Jornada Draw Watershed (HUC8 13030103)
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Appendix E High-Potential Historic Sites
APPENDIX E HIGH-POTENTIAL HISTORIC SITES National Trails System Act, SEC. 12. [16USC1251] As used in this Act: (1) The term “high-potential historic sites” means those historic sites related to the route, or sites in close proximity thereto, which provide opportunity to interpret the historic significance of the trail during the period of its major use. Criteria for consideration as high-potential sites include historic sig nificance, presence of visible historic remnants, scenic quality, and relative freedom from intrusion.. Mission Ysleta, Mission Trail Indian and Spanish architecture including El Paso, Texas carved ceiling beams called “vigas” and bell NATIONAL REGISTER tower. Era: 17th, 18th, and 19th Century Mission Ysleta was first erected in 1692. San Elizario, Mission Trail Through a series of flooding and fire, the mis El Paso, Texas sion has been rebuilt three times. Named for the NATIONAL REGISTER patron saint of the Tiguas, the mission was first Era: 17th, 18th, and 19th Century known as San Antonio de la Ysleta. The beauti ful silver bell tower was added in the 1880s. San Elizario was built first as a military pre sidio to protect the citizens of the river settle The missions of El Paso have a tremendous ments from Apache attacks in 1789. The struc history spanning three centuries. They are con ture as it stands today has interior pillars, sidered the longest, continuously occupied reli detailed in gilt, and an extraordinary painted tin gious structures within the United States and as ceiling. far as we know, the churches have never missed one day of services. -
A Proposed Low Distortion Projection for the City of Las Cruces and Dona Ana County Scott Farnham, PE, PS City Surveyor, City of Las Cruces NM October 2020
A Proposed Low Distortion Projection for the City of Las Cruces and Dona Ana County Scott Farnham, PE, PS City Surveyor, City of Las Cruces NM October 2020 Introduction As part of the ongoing modernization of the U.S. National Spatial Reference System (NSRS), the National Geodetic Survey (NGS) will replace our horizontal and vertical datums (NAD83 and NAVD88) with new geometric datums assigned in the North American Terrestrial Reference Frame of 2022 (NATRF2022). The City of Las Cruces / Dona Ana County and the City of Albuquerque / Bernalillo County submitted proposals to NGS to incorporate Low Distortion Projections (LDP) as part of the New Mexico State Plane Coordinate Systems. Approval by NGS was obtained on June 17, 2019 for the proposed systems (see approval notice). Design of the LDP is the responsibility of the submitting agencies and must be submitted to NGS on or prior to March 31, 2021. Mark Marrujo1 with NMDOT is submitting final LDP design forms to NGS for the State of New Mexico. The City of Las Cruces (City) is designing a new Low Distortion Projection for Public Works Department, Engineering and Architecture projects to NGS criteria. To meet NGS LDP minimum size and shape criterion, the LDP area extends to Dona Ana County (County) boundary lines. This report presents design analysis and conclusions of the proposed City / County local NGS LDP system for stakeholders’ review prior to NGS final design submittal. NGS NM SPCS2022 Zones and Stakeholder Organizations NGS is designing new State Plane Coordinate Systems (SPCS2022) for New Mexico. The default SPCS2022 designs for the State are a statewide single zone and the three State Plane Zones: West, Central, and East. -
The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/63 The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G. Lucas, Karl Krainer, Dan S. Chaney, William A. DiMichele, Sebastian Voigt, David S. Berman, and Amy C. Henrici, 2012, pp. 345-376 in: Geology of the Warm Springs Region, Lucas, Spencer G.; McLemore, Virginia T.; Lueth, Virgil W.; Spielmann, Justin A.; Krainer, Karl, New Mexico Geological Society 63rd Annual Fall Field Conference Guidebook, 580 p. This is one of many related papers that were included in the 2012 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. -
Cultural Resources Overview Desert Peaks Complex of the Organ Mountains – Desert Peaks National Monument Doña Ana County, New Mexico
Cultural Resources Overview Desert Peaks Complex of the Organ Mountains – Desert Peaks National Monument Doña Ana County, New Mexico Myles R. Miller, Lawrence L. Loendorf, Tim Graves, Mark Sechrist, Mark Willis, and Margaret Berrier Report submitted to the Wilderness Society Sacred Sites Research, Inc. July 18, 2017 Public Version This version of the Cultural Resources overview is intended for public distribution. Sensitive information on site locations, including maps and geographic coordinates, has been removed in accordance with State and Federal antiquities regulations. Executive Summary Since the passage of the National Historic Preservation Act (NHPA) in 1966, at least 50 cultural resource surveys or reviews have been conducted within the boundaries of the Desert Peaks Complex. These surveys were conducted under Sections 106 and 110 of the NHPA. More recently, local avocational archaeologists and supporters of the Organ Monument-Desert Peaks National Monument have recorded several significant rock art sites along Broad and Valles canyons. A review of site records on file at the New Mexico Historic Preservation Division and consultations with regional archaeologists compiled information on over 160 prehistoric and historic archaeological sites in the Desert Peaks Complex. Hundreds of additional sites have yet to be discovered and recorded throughout the complex. The known sites represent over 13,000 years of prehistory and history, from the first New World hunters who gazed at the nighttime stars to modern astronomers who studied the same stars while peering through telescopes on Magdalena Peak. Prehistoric sites in the complex include ancient hunting and gathering sites, earth oven pits where agave and yucca were baked for food and fermented mescal, pithouse and pueblo villages occupied by early farmers of the Southwest, quarry sites where materials for stone tools were obtained, and caves and shrines used for rituals and ceremonies. -
Plan for the Recovery of Desert Bighorn Sheep in New Mexico 2003-2013
PLAN FOR THE RECOVERY OF DESERT BIGHORN SHEEP IN NEW MEXICO 2003-2013 New Mexico Department of Game and Fish August 2003 Executive Summary Desert bighorn sheep (Ovis canadensis mexicana) were once prolific in New Mexico, occupying most arid mountain ranges in the southern part of the state. Over-hunting, and disease transmission from livestock are 2 primary reasons for the dramatic decline in bighorn sheep numbers throughout the west during the early 1900s. In 1980, desert bighorn were placed on New Mexico’s endangered species list. From 1992-2003, approximately 25% of bighorn were radiocollared to learn causes of mortality driving this species towards extinction. Approximately 85% of all known-cause non-hunter killed radiocollared individuals have been killed by mountain lions. Despite the lack of a native ungulate prey base in desert bighorn range, mountain lion populations remain high, leading to the hypothesis that mountain lions are subsidized predators feeding on exotic ungulates, including cattle. Lack of fine fuels from cattle grazing have resulted in a lack of fire on the landscape. This has lead to increased woody vegetation which inhibits bighorn’s ability to detect and escape from predators. Bighorn numbers in spring 2003 in New Mexico totaled 213 in the wild, and 91 at the Red Rock captive breeding facility. This is in spite of releasing 266 bighorn from Red Rock and 30 bighorn from Arizona between 1979 and 2002. Several existing herds of desert bighorn likely need an augmentation to prevent them from going extinct. The presence of domestic sheep and Barbary sheep, which pose risks to bighorn from fatal disease transmission and aggression, respectively, preclude reintroduction onto many unoccupied mountain ranges. -
Silver and Gold Occurrences in New Mexico by Robert M
New Mexico Bureau of Mines & Mineral Resources Resource Map 15 March 1986 Silver and gold occurrences in New Mexico by Robert M. North and Virginia T. Mclemore New Mexico Bureau of Mines and Mineral Resources, Socorro, New Mexico 87801 Abstract Anomalous amounts of silver and/or gold have been identified in 153 mining districts or prospect areas of New Mexico. Production from most of these occurrences has been small; figures or estimates are given when known. Thirty-five districts have produced in excess of 10,000 troy ounces of gold or 200,000 ounces of silver. Silver and gold in New Mexico occur in 14 distinct types of deposits ranging in age from Precam brian (Proterozoic) to Recent. Mid-Tertiary to Recent deposits include the placer, volcanic-epithermal, supergene copper-uranium (silver), and Great Plains Margin types. Late Cretaceous to mid-Tertiary deposits include the sedimentary-hydrothermal barite-fluorite-galena, carbonate-hosted silver (lead manganese ), lead-zinc and copper skarn, Laramide vein, and prophyry-copper types. Late Paleozoic to early Mesozoic deposits include the sedimentary-copper type and possibly some of the Permian Mississippi Valley type. Precambrian deposits include the vein and replacement and Precambrian massive-sulfide types. Deposits that have produced significant silver and/or gold as the primary product are the placer, volcanic-epithermal, Great Plains Margin, carbonate-hosted silver, and Lar amide vein types. Deposits that have produced significant precious metals as a byproduct of base metal mining include the carbonate-hosted lead-zinc, copper skarn, and porphyry-copper types. Introduction Precious metals in varying degrees of importance or 14 ppm (0.41 oz/ton) silver. -
Evidence for Controlled Deformation During Laramide Orogeny
Geologic structure of the northern margin of the Chihuahua trough 43 BOLETÍN DE LA SOCIEDAD GEOLÓGICA MEXICANA D GEOL DA Ó VOLUMEN 60, NÚM. 1, 2008, P. 43-69 E G I I C C O A S 1904 M 2004 . C EX . ICANA A C i e n A ñ o s Geologic structure of the northern margin of the Chihuahua trough: Evidence for controlled deformation during Laramide Orogeny Dana Carciumaru1,*, Roberto Ortega2 1 Orbis Consultores en Geología y Geofísica, Mexico, D.F, Mexico. 2 Centro de Investigación Científi ca y de Educación Superior de Ensenada (CICESE) Unidad La Paz, Mirafl ores 334, Fracc.Bella Vista, La Paz, BCS, 23050, Mexico. *[email protected] Abstract In this article we studied the northern part of the Laramide foreland of the Chihuahua Trough. The purpose of this work is twofold; fi rst we studied whether the deformation involves or not the basement along crustal faults (thin- or thick- skinned deformation), and second, we studied the nature of the principal shortening directions in the Chihuahua Trough. In this region, style of deformation changes from motion on moderate to low angle thrust and reverse faults within the interior of the basin to basement involved reverse faulting on the adjacent platform. Shortening directions estimated from the geometry of folds and faults and inversion of fault slip data indicate that both basement involved structures and faults within the basin record a similar Laramide deformation style. Map scale relationships indicate that motion on high angle basement involved thrusts post dates low angle thrusting. This is consistent with the two sets of faults forming during a single progressive deformation with in - sequence - thrusting migrating out of the basin onto the platform. -
Mineral and Energy Resources of the BLM Roswell Resource Area, East-Central New Mexico
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Mineral and Energy Resources of the BLM Roswell Resource Area, East-central New Mexico by Susan Bartsch-Winkleri, editor Open-File Report 92-0261 1992 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1 Denver, Colorado iMail Stop 937 Federal Center P.O. Box 25046 Denver, Colorado 80225 MINERAL AND ENERGY RESOURCES OF THE BLM ROSWELL RESOURCE AREA, EAST-CENTRAL NEW MEXICO Summary.......................................................................................... 1 Introduction.................................................................................... 1 Location and geography of study area...................................... 1 Purpose and methodology........................................................ 3 Acknowledgements......................................................................... 4 Geology of east-central New Mexico, by Susan Bartsch-Winkler, with a section on Intrusive and extrusive alkaline rocks of the Lincoln County porphyry belt by Theodore J. Armbrustmacher 4 General..................................................................................... 4 Structure................................................................................. 5 Uplifts........................................................................ -
Geologic Map of the Truth Or Consequences 30' X 60' Minute
1 GeoloPic MaD of the Truth or Conseauences 30 x 60 Minute Ouadrande (1:lOO.OOO scale) Richard W. Harrison, Richard P. Lozinsky, Ted L. Eggleston, and William C. McIntosh INTRODUCTION The geologic map of the Truth or Consequences 30 x 60 minute quadrangle has grown out of the Ph.D. dissertations and related work of the authors in south-central New Mexico. Funding and support for this work was provided by New Mexico Bureau of Mines and Mineral Resources. And while the authors have mapped extensive portionsof the sheet in either detailed or reconnaissance fashion, large areas of the sheet have been compiled from existing maps (see attached diagram for sources). This is an in-progress status report. Many aspects of the complex geology found in this area are yet to be worked out. Descriptions of stratigraphy and swcture provided in this report are brief. For more details, reference is given to Eggleston (1986), McIntosh (1989), Harrison (1990), and Lozinsky and Hawley (1986). STRATIGRAPHY QC Quaternarycolluvium QcaQuaternary alluvium andcolluvium, undivided QPgQuaternary piedmont slopedeposits To basalts:Tertiary Pliocene, approximately 4.2-4.8 Ma (IUAr dates) in Winston-Las Animas grabens, approximately2.1 Ma (K/Ardate) in Cutter Sag area, the younger group upon a pediment surface in the Cutter Sag area. Tsf Santa Fe Group: Oligocene and younger basin fill of the Rio Grande drainage west of the Continental Divide: basal beds are intercalated with Oligocene volcanic rocks,are moderately well indurated, more voluminous, younger beds overlie basal beds with angular unconformity andare generally near horizontalin attitude. The Santa Fe Group is dominantly volcaniclastic and heterolithic. -
Bulletin 39: the Metal Resources of New Mexico and Their Economic
BULLETIN 3 9 The Metal Resources of New Mexico and Their Economic Features Through 1954 A revision of Bulletin 7, by Lasky and Wootton, with detailed information for the years 1932-1954 BY EUGENE CARTER ANDERSON 1957 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EX OFFICIO THE HONORABLE EDWIN L. MECHEM………...Governor of New Mexico MRS. GEORGIA L. LUSK ......................Superintendent of Public Instruction APPOINTED MEMBERS ROBERT W. BOTTS ....................................................................Albuquerque HOLM O. BURSUM, JR. .....................................................................Socorro THOMAS M. CRAMER .................................................................... Carlsbad JOHN N. MATHEWS, JR. ...................................................................Socorro RICHARD A. MATUSZESKI ......................................................Albuquerque Contents Page INTRODUCTION .......................................................................................................... 1 Purpose and Scope of Bulletin ..................................................................................... 1 Other Reports Dealing With the Geology and Mineral Resources of New Mexico ...................................................................................................... -
Compiled by F. Allan Hills and KA Sargent This Map Report Is One of a Series of Geologic and Hydro
DEPARTMENT OF THE INTERIOR TO ACCOMPANY UNITED STATES GEOLOGICAL SURVEY WRI REPORT 83-4118-D MAP SHOWING OUTCROPS OF GRANITIC ROCKS AND SILICIC SHALLOW-INTRUSIVE ROCKS, BASIN AND RANGE PROVINCE, NEW MEXICO Compiled by F. Allan Hills and K. A. Sargent INTRODUCTION This map report is one of a series of geologic and hydro- logic maps covering all or parts of the States within the Basin and Range province of the western United States. The map reports contain information on subjects that characterize the geohy- drology of the province, including the ground-water hydrology, ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources. This work is part of the U.S. Geological Survey's program for geologic and hydro- logic evalutaion of the Basin and Range province to identify potentially suitable regions for further study relative to storage of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984). This map report on the granitic rocks and silicic shallow- intrusive rocks of New Mexico was prepared from published geo logic maps and reports utilizing the project guidelines of Sargent and Bedinger (1984). The map shows outcrops of mostly plutonic granitic rocks, but also of fine-grained and partly glassy, silicic, shallow-intrusive rocks. The outcrops have been grouped into numbered county areas, which are outlined on the map. The Description of Map Units includes the geologic, and if available, radiometric ages, the lithology, thickness where available, and sources of data. Because the classification of plutonic igneous rocks has changed since publication of many reports used in this study, the rock terminology in the original reports has been converted, where possible, to that adopted by the International Union of Geologic Sciences (IUGS), as reported by Streckeisen (1976). -
Metamorphism
Contents AΒSTRACT 7 STRUCTURAL GEOLOGY 31 INTRODUCTION 7 SMP BLOCK 31 METAMORPHIC ROCKS 11 SAN ANDRES MOUNTAINS 32 MICA-QUARTZ SCHIST AND PHYLLITE 11 PEDERNAL HILLS 32 QUARTZITE AND RELATED ROCKS 13 LADRON MOUNTAINS 33 MAFIC META-IGNEOUS ROCKS 16 OTHER AREAS 33 SILICEOUS META-IGNEOUS ROCKS 18 CONCLUSIONS 33 GNEISS 20 METAMORPHISM 34 STRATIGRAPHY 21 GEOCHRONOLOGY 37 GRANITIC ROCKS 24 GEOCHEMISTRY 38 NORTH AND SOUTH SANDIA PLUTONS 25 MAFIC META-IGNEOUS ROCKS 38 MANZANITA PLUTON 26 SILICEOUS META-IGNEOUS ROCKS AND GRANITIC ROCKS 40 ΟJΙΤΑ AND MONTE LARGO PLUTONS 26 High-Ca group 40 PRIEST PLUTON 27 High-K group 42 LOS PINOS PLUTON 27 High-Si group 43 SEPULTURA PLUTON 27 Effects of alteration 44 PEDERNAL PLUTON 27 FELDSPATHIC QUARTZITES AND ARKOSITES 45 LADRON PLUTON 28 MAGMA ORIGIN 47 CAPIROTE PLUTON 28 TECTONIC SETTING AND LA JOYITA PLUTON 28 GEOLOGIC EVOLUTION 48 POLVADERA PLUTON 28 MINERAL DEPOSITS 50 MAGDALENA PLUTON 28 REFERENCES 51 OSCURA AND CAPITOL PEAK PLUTONS 28 APPENDICES 54 MOCKINGBIRD GAP PLUTON 29 1—Composite stratigraphic sections 54 STRAWBERRY PEAK AND MAYBERRY PLUTONS 30 2—Major-element chemical analyses (microfiche SAN ANDRES PLUTON 30 in pocket) MINERAL HILL PLUTON 30 3—Trace-element contents (microfiche in pocket) GRANITIC ROCKS OF THE CABALLO MOUNTAINS AND 4—Sample locations (microfiche in pocket) RED HILLS 30 INDEX 57 MISCELLANEOUS PLUTONS 30 Tables 1—Relative percentages of metamorphic rocks in Precambrian 9—Geochemical classification of Precambrian siliceous meta- sections 11 igneous rocks and granitic plutons 40 2—Modal