Map and Data for Quaternary Faults in West Texas and Adjacent Parts of Mexico
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A Glimpse of Some of the Geology and Mineral Resources: Sierra Blanca
THE EL.PAS0 GEOLOGICAL SOCIETY I I GUIDEBOOK i FIFTH ANNUAL FIELD TRIP I I I I A GLIMPSE OF SOME OF THE I GEOLOGY AND MINERAL RESOURCES I I SIERRA BLANCA-VAN HORN COUNTRY HUDSPETH AND CULBEWSON COUNTIES TEXAS > APRIL 3, 1971 iii TABLE OF CONTENTS F - The Texas Lineament in Eagle Flat, Texas ------------- 28 INTRODUCTION The Trans Pecos region of West Texas has attracted the attention I it deserves as a source of useful minerals both metallic and nsn- metallic. Because of the preoccupation of the people of Texas with petroleum production, many have overlooked the fact that them have been several important metal mines tn this province and that talc deposi ts are s ti1 l being worked here. Undoubtedly othep economic mineral deposits exist in the region awai ting discovery by intensive geological prospecting. The af'fi cers of the El Paso Geological Society and the field trip leadek hope that this trip will heighten inteest in the finding and developing of mineral deposi ts in Trans Pecos Texas. We welcome all our visitcs~sand know that they will wish to jodn us in thanking all those who made thds trip possible. We wish especially to acknowledge the kindness of the Pioneer Talc Company in showing us through the mill at Allamore and allowlng the group to visdt the Texsla- Talc mine. We also wish to thank Mr. Sandy Neal of Van Haon for per- mission to cross the Neal Ranch on the way to the Hazel Wne. John M. Hills, President El Paso Geological Society EL PAS0 GEOLOGICAL SOCIETY OFFICERS John M. -
Geochronology of the Trans-Pecos Texas Volcanic Field John Andrew Wilson, 1980, Pp
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/31 Geochronology of the Trans-Pecos Texas volcanic field John Andrew Wilson, 1980, pp. 205-211 in: Trans Pecos Region (West Texas), Dickerson, P. W.; Hoffer, J. M.; Callender, J. F.; [eds.], New Mexico Geological Society 31st Annual Fall Field Conference Guidebook, 308 p. This is one of many related papers that were included in the 1980 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. -
2018 Hummingbird Celebration Field Trips
Davis Mountains Hummingbird Celebration Field Trips & Photo Workshops Unless otherwise noted, all Field Trips will Carpool from the Chamber. What to bring on your Field Trip: Hat, Water, Binoculars and a Snack Come Early - Enjoy Special Field Trips and Extras! SOLD OUT! SPECIAL FIELD TRIP #1 – Photographing High Elevation Hummingbirds DAYS: Monday thru Thursday Noon (8/20-23) PARTICIPATION LIMIT: 8 DRIVE: Crow’s Nest Ranch PRICE: $875 DESCRIPTION Learn advanced hummingbird photography from professional wildlife photograper (& biologist) Larry Ditto. Practice the secrets of the “Pros” in the Davis Mountains and photograph a variety of species coming to feeders. This is a rare opportunity to capture potentially ten species. TARGET BIRDS: Rivoli’s, Lucifer, Ruby-throated, Black-chinned, Calliope, Broad-tailed and Rufous hummingbirds. Could possibly get Blue-throated, Mexican Violet Ear and Broad-billed Hummingbirds. SPECIAL FIELD TRIP #2 (Arrive Weds. Afternoon) – Hummingbirds, Sky Islands and Astronomy DAYS: Wednesday evening, August, 22 ONLY PARTICIPATION LIMIT: 30 EXTRAS TO BRING: PORTABLE CHAIR TRIP TIME: 5:30 – 9:30 PM DRIVE DIFFICULTY: EASY – ADA Accessible PRICE: $55 DESCRIPTION Take a trip to see Hummingbirds, Enjoy Spectacular Vistas and Explore the World of Astronomy You are invited to spend the evening as guests of the McDonald Observatory to enjoy some of the smallest and largest wonders in the Universe. View a variety of hummingbird species, enjoy breathtaking vistas, a very fine dinner and learn about astronomy from the experts. We will carpool twelve miles up to the McDonald Observatory complex on Mount Locke. Starting in town at 5,050 feet we will climb out of Yucca-Sotol Grasslands to the higher elevation of Oak-Pinyon forest at 6,791 feet. -
United States Geological Survey
DEFARTM KUT OF THE 1STEK1OK BULLETIN OK THE UNITED STATES GEOLOGICAL SURVEY No. 19O S F, GEOGRAPHY, 28 WASHINGTON GOVERNMENT PRINTING OFFICE 1902 UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR GAZETTEEK OF TEXAS BY HENRY G-A-NNETT WASHINGTON GOVERNMENT PRINTING OFFICE 1902 CONTENTS Page. Area .................................................................... 11 Topography and drainage..... ............................................ 12 Climate.................................................................. 12 Forests ...............................................................'... 13 Exploration and settlement............................................... 13 Population..............'................................................. 14 Industries ............................................................... 16 Lands and surveys........................................................ 17 Railroads................................................................. 17 The gazetteer............................................................. 18 ILLUSTRATIONS. Page. PF,ATE I. Map of Texas ................................................ At end. ry (A, Mean annual temperature.......:............................ 12 \B, Mean annual rainfall ........................................ 12 -ryj (A, Magnetic declination ........................................ 12 I B, Wooded areas............................................... 12 Density of population in 1850 ................................ 14 B, Density of population in 1860 -
Physiographic Features, Trans-Pecos Region James R
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/31 Physiographic features, Trans-Pecos region James R. Underwood Jr., 1980, pp. 57-58 in: Trans Pecos Region (West Texas), Dickerson, P. W.; Hoffer, J. M.; Callender, J. F.; [eds.], New Mexico Geological Society 31st Annual Fall Field Conference Guidebook, 308 p. This is one of many related papers that were included in the 1980 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. -
Geology of the Eagle Mountains, Hudspeth County, Texas James R
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/31 Geology of the Eagle Mountains, Hudspeth County, Texas James R. Underwood Jr., 1980, pp. 183-193 in: Trans Pecos Region (West Texas), Dickerson, P. W.; Hoffer, J. M.; Callender, J. F.; [eds.], New Mexico Geological Society 31st Annual Fall Field Conference Guidebook, 308 p. This is one of many related papers that were included in the 1980 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. -
Chapter 17 Hydrogeology of the Salt Basin
Chapter 17 Hydrogeology of the Salt Basin Edward S. Angle1 Introduction The Salt Basin of West Texas has been a significant source of groundwater to local users in West Texas for most of the last century. In a region of normally low rainfall and high evaporation, groundwater is a vital resource to municipalities, industries, and landowners in the Salt Basin. Because El Paso is facing serious water shortages in the next 20 to 30 years, city and regional planners are looking, in part, to water resources in the Salt Basin. It is therefore important to understand how pumping and drought impact the aquifers of the Salt Basin to maintain its viability for West Texans in the future. Although many people think of the Salt Basin as being the salt flats north of Van Horn, the Salt Basin as a physiographic feature extends much farther south and includes the Salt, Wild Horse, Michigan, Lobo, and Ryan Flats (fig. 17-1). The sediments beneath these flats hold water that form part of the West Texas Bolsons aquifer (Ashworth and Hopkins, 1995). The purpose of this paper is to present a brief overview of the hydrogeology of the area and to present results of water-level and water-quality information collected between 1992 and 1994 by the Texas Water Development Board. Physiography The Salt Basin is located in the Trans-Pecos region of West Texas. It forms a valley that extends from just north of the New Mexico border in Hudspeth and Culberson Counties along a southeastern trend through western Jeff Davis County, where it ends in the northwest portion of Presidio County. -
Mammals of the Guadalupe Mountains National Park, Texas
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Mammalogy Papers: University of Nebraska State Museum Museum, University of Nebraska State 4-4-1975 Mammals of the Guadalupe Mountains National Park, Texas Hugh H. Genoways University of Nebraska - Lincoln, [email protected] Robert J. Baker Texas Tech University, [email protected] John E. Cornely Texas Tech University Follow this and additional works at: https://digitalcommons.unl.edu/museummammalogy Part of the Biodiversity Commons, Other Ecology and Evolutionary Biology Commons, and the Zoology Commons Genoways, Hugh H.; Baker, Robert J.; and Cornely, John E., "Mammals of the Guadalupe Mountains National Park, Texas" (1975). Mammalogy Papers: University of Nebraska State Museum. 114. https://digitalcommons.unl.edu/museummammalogy/114 This Article is brought to you for free and open access by the Museum, University of Nebraska State at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Mammalogy Papers: University of Nebraska State Museum by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Mammals of the Guadalupe Mountains National Park, Texas HUGH H. GENOWAYS, ROBERT J. BAKER and JOHN E. CORNELY, Texas Tech University, Lubbock The Guadalupe Mountains National Park was authorized by an act of Congress on 15 October 1966 and was formally established on 30 September 1972. The park covers 76,468.6 acres located in Culberson and Hudspeth counties of Trans-Pecos Texas. The park contains the Texas portion ofthe uplifted Capitan Reef of Permian age. The southern end ofthe escarpment is marked by the prominent El Capitan. The escarpment extending northwest from El Capitan contains other impressive peaks including Guadalupe Peak, which at 8759 ft is the highest point in Texas. -
Chapter 2 Geologic History of West Texas
Chapter 2 Geologic History of West Texas Kevin Urbanczyk1, David Rohr1, and John C. White1 Introduction The region embraced within the Trans-Pecos region of Texas encompasses many snapshots of North American geologic history. Precambrian crystalline metamorphic rocks are exposed in the Franklin Mountains, Van Horn Mountains, and Sierra Diablo Mountains. Xenoliths of these rocks recovered from volcanic rocks in the Davis Mountains, Bofecillos Mountains, and Chisos Mountains provide strong evidence that almost all of Trans-Pecos Texas is underlain by Precambrian rocks similar to those that crop out at the surface. Cambrian to Pennsylvanian rocks crop out in the Franklin Mountains, Marathon Basin, Solitario, and at Persimmon Gap. These rocks represent a transgressive, then regressive, marine sequence that was caught between the North American continent and another unidentified continent during the Pennsylvanian and intensely deformed and thrust onto North America forming the Marathon-Ouachita Mountains. The foreland basin of these mountains became the Permian Basin, and the carbonate rocks associated with this intracratonic sea now crop out in the Guadalupe, Glass, Apache, Van Horn, and Sierra Diablo mountain ranges. A depositional hiatus from the Triassic to Mid-Cretaceous was followed by the deposition of Mid- to Late- Cretaceous limestone that covers much of central and west Texas and frequently hosts important aquifers. From the Late Cretaceous to the Early Tertiary, these rocks were locally deformed during the Laramide Orogeny, which can be seen in the Del Norte- Santiago Mountains, Mariscal Mountain, the Terlingua-Fresno Monocline, and in the Chihuahua Tectonic Belt. Laramide compression was followed by a long period of large- scale ignimbritic volcanism in Trans-Pecos Texas. -
Tertiary Formations of Rim Rock Country, Presidio County, Trans-Pecos Texas
Tertiary Formations of Rim Rock Country, Presidio County, Trans-Pecos Texas RONALD K. DeFORD The University of Texas Reprinted, from THE TEXAS JOURNAL OP SCIENCE, Vol. X, No. 1, March, 1958 Reprinted from THE TEXAS JOURNAL OP SCIENCE, Vol. X, No. 1, March, 1958 Tertiary Formations of Rim Rock Country, Presidio County, Trans-Pecos Texas RONALD K. DeFORD The University of Texas ABSTRACT The rim rock of the Vieja Rim, the quartz pantellerite of Lord, is named the Bracks Rhyolite. Beneath the Bracks, the "Vieja series" of Vaughn (1900), which is newly subdivided into five formations named, in descending order,the Chambers Tuff, Buckshot Ignimbrite, Colmena Tuff, Gill Breccia, and Jeff Conglomerate, rests unconform- ably on Upper Cretaceous formations. The Vieja Group is expanded to include also the Bracks and three overlying formations, named, in ascending order, the Capote Mountain Tuff, the Brite Ignimbrite, the Petan Basalt. An ancient post-volcanic gravel above the Petan ante- dates the bolson fill. The minimum hiatus at the base of the Vieja may include part of the Upper Cretaceous, all the Paleocene, and most of the Eocene epochs. The age of major faulting that created the bolsons is pre-Pleistocene, and probably most of the bolson fill was deposited before the end of the Tertiary Period. INTRODUCTION In 1922 Charles Laurence Baker (1927, p. 5, fn. 1) completed a manuscript on the geology of the most inaccessible part of Texas, which he had mapped at the rate of 35 square miles per day. His map- ping was an exploratory feat of the first order, and his account of the geology is fundamental. -
Quaternary Faulting in Salt Basin Graben, West Texas Lisa K
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/31 Quaternary faulting in Salt Basin Graben, West Texas Lisa K. Goetz, 1980, pp. 83-92 in: Trans Pecos Region (West Texas), Dickerson, P. W.; Hoffer, J. M.; Callender, J. F.; [eds.], New Mexico Geological Society 31st Annual Fall Field Conference Guidebook, 308 p. This is one of many related papers that were included in the 1980 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. -
Early Basin and Range Development in Trans&Hyphen;Pecos Texas And
JOURNALOF GEOPHYSICALRESEARCH, VOL. 91, NO. B6, PAGES6213-6224, MAY 10, 1986 EARLY BASIN AND RANGE DEVELOPMENT IN TRANS-PECOS TEXAS AND AD3ACENT CHIHUAHUA: MAGMATISM AND ORIENTATION, TIMING, AND STYLE OF EXTENSION Christopher D. Henry and 3onathan G. Price Bureau of Economic Geology, The University of Texas at Austin Abstract. Magmatism during early Basin and Range Zoback and Thompson [1978], Zoback e(al. [1981], extension in Trans-Pecos Texas consisted of widespread Lipman [1981], and Laughlinet al. [19831have usedthis but volumetrically minor alkali basalts (24-17 Ma), an principle to present evidence.that early (30-10 Ma) alkalic mafic to intermediate composition strato- tension throughout the Basin and Range province was volcano (28-27 Ma), and a dominantly rhyolitic, possibly oriented ENE. Data from the Rio Grande rift in New bimodal, caldera complex in adjacent Chihuahua (31- Mexico were included in thes• studies, but until 28 Ma). This magmatism contrasted sharply with the recently, few data were available from Texas. much more voluminous and compositionally more di- Dasch et al. [1969], in the only previous study to verse Eocene-Oligocene magmatism. The age and ori- address this question, dated WNW striking and NNW entation of dikes eraplaced during this magmatic epi- striking Rim Rock dikes in the Texas portion of the sode have been used to determine the orientation of Basin and Range province (Figure 1). They suggested least principal stress, o 3 . An ENE orientation of o3, that o 3 was NNE at about 23 Ma and ENE at about similar to early extension throughout the Basin and 19 Ma.