Organ Mountains National Conservation Area
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An Interpretation of the Structural Geology of the Franklin Mountains, Texas Earl M
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/26 An interpretation of the structural geology of the Franklin Mountains, Texas Earl M. P. Lovejoy, 1975, pp. 261-268 in: Las Cruces Country, Seager, W. R.; Clemons, R. E.; Callender, J. F.; [eds.], New Mexico Geological Society 26th Annual Fall Field Conference Guidebook, 376 p. This is one of many related papers that were included in the 1975 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. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
An Environmental History of the Middle Rio Grande Basin
United States Department of From the Rio to the Sierra: Agriculture Forest Service An Environmental History of Rocky Mountain Research Station the Middle Rio Grande Basin Fort Collins, Colorado 80526 General Technical Report RMRS-GTR-5 Dan Scurlock i Scurlock, Dan. 1998. From the rio to the sierra: An environmental history of the Middle Rio Grande Basin. General Technical Report RMRS-GTR-5. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 440 p. Abstract Various human groups have greatly affected the processes and evolution of Middle Rio Grande Basin ecosystems, especially riparian zones, from A.D. 1540 to the present. Overgrazing, clear-cutting, irrigation farming, fire suppression, intensive hunting, and introduction of exotic plants have combined with droughts and floods to bring about environmental and associated cultural changes in the Basin. As a result of these changes, public laws were passed and agencies created to rectify or mitigate various environmental problems in the region. Although restoration and remedial programs have improved the overall “health” of Basin ecosystems, most old and new environmental problems persist. Keywords: environmental impact, environmental history, historic climate, historic fauna, historic flora, Rio Grande Publisher’s Note The opinions and recommendations expressed in this report are those of the author and do not necessarily reflect the views of the USDA Forest Service. Mention of trade names does not constitute endorsement or recommendation for use by the Federal Government. The author withheld diacritical marks from the Spanish words in text for consistency with English punctuation. Publisher Rocky Mountain Research Station Fort Collins, Colorado May 1998 You may order additional copies of this publication by sending your mailing information in label form through one of the following media. -
Late Paleozoic Tectonic and Sedimentologic History of the Penasco Uplift, North-Central New Mexico
RICE UNIVERSITY LATE PALEOZOIC TECTONIC AND SEDIMENTOLOGIC HISTORY OF THE PENASCO UPLIFT, NORTH-CENTRAL NEW MEXICO by ROY DONALD ADAMS A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE MASTER OF ARTS APPROVED, THESIS COMMITTEE: 0^ (3- /jtd&i obfe B. Anderson, Chairman Assistant Professor pf Geology KT Rudy R. Schwarzer, Adjunct Assistant Professor of GSology John /E. Warme Professor of Geology Donald R. Baker Professor of Geology Houston, Texas May, 1980 ABSTRACT LATE PALEOZOIC TECTONIC AND SEDIMENTOLOGIC HISTORY OF THE PENASCO UPLIFT, NORTH-CENTRAL NEW MEXICO Roy Donald Adams The Paleozoic Peiiasco Uplift, located on the site of the present Nacimiento Mountains of north-central New Mexico, acted as a sediment source and modifier of regional sedimentation patterns from Middle Pennsylvanian to Early Permian time. The earliest history of the uplift is still poorly defined. Orogenic activity may have started as early as the Late Mississippian, or there may have been quiescence until after deposition of the Morrow-age Osha Canyon Formation and prior to deposition of the Atoka-age Sandia Formation. Coarse, arkosic siliciclastic sediments inter- bedded with fossilferious carbonates in the Madera Formation indicate that by early Desmoinesian time the Peiiasco Uplift had risen sufficiently to expose and erode Precambrian rocks. Paleotransport indicators in the arkosic sediments show transport away from the uplift. Throughout the remainder of the Pennsylvanian, the Peiiasco Uplift was a sediment source. The siliciclastic sediments derived from the Peiiasco Uplift formed a wedge that prograded out onto and interfingered with carbonate sediments of a shallow normal marine shelf. A change in paleotransport directions from northeasterly to southwesterly occurs on the east side of the Peiiasco Uplift and is due to the arrival of a flood of siliciclastic sediments derived from the Uncompahgre-San Luis Uplift to the northeast. -
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. -
Promise Beheld and the Limits of Place
Promise Beheld and the Limits of Place A Historic Resource Study of Carlsbad Caverns and Guadalupe Mountains National Parks and the Surrounding Areas By Hal K. Rothman Daniel Holder, Research Associate National Park Service, Southwest Regional Office Series Number Acknowledgments This book would not be possible without the full cooperation of the men and women working for the National Park Service, starting with the superintendents of the two parks, Frank Deckert at Carlsbad Caverns National Park and Larry Henderson at Guadalupe Mountains National Park. One of the true joys of writing about the park system is meeting the professionals who interpret, protect and preserve the nation’s treasures. Just as important are the librarians, archivists and researchers who assisted us at libraries in several states. There are too many to mention individuals, so all we can say is thank you to all those people who guided us through the catalogs, pulled books and documents for us, and filed them back away after we left. One individual who deserves special mention is Jed Howard of Carlsbad, who provided local insight into the area’s national parks. Through his position with the Southeastern New Mexico Historical Society, he supplied many of the photographs in this book. We sincerely appreciate all of his help. And finally, this book is the product of many sacrifices on the part of our families. This book is dedicated to LauraLee and Lucille, who gave us the time to write it, and Talia, Brent, and Megan, who provide the reasons for writing. Hal Rothman Dan Holder September 1998 i Executive Summary Located on the great Permian Uplift, the Guadalupe Mountains and Carlsbad Caverns national parks area is rich in prehistory and history. -
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. -
General Geology of the Franklin Mountains, El Paso County, Texas
THE GENERAL GEOLOGY OF THE FRANKLIN MOUNTAINS, EL PASO COUNTY, TEXAS EL PASO GEOLOGICAL SOCIETY AND PERMIAN BASIN SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS FEBRUARY 24, 1968 Society Members Permian Basin Section El Paso Geological Society Society of Economic Paleontologists and Mineralogists Robert Habbit, President W.F. Anderson, President David V. LeMone, Vice President Richard C. Todd, First Vice President Karl W. Klement, Second Vice President Charles Crowley, Secretary Kenneth O. Sewald, Secretary William S. Strain Gerald L. Scott, Treasurer Editor and Coordinator: David V. LeMone ii TABLE OF CONTENTS Page Introduction ............................................................................. ii Robert Habbit General Geology of the Franklin Mountains: Road Log .......................................... 1 David V. LeMone Precambrian Rocks of the Fusselman Canyon Area ............................................. 12 W.N. McAnulty, Jr. Paleoecology of a Canadian (Lower Ordovician) Algal Complex .................................. 15 David V. LeMone Late Paleozoic in the El Paso Border Region .................................................. 16 Frank E. Kottlowski Late Cenozoic Strata of the El Paso Area ..................................................... 17 William S.Strain A Preliminary Note on the Geology of the Campus “Andesite .................................... 18 Jerry M. Hoffer Conjectural Dating by Means of Gravity Slide Masses of Cenozoic Tectonics of the Southern Franklin Mountains, El Paso County, Texas .......................................... -
Kornze Testimony Re S. 3049 Organ Mountains-Desert Peaks 9-22-16
Statement of Neil Kornze Director U.S. Department of the Interior, Bureau of Land Management Senate Energy and Natural Resources Committee S. 3049, Organ Mountains-Desert Peaks Conservation Act September 22, 2016 Thank you for inviting the Bureau of Land Management (BLM) to testify on S. 3049, the Organ Mountains-Desert Peaks Conservation Act. The BLM supports S. 3049, which designates eight new wilderness areas and includes direction for future management on additional public lands in Doña Ana County, New Mexico. We would like the opportunity to work further with the sponsors and Subcommittee on certain aspects of the bill that we believe would facilitate implementation and improve the manageability of the areas that would be designated by S. 3049. Background Doña Ana County is many things – the county with the second highest population in New Mexico; home to Las Cruces, one of the fastest growing cities in the country; and a land of amazing beauty. Towering mountain ranges, dramatic deserts, and fertile valleys characterize this corner of the Land of Enchantment. The Organ Mountains, east of the city of Las Cruces, dominate the landscape. Characterized by steep, angular, barren rock outcroppings, the Organ Mountains rise to nearly 9,000 feet in elevation and extend for 20 miles, running generally north and south. This high-desert landscape within the Chihuahua Desert contains a multitude of biological zones – mixed desert shrubs and grasslands in the lowlands ascending to pinon and juniper woodlands, and finally to ponderosa pines at the highest elevations. Consequently, the area is home to a high diversity of animal life, including peregrine falcons and other raptors, as well as mountain lions and other mammals. -
Features of the Tularosa Basin Place Names in New Mexico, As You Might Imagine, Often Derive from Native American, Spanish, and Anglo Words and Family Names
National Park Service White Sands Department of the Interior White Sands National Monument Features of the Tularosa Basin Place names in New Mexico, as you might imagine, often derive from Native American, Spanish, and Anglo words and family names. The Tularosa Basin is no exception—the word “tularosa” is Spanish for “reddish reeds.” Like much of the American Southwest, the basin is full of such colorful place names. Below you’ll find a description of the most significant features, arranged to correspond with the accompanying map. The Chupadera Mesa is an upland rising at the north end of the Tularosa Basin. Chupadera probably refers to “sinkholes”—although geographer T. M. Pearce says that it could also refer to “sucking insects.” Chupadero The Oscura Mountains form the northwest border of the Tularosa Mesa basin. Oscura means “dark” in Spanish, and with their piñon and juniper forested tops, the Oscura Mountains can appear darker than the neighboring San Andres Mountain range to the south. The highest elevation in the range is Oscura Peak at 8,732 feet high. The San Andres Mountains border the Tularosa Basin on the west. The range extends approximately 75 miles north to south. The highest Oscura point is Salinas Peak, with an elevation just under 9,000 feet. The Mountains southern San Andres Mountains are home to a wildlife refuge of the same name. However, the San Andres National Wildlife Refuge and the San Andres Mountains are within the boundaries of the White * Carrizozo Sands Missile Range and therefore closed to public access. The Oscura Mountains to the north are separated from the San Andres range at Mockingbird Gap, while the Organ Mountains to the south are separated from the San Andres by San Augustin Pass. -
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). -
EPGS Guidebook
THE EL PAS0 GEOLOGICAL SOCIETY GUIDEBOOK FOURTH ANNUAL FIELD TRIP CENOZOIC STRATIGRAPHY Of THE RIO GRANDE VALLEY AREA DORA ANA COUNTY NEW MEXICO MARCH 14, 1970 CENOZOIC STRATIGRAPHY OF THE RIO GRANDE VALLEY AREA DQk ANA COUNTY, NEW MEXICO John W. Hawley - Editor and Cmpi ler GUIDEBOOK FOURTH ANNUAL FIELD TRIP of the EL PAS0 GEOLOGICAL SOCIETY March 14, 1970 Compiled in Cooperati on with: Department of Geological Sciences, University of Texas at El Paso Earth Sciences and Astronomy Department, New Mexi co State University Soi 1 Survey Investigations, SCS, USDA, University Park, New Mexico New Mexico State Bureau of Mines and Mineral Resources, Socorro, New Mexico EL PAS0 GEOLOGICAL SOCIETY OFFICERS Charles J. Crowley Presi dent El Paso Natural Gas C. Tom Hollenshead Vice President El Paso Natural Gas Carl Cotton Secretary El Paso Indpt. School Dist. Thomas F. Cliett Treasurer El Paso Water Utilities Wi11 iam N. McAnul ty Counci lor Dept. Geol. Sci., UTEP Robert D. Habbit Councilor El Paso Natural Gas FIELD TRIP COMMITTEES Guidebook John W. Hawley Edi tor and compi 1er Soi 1 Survey Invest., SCS Jerry M. Hoffer Contributor and editing Dept. Geol. Sci., UTEP William R. Seager Contributor and editing Earth Sci. Dept. NMSU Frank E. Kottlowski Contributor and editing N. M. Bur. Mines & Min. Res. Earl M.P. Lovejoy Contributor and editing Dept. Geol. Sci., UTEP William S. Strain Contributor and editing Dept. Geol. Sci., UTEP Paul a Blackshear Typing Dept. Geol . Sci ., UTEP Robert Sepul veda Drafting Dept. Geol . Sci ., UTEP Caravan Earl M. P. Lovejoy Pub1 icity and Regi stration Charles J. -
Stratigraphy of the San Andres Mountains in South-Central New Mexico Frank E
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/26 Stratigraphy of the San Andres Mountains in south-central New Mexico Frank E. Kottlowski, 1975, pp. 95-104 in: Las Cruces Country, Seager, W. R.; Clemons, R. E.; Callender, J. F.; [eds.], New Mexico Geological Society 26th Annual Fall Field Conference Guidebook, 376 p. This is one of many related papers that were included in the 1975 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. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.