qpo Kca Mesozoic-Paleozoic Qvo East A' Cedar Lake Bend in section Tb Tb Tp 5,000 feet ASL Kmh Cedar Lake fault Late Cretaceous Main - central fault West A 3,000' Central horst Water well anticline 4,500 The map has not been reviewed according to New Mexico Bureau of Geology and Mineral Resources standards. The contents of the report and map should not be considered final and complete until reviewed and published by the New Mexico Bureau of Geology and Mineral Resources. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the State of New Mexico, or the U.S. Government.
