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NMBGMR Open-file Geologic Map 213 Last Modified 2016 NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES A DIVISION OF NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY o Qv QT cf Q vo J QT cf J t7 Tb o Tbc o Q Tc c e at Qv vo o J o Q J Qc g o y s Qv vo Qv Qv Q Qv QT cc Qv J ill ȱ ¢ȱ ǰȱ Ȭȱ ȯȬȱ ¢ǰȱ ǰȱ ȱ Dzȱ¢ȱȱȱǯȱȱȱȱȱĚȱȱ¢ȱȱȃ¢ȱȄȱ ȱĚǯȱȱȱ ȱȱȱȱǯȱȱȱŘǰŖŖŖȱǻŜŗŖǼȱǯ £ȱǰȱěȯȱȱ¢ǯ | ȱ ȯǰȱ Ȭȱ ȱ ȱ ǯȱ ¢ȱ śŖȱ ǻŗśǼȱ ¡ȱ ȱ ȱ ȱȱȱȱǯ Pa ¢ȱ ȱ ȯȬ¢ȱ ȱ ȱ ǰȱ ȱ ǰȱ ȱ mudstone containing mostly boulder-to cobble-sized clasts of TuȱȱȱȱȬĚ ȱěDzȱȱ ¢ȱȱȱȱȱȱȱǰȱȱȱȱȱ ȱ ¢ȱ ȱ ȱ ěȱ ȱ ¢ȱ ȱ ¢ȱ ǯȱ ȱ ȱ ȃ¢ȱȄȱȱȱȱȱȱȱǰȱȱ ȱȱ¢ȱęȱȱ ȱȱȱȱȱ ȱȱȱȱȱȱǯȱȱȱŗǰŚŖŖȱǻŚŘŝǼȱǯ ¢ ȱȯȱȱ ȱȱȱȱȱ ȱȱǰȱ¢ȱȱ ȱǰȱȬȱȱȬȱǰȱȱȱȱȱĵǰȱ ȱȱȱ ȱ ȱ ¢ȱ ǯȱ ȱ ȱ ȱ Ȭȱ ȱ Ȭǰȱ ǰȱ burrowed, gray cherty limestone and interbedded shale conformably overlain by Bar B ǯȱ ȱ ȱ ȱ ȱ ǰȱ ǰȱ ȱ ȱ ȱ ȱ ȱȱȱȱȱȱȱȱǯȱ¡ȱ¢ȱȱȱ ȱȱȱ ȱȱǻȱ ȱǼǯȱ¡¢ȱşŗŖȱǻŘŝŝǼȱǯ * ȱ¢ȱȯȱȱȱřǰȱǻŗǼȱȱȱȬȱȱȱ ȱ ǰȱ ȱ ¢ȱ ěȬǰȱ ¢ȱ ȱ ȱ ŘŖȱ ǻŜǼȱ ǯȱ ¢ȱȱ¢ȱȱ ȱǯȱȱȱ¡¢ȱŘřȱǻŝǼǯ M ȱȱǰȱěȯȱȱ¢ǯ ȱȱǰȱȬĚ ȱěȱŝȯȬǰȱ¢ȱȱȬĚ ȱěDzȱ¢ȱȱ ȱȱȱDzȱȱȱřȬŗŖȱǻŗȬřǼȱǯ ȱ ȯȬ¢ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱřŘȱȱǻŗŖȱǼȱȱ ȱȱǯȱ¡ȱȱȱŘřŜȱǻŝŘǼȱȱ ȱ¢ȱȱȱȬȱǯ Dp ȱ ȱ ǰȱ ȱ ȯReddish-brown to tan conglomerate, ȱ ǰȱ ȱ ȱ ȱ ȱ ȱ ěȱ ȱ ȱ ȬȱDzȱȱȱȱȱěȱȱȱȱǰȱȱ ȱȱȱ ȱDzȱȬĚ ȱŜȱȱȱȱȱȱȱǯȱȱȱǰȱȱ Ěǰȱ ȱ ȱ ȱ Ȭȱ ȱ ȱ ǯȱ¡¢ȱ ŚŘśȱ ǻŗřŖǼȱǯ ȱ ȯȱ ȱ ¢ǰȱ Ȭȱ ǯȱ ¢ȱ ęȱ ȱ £ȱ ȱĚȱȱȱȱ¢ȱ¡ȱȱ ȱȱȱȱǯȱȱȱśŖȱ ǻŗśǼȱǯ Sf ȱȱǰȱȬĚ ȱěȱŜȯ¢Ȭǰȱ¢ȱȬĚ ȱěDzȱ¢ȱ Dzȱ interbedded with ǯȱ¡¢ȱřśȱǻŗŖǼȱǯ ȱǰȱěȯȱȱ¢ǯ = A 5 7 Qvy 3618000 3,000 Elev. (ft) Qvof Qvy J Trv 1250 ? ? Trv Qvof Qvof Trv Qcg Qvy Qvo Qvy Qvo Qvy Qvy Qv y B Foothills fault Black Hills Fault Salem Bench 5,000 Qvy Qvy QTcf Qvof Qvof Rio Grande Qvyf Qvy QTc QTc QTcu QTc Qvo Qvo QTc Qvy 1,000 Tlr ? Tt 2,000 Q vo f Qvof Qvof 3616000 Qv Qvof Trv ou Qvou 5 o Qv Qvy Elev. (m) South 298000 QTcu J 4,000 QTcu 41 Tu 299000 Trvc 32°37'30"N ¢ȱȱǻ ȱŖǚȱȱřŖǚǼȱǰȱȱȱ¢ȱȱ from aerial photographs—Showing approximate strike and direction of dip g ȱȱǻȱȱ ȱȱȱęǼȱȯ strike and dip £ȱ Erosional remnant of La Mesa surface, the constructional top of the Camp ȱĚȱȱǻQTcfǼǯ J A A' Location of geologic cross section Comments to Map Users May 1995 by William R. Seager John W. Hawley G. H. Mack 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. Department of Geological Sciences, P.O. Box 30001, New Mexico State University, Las Cruces, NM, 88003 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. Hatch test well (projected) Qvy Basin Rio Grande Qvou Qvy Qvyf Qvo Qvy Qvy Qvo Qvy Qvy Qcg Qvy Qvo Black Hills fault Black Hills Qvyf * Tpp Trvc Tbt5 Tbc Tu ? Trvc Trvc ? T.D. 2000' 1,000 Sf | ? Trv | M Dp Tlr ? Tpp Tlr ? 500 | ? Thr Sea Level Sea Level Tu Tbt Tt Tpp -1,000 Qvy Qvo Qvo Qvy Tu QTc 1,000 Correlation of Map Units Palm Park Tbt7 Tbc Tbt6 Qvo Tbt5 Qvo Qvo Thr Tpp Red House D' Mtn. Palm North fault 1,500 Black Hills bench Bend in section ? Pliocene Pleistocene Hol. ȱȯ ȱȱȱ 79 Qvy Rincon Trvc Tu 2,000 Miocene p ȱȯ ȱȱȱǯȱȱ ȱǰȱ ȱ ȱ¡¢ȱ ǰȱĴȱ ȱ New Mexico Bureau of Geology and Mineral Resources Open-file Geologic Map 213 Geologic Map of the Hatch 7.5-Minute Quadrangle, Doña Ana County, New Mexico ȯ¡ȱȱȱȱȱȱȱĚȱȱ (QTcd) ¢ȱȯ ȱȱȱǯȱȱ ȱǰȱ ȱ¡¢ȱ ǰȱĴȱ ȱ 16 Tu 107°7'30"W z 10 Qvo Tbt = Qva Qvo Qvou Qvof Unconformity -500 -2,000 Elev. (ft) Elev. (m) Geologic Cross Section E-E’ Qcg QTcc QTcu QTcf E F-F' South Hatch Uplift Rodney fault Bend in section Rincon Bend in section Black Hills fault Basin Black Hills Black Hills Red House Mountain bench Palm Park QTcu Angular unconformity Trv Trvc QTcc QTcc Trvc 4,000 Local unconformity Thr Trvc Tu Hatch test well (projected) Trvc Tu Qvy Qvy Rio Grande Tpp Tu Trv 1,000 ? Tpp 2000' T.D. Tbt6 500 Tlr ? 1,000 | Thr Tu ? Tbt Sea Level ? Tt ? ? -1,000 Sf Tt Tlr Angular unconformity | ? Dp Tlr Tbt5 Sf M Tpp Pa ? Sea Level * Tbc 1,500 Dp Qva * Qvo Tt Tbt7 Tpp Tbt5 Minor (?) unconformity Qvo Qvo Qva Tbt6 Qvo Tbt7 Trvc Tt 2,000 Qvo Qvy Qvyf Trvc 3,000 Tbt7 Tbc Tbt6 Tbc Qvy QTcf Tbt Tbt Tu Qvy Qvy E' North Palm fault 5,000 Thr Oligocene CONTOUR INTERVAL 20 FEET Qvo 3,000 Eocene 1 KILOMETER ( Thr 300000 Normal fault—solid where exposed, dashed were approximately known, Ĵȱ ȱǰȱȱ ȱǯȱȬȱȱ downthrown side 24 Trvc Trvc Tbt Miss. Penn. Perm. Paleoc. 7000 FEET QTcc Rodey fault Tbt ? = ? -500 Elev. (m) Pa * -2,000 Elev. (ft) Unconformity Dp D-D' West E-E' 5,000 QTcf QTcc Unconformity Sf Geologic Cross Section F-F’ F M Unconformity Dev. 0 6000 Qvo Qvy Trvc Sil. 5000 J J J 4000 Hatch Uplift Qvy 3612000 Bend in section F-F' 5,000 3000 Geologic Cross Section D-D’ D 13 5 1,200 ? o QTcu Qv r(? ) Ca n yon Th o Qv Wa t er 69 1,250 Trv 34 Trvc 3,900 Elev. (ft) 15 25 ? ? Tpp 3613000 15 Qvy Qvyf 4,000 o Qv J 10 F’ u http://geoinfo.nmt.edu 12 ? Trv QTc 0.5 2000 [575] 835-5490 This and other STATEMAP quadrangles are available for free download in both PDF and ArcGIS formats at: Trv New Mexico Bureau of Geology and Mineral Resources New Mexico Tech 801 Leroy Place Socorro, New Mexico 87801-4796 10 At least as low as 4,160' Qvou Qvof Qvo ? ? ? ? Qvo Rio Grande Qvy 4,100 7 o 1000 1 MILE Magnetic Declination January 1995 10º 49' East At Map Center Quadrangle Location E 12 12 45 13 Qv NEW MEXICO SIERRA ALTA 15 SOUSE SPRINGS 45 0 0 NATIONAL GEODETIC VERTICAL DATUM OF 1929 HOCKETT 12 25 0.5 1000 ALIVIO RINCON 10 15 HATCH HATCH Geologic contact—solid where exposed or well-known, dashed where approximately known 1:24,000 1 ARROYO CUERVO 15 QTcf with QTcc tongues Bend in section Qvy Explanation of Map Symbols 1 MCLEOD TANK D Trvc 107°10'0"W 107°12'30"W 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 GARFIELD 297000 QTcc 296000 25 15 5 35 Qvo 4,200 Qvo 70 22 1,300 QTcf 107°15'0"W 295000 Qcg 294000 293000 30 4,300 292000 QTcu 5 20 1,350 QTcc QTcc 291000 14 290000 10 QTcc J 289000 J 10 QTcf Qvo QTcc Qvo QTcf 10 3612000 T HA CH 5 Qvo 60 35 30 70 40 23 QTcu 45 Qvo 5 5 20 Trvc Qvo F Qvy Trvc 30 15 3614000 QTcf QTcf QTcf Qvo 7 5 12 60 Qvo 67 Qvo 18 12 25 66 Q v 7 Trvc 22 22 o 22 T o 17 80 Qvo Qv IF 12 L P 13 Tu U 5 57 30 12 Qvo QTcu 10 12 20 8 6 20 Qvo 15 11 10 12 19 QTcu 15 20 13 QTcu 18 26 Tu 1522 Qvo QTcf 5 10 17 Qcg 8 Trvc 15 18 Qvo 31 Tu 5 5 Qvo QTcf 10 QTcc 17 Qvo o Qv 12 QTcc Qvo Trvc 5 Trvc QTcf 3 Qvo Trvc Tu Qvo Qvo 15 7 Qvy Trv Qva Qva Tu QTcc QTcf 15 5 Trvc 5 Qvo 5 15 Qvo QTcu QTcf Bend in section 60 Qvo 7 3 Thr(?) Trvc 3613000 32°37'30"N Qvo 20 12 Trv Tu Qcg Qcg Bend in section 4,400 Trv QTcc Trvc 5 Trv QTcf 7 Qvo Fa QTcc Qvo 15 t ul Qvy Trv 2 Trv Qvo Trv Trvc Bend in section 4,500 Qvo Trvc 65 y de Ro 75 Trv 4 3 Tu 10 Trv Qvo Trv Qvy 8 Thr(?) 7 Qvo Qvo Tu Qvo Trv 3614000 lt Fau 1,400 Tbt5 Trv Qvo Trv 72 15 5 QTcu 4,600 QTcf 12 Qvo Qvo Trv 10 Qvo Qvo 5 Trvc QTcf Bend in section Southwest Qvo Qvo QTcf Qvo 8 Qvou 3615000 Northwest Trvc Qvo Trv 3615000 Trv C' (C-C’ Vertical exaggeration = 10x) C Qvo Qvo Qvy QTcf Geologic Cross Section C-C’ 5 Trv Qvyf Qvou Sea Level Elev. (m) ? Qvou = ? Qvof Qvof Qvy Hatch test well (approximately located) ? Sea Level Elev. (ft) ?) QTcf 3616000 Tbc lt ( Qvof QTcf Qvy fau Trv 1,000 32°40'0"N Qvy ills Qvof ? Fo oth Trv 500 Pz Tu Qvof C Tbc Tbt5 Tpp Thr ? 3,000 Qvof B 1,500 Qvo ? QTcf 3617000 32°40'0"N Northwest Tbt6 Qvo Tbt5 Trvc Trv B' Palm Park Tu ? ? Trv Trv 3617000 Qvo Qvy 4,000 Qvof 1000 Elev. (m) Bend in section Southwest Trv Trvc Trvc Geologic Cross Section B-B’ Qvof Trv Trv 1500 QTcu Qvy QTcf 10 7 Qvyf 4,000 Qv of Trv Rio Grande QTcf Trv Trv Northwest Foothills fault 5,000 3 Qvof A' Southwest 5 Qvof Geologic Cross Section A-A’ 3619000 7 Qvo 10 Tr v H Tc c Q LS QT cc IL Qv y H QT cc o Qv K vo R Trv Qvy Qvy ȱ ȱ ȯRed and grayish-red conglomerate and conglomeratic sandstone ȱȱȬȱȱȬ£ȱȱȱ£ȱȱȱȱ Dzȱ¢ȱŘŖȱǻŜǼȱȱȱȱ¡ȱȱȱ ȱȱȱǯ Tlr 5 Trv A 5 Qvou Qvy Trv 3618000 k Qvyf Tbt6 10 4 Qvou y 10 8 Qvou Qvou Qvy Qv 5 Qvo Qvou Tbc 24 fa ul t 9 Qvo Qvou Tbt7 ȱȱǰȱȱȱȱěȯřŖŖȱǻşŗǼȱȱȱǯ QTcu Tt ȱ ¢ȱ ǰȱ ȱ ȯReddish-brown to tan conglomerate, conglomeritic sandstone, and mudstone; boulder- to cobble-sized clasts are predominantly £ȱ ǰȱ ǰȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ¢ȱ ȱȱȱȱȱȱȱȱǯȱȱȱȃ¢ȱȄȱȱȱȱ ȱȱȱȱȱȱ ȱȱȱȱȱȱȱȱȱȱǯȱ ȱȱ ȱ¢ȱȱȬĚȱǰȱTrvǯȱȱȱŘǰŖŖŖȱǻŜŗŖǼȱǯ o Qvo Qvou t ul fa A K AC Trv 32°42'30"N Tbt 3620000 Trvc 3 3619000 Qvof Qvo BENCH 3 P Q BL Qvof 12 QTcf 8 8 3 Trvc Qv c Bla Qvo Qvo Trv 8 Qvo 3 Qvo 10 10 Trv 3 Qvo 7 Qvo Qvo Qvo QTcf 4 3621000 Trv 8 Trv Qvo 23 Tt 8 QTcc Tt ȱȱȯǰȱ¢ǰȱǰȱȱȱǰȱǰȱȱȱDzȱ ȱƝȱȱȱȱȱ¡ȱȱȱȱȱȱ ȱȱȱǯȱȱȱŗǰśŖŖȱ ǻŚśŝǼȱǯ Tpp ȱȱȯ¢ȱȱȱȱȱȱĚ ȱȱȱȱ ȱ ȱ ȱ ȱ ǯȱ ¢ȱ ȱ ¢ȱ ȱ ȱ ȱ ȱ ȱ ȱȱ ȱȱȱ¢ȱȱ¢ȱ ¢ȱȱȱȱȱ ȱ ǯȱ¡¢ȱŚŖŖȱǻŗŘŘǼȱǯ Tu ȱ ȱ ǰȱ Ȭȱ ȯWell- to moderately-cemented, tan to reddish-brown, boulder to cobble-pebble conglomerate and conglomeritic sandstone; derived ȱȱ ȱȱȱȱȱȱDzȱȱ ȱ downslope and is gradational upward into ȱDzȱȱ ȱ¢ȱǯȱȱȱŗśŖȱ ǻŚŞǼȱǯ 23 Qcg Qvo Qvo Trv QTcf Qvo Qvo ȱȱǰȱĚȱȱȱȯȬ¢ǰȱ¢ ǰȱȱȱȱȱǰȱ ǰȱ ǰȱ ǰȱ ȱ ȱ ȱ ȱ ȱ Ěȱ ȱȱȱȱȱȱȱȱǰȱȱ ȱȱȱȱĚȱȱ ȱǯȱȱȱȬȱȱȱȱ¢ȱ ȱȱ ǯȱȱȱȱřŖŖȱǻşŗǼȱǯ QTcf Tu Tt Trv ȱȱǰȱěȯȱȱ¢ǯ QTc 3622000 Tu 23 Qvo QTcc QTcf Qvof LS Trv 10 ȱȱǰȱȬĚ ȱěȱśȯȬ¢ǰȱ¢Ȭ ǰȱ¢ȬȱȬĚ ȱěȱ ȱ ȱ ȱ ȱ ȱ ȱ ¢ȱ ĵǯȱ ¡¢ȱ śśȱ ǻŗŝǼȱǯ Tbt5 ȱ ȯȱ ȱ Ȭȱ ȱ Ȭ¢ǰȱ Ȭǰȱ ěȱ ȱ and interbedded, pale-red to pale-tan mudstone; interpreted to be distal parts of alluvial aprons ȱȱ¢ȱȱDzȱȱȱ ȱ ȱȱȱǯȱ ȱȱȱŗǰřŖŖȱǻřşŜǼȱǯ Tt Tbc Tt 18 Thr ȱ ȱ ǰȱ ȱ Ȭȱ ȯBoulder to pebble conglomerate and ȱ ȱȱȱȱȱȱȱȱřȱǻŗǼȱȱȱȱǯȱȱȱǃȱŜśȱǻŘŖǼȱ ȱȱȱȱȱǰȱȱ ǯ Tbt6 Tu vy QTcf Qvo 3620000 IL 4 Trv Tbt6 Qcg Tbc Tt QTcf QTcc Qvo Qvof LM H Qvo 6 Tbt7 Trv ěȱȱȱ¢ Qva Tt Qvo QTcc Qvy Q Trv QTcc Tpp PA Q vo Trv 5 3623000 Qva Tbt7 Qvo QTcf QTcc Qvo QTcf Tt Trvc ȱȱȱ Qvou Tbt5 11 7 Tt 2 Qvo Qvof QTcf QTcc Trv Tbc Tbc QTcc Qvo Qvo Qvo Qvo Qvof Qcg vo Tbc 24 Trv QTcc Trv Qvo Qvof 5 Trv Qvo Qvy QTcc Tt 2 32°42'30"N Q Lower Santa Fe Group, Rincon Valley Formation, Hayner Ranch Formation, Thurman Formation (description of individual units listed below) Tpp Qvo Qvo 3621000 Trv cf QT Tbt6 Tu Qvo QTcc Tbt5 Tbt5 Tbt6 25 QTcf Tpp 9 Tt ǰȱ ¢Ȭęȱ ȯArroyo, fan, and terrace deposits (from boulder gravel to silt-clay), associated with surfaces graded to or within a few feet of the modern Rio Grande ĚǯȱȱȱȱŚŖȱǻŗŘǼȱǯ ȱ¢ȬęǰȱĚȱȯȱȱȱĚȱȱǻȱȱȱȱ ȱȱȬ¢ǼǰȱȱȱȱŗŞŖȱǻśśǼȱȱȱȱȱĚDzȱȱęȱ with QvoȱDzȱȱȱȱśŖȱǻŗśǼȱǯ Qvof Tpp Tbt7 QTcf 25 Qvo Qvo Qvou Trv Tpp Tu Qvo Qcg Trv 3624000 Qvy Tu Qvyf QTcc QTcf QTcf Qvo Tu Tt QTcc Trv Qvo Q Qvof Qvof f vo Qvo QTcf v Tr QTcc Tu ¢ ȱ ¢Ȭęȱ ȯArroyo, fan, terrace deposits, and erosion-surface veneers (from boulder gravel to silt-clay), associated with graded surfaces formed during at least three major ȱ ȱ ¢ȱ ȱ ȱ ȱ Ȭęǯȱ ȱ ȱ ȱ ȱ ȱȱȱȱǰȱ¢ȱȱȱǻǼȱǯȱȱȱȱŜŜȱǻŘŖǼȱǯ Qvo Tbc Tbc 10 15 Tbt7 es QTcf o Qv QTcc Qvo Qvo 57 QTcf Qvo ci Qcg f Tc Q Qvo fa QTcf v Tr Trv l Tbc Tbc Tbt6 Qvo Tbt5 Qvo 5 3622000 Tbt5 Quaternary ȱ¢ȬęǰȱĚȱȯȱȱĚȱȱȱȱǻ¢ȱǰȱ ǰȱȱ¢ǼDzȱȱȱȱŝŖȱǻŘŗǼȱǯ Qvyf Tpp Tbt5 Tpp Qvo Qvy QTcc 4 via Qvo Qvo Tpp 14 Tu Qvo QTcf 6 Qvo Qvo flu Tlr Tpp fault QTcf K C' o Trvc Rice C Hil ls p Qvy o o QTcc QTcf QTcu Qv Qvof ck Bla Qv Qvo Trvc o Qvo m Qvo QTcf vo Trv Qvo QTcf 5 Qv A Qvy 3625000 Tpp Qvo 15 QTcf QTcf Trv Trvc Tpp Dp M 42 Pa Qvo 15 QTcf Qvo Qvo t5 Q Qvo Tb Qvo Qvo QTcc Qcg QTcf QTcf Trvc Qvo Trvc Trv f Tc Q Trv Qvo Trv Qv 10 Trvc Q cg 5 6 Qvof Qvof o Qcg 20 15 32°45'0"N Sf * 12 Tpp L Tpp Trvc p A p5 Trvc 5 Trvc QTcf im x ro Qv Tu Trvc 17 Qvy cf QT B Qva Pal m E' * 7 Tpp Qvo Qvo Ca Qvo QTcu Q vo 6 17 Sf 35 41 Tpp ȱȱȱ 107°7'30"W D' Pa Qvo QTcu 17 of sl p Tbt6 30 it 10 16 15 15 QTcf 13 5 Trv Trvc u e op m Qvo S Qvo 10 M li 17 Qvof 3623000 Qvo E AL Tu 28 QTcu 20 Qvof 300000 20 CH N BE 30 27 Qvof QTcc Trvc Trv Qvo 12 QTcf Tr vc QTcu Qcg QTcf Qvof Qcg QTcc Qvy Thr 24 v Tr Qvo 14 Qvo QTcf QTcc 12 Q vo QTcc 12 15 15 QTcc 12 16 16 Qvo 11 Qvo y Qvo 75 vo Trvc Qvo Qvo Qvo 15 3624000 QTcf 15 QTcu Trvc 15 Qvo Qv Q B' 75 Thr 10 f QTcf QTcf 10 QTc Qvo 10 15 Qcg Qvo QTcc 16 QTcf Qvo Qvof 12 10 Qvo 17 10 Tc c Qvo Qvo QTcf Q Thr Thr Qvo 3625000 Qvo QTcf 6 QTcf Thr 15 299000 298000 297000 Thr Qvo QTcf QTcc Qvo Qvo Qvo 5 QTcf QTcf 15 Qvo 12 Trvc QTcc 5 107°10'0"W A' 296000 Qvo QTcc QTcf Qvy 295000 Trvc 294000 Qvo Qvo QTcf 293000 f QTc Qvy QTcc 292000 291000 32°45'0"N 107°12'30"W 290000 QTcf QTcc 107°15'0"W 4,000 Trvc QTcu Qvy Qvy Hatch Uplift Tu Tbt Qvo Qvo QTc Trv 1,500 Trv Trvc ? Tu Tbt Tpp East Rodey graben Tu Tbt 3,000 Rodney fault Trvc Qvy Trvc Trvc Trvc F' Trvc ? Tu ? 1,000 Tu Tpp Tbt 2,000 Tpp 500 1,000 Elev. (ft) Elev. (m)
