2 edition of Water resources in basin-fill deposits in the Tularosa Basin, New Mexico found in the catalog.
Water resources in basin-fill deposits in the Tularosa Basin, New Mexico
Brennon R. Orr
1986 by U.S. Dept. of the Interior, Geological Survey, Open-File Services Section, Branch of Distribution in Albuquerque, N.M, Denver, Colo .
Written in English
|Statement||by Brennon R. Orr and Robert G. Myers ; prepared in cooperation with the U.S. Bureau of Reclamation.|
|Series||Water-resources investigations report -- 85-4219|
|Contributions||Myers, Robert G. 1950-, United States. Bureau of Reclamation, Geological Survey (U.S.)|
|The Physical Object|
|Pagination||vi, 94 p. :|
|Number of Pages||94|
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Get this from a library. Water resources in basin-fill deposits in the Tularosa Basin, New Mexico. [Brennon R Orr; Robert G Myers; United States. Bureau of. WATER RESOURCES IN BASIN-FILL DEPOSITS IN THE TULAROSA BASIN, NEW MEXICO By Brennon R.
Orr and Robert G. Myers ABSTRACT The Tularosa Basin, a faulted intermontane depression in south-central New Mexico, contains a thick sequence of alluvial and lacustrine deposits of Tertiary and Quaternary by: New Mexico Bureau of GeoloGy aNd MiNeral resources Brackish Water Assessment in the Eastern Tularosa Basin, New Mexico open-file report June B.
Talon Newton Lewis Land 4, 4, 3, 3, 2, 0 5 10 15 20 25 Elevation (ft) Distance (mi) saline and brine slig htly brackis h slightly brackish h large vertical exageration surface File Size: 1MB. Orr, B.R., and Myers, R.G.,Water resources in basin-fill deposits in the Tularosa Basin, New Mexico: U.S.
Geological Survey Water-Resources Investigations Report94 p. Orzol, L.L.,User's guide for MODTOOLS—Computer programs for translating data of MODFLOW and MODPATH into geographic information system files: U.S.
Simulation of Ground-Water Flow in the Basin-Fill Aquifer of the Tularosa Basin, South-Central New Mexico, Predevelopment through By G.F. Huff Abstract The hydrology of the basin-fill aquifer in the Tularosa Basin was evaluated through construction and calibration of steady-state and transient three-dimensional ground-water-flow simulations.
to feet of weakly cemented basin-fill deposits in the Tularosa area. These sedi-ments have a high hydraulic conductivity and are the primary aquifer in the basin. Using water-level measurements col-lected between andwe were able to determine zones where aquifers are recharging, being pumped, declining, or not changing.
Simulation of ground-water flow in the basin-fill aquifer of the Tularosa Basin, south-central New Mexico, predevelopment through USGS Scientific Investigations Report [Glenn F.
Huff] on *FREE* shipping on qualifying offers. The United States Geological Survey (USGS) is a scientific organization created inand is part of the U.S. : Glenn F. Huff. Water resources development -- New Mexico.
See also what's at your library, or elsewhere. Water resources in basin-fill deposits in the Tularosa Basin, New Mexico / (Albuquerque, N.M.: U.S. Dept. of the Interior, Water resources in New. The surface divide near the New Mexico/Texas State line separates the Tularosa Basin (a closed basin) and the Hueco Basin (a through-flowing basin) topographically.
The surface divide does not correspond to a structural or ground-water divide, and the two basins are connected by interbasin ground-water flow from New Mexico into Texas (Wilkins. James M. Barker, Barry S. Kues, George S.
Austin and Spencer G. Lucas, eds.,pages. The New Mexico Geological Society Fall Field Conference tours the south-central part of New Mexico after a year hiatus (Guidebook 15).Topics in this guidebook range from several papers on the Precambrian, both as basement rocks and exposures, to Pleistocene glaciation.
The Mimbres basin is a closed basin that occupies parts of Southwest New Mexico and Northwestern Chihuahua, Mexico. The lowest part of the basin was an ancient lake during the first days of men.
In there was still a very high water table in the vicinity of Deming New Mexico. At present, fossil fuel powered pumps are depleting theFile Size: 1MB. Basin-fill deposits function as the principal aquifers in the upper Humboldt River basin.
Over much of the basin lowlands, the upper feet of basin fill consists of clay, silt, sand, and gravel deposited in a lake of middle to late Pliocene age. Fine-grained lacustrine sediments compose from 30 to more than 70 percent of the deposits. Get this from a library.
Geology of the Sierra Blanca, Sacramento, and Capitan Ranges, New Mexico: New Mexico Geological Society Forty-second Annual Field Conference, October[James M Barker; New Mexico Geological Society.
Annual Field Conference]. Selected hydrologic data for the upper Rio Hondo Basin, Lincoln County, New Mexico - Simulation of ground-water flow in the basin-fill aquifer of the Tularosa Basin, south-central New Mexico - Precipitation, ground-water age, ground-water nitrate concentrations,and ground-water levels, in eastern Bernalillo County, New Mexico.
The floor of the northern Tularosa Basin between the Oscura Mountains and Alkali Flat consists of a southsloping gypsum-alluvial discharge plain with distal alluvial fans, stream valleys, springs and marshes, eolian blowouts, loess, and the Carrizozo Malpais lava flow.
Simulation of ground water flow in the basin fill aquifer of the Tularosa Basin south cental New Mexico Catalog Record - Electronic Resource Available Shipping list no.: P. Includes bibliographical references (p. Also available via the Internet at the U.S.
Geological Survey Publications Warehouse site. ENVIRONMENTAL TRACERS IN GROUNDWATER OF THE SALT BASIN, NEW MEXICO, AND IMPLICATIONS FOR WATER RESOURCES. SOPHIA CARMELITA SIGSTEDT. Master of Science in Hydrology.
New Me. Estancia Basin Resource Association. The Estancia Basin Resource Association (EBRA) is a grassroots organization dedicated to preservation of water resources within the. New Mexico Geological Society Guidebook, 55th Field Conference, Geology of the Taos Region,p.
CHEMICAL AND ISOTOPIC CONSTRAINTS ON SOURCE-WATERS AND CONNECTIVITY OF BASIN-FILL AQUIFERS. The New Mexico Bureau of Mines and Mineral Resources, University of New Mexico, New Mexico Geological Society and the Pecos River Commission have also contributed signifi- cant studies of the ground-water resources of New Mexico in terms of eight major areas: High Plains, Rio Grande Valley, Canadian and Cimarron River Basins, Pecos River Basin.
Thicker upper basin fill within the northwest basin indicates that the basin subsided more in the northwest than in the southeast during deposition of the upper basin fill. The two major faults that bound the Hueco graben on the west and southwest, the East Franklin Mountains fault and Amargosa fault, respectively, have had the most recent.
The basin fill deposits can be broadly divided into lower basin fill, upper basin fill, and surficial deposits (Fig. 2; Collins and Raney, ). The Pliocene–Pleistocene Fort Hancock and Camp Rice Formations (Strain, ) represent the upper part of the upper basin : Pawan Budhathoki, Diane I.
Doser, Anita Thapalia, Richard P. Langford, Victor M. Avila. The Sacramento Mountains of south-central New Mexico include a broad area of forested, well-watered terrain, the source of perennial streams flowing east toward the Roswell Basin and the Pecos River and of intermittent streams flowing west into the Tularosa -development and recent water level data indicate groundwater movement from Tularosa Valley to the Cited by: In the Mesilla Basin in southern New Mexico, we identified zones of mixing between recharging irrigation water with groundwater within the depth range of ~ 50– m below the ground surface.
Chemical and isotopic data were obtained from ground water and surface water throughout the Middle Rio Grande Basin (MRGB), New Mexico, and supplemented with selected data from the U.S. Geological.
The area trends north-south along the east side of Tularosa-Hueco Bolson astride the Texas-New Mexico border approximately 40 km northeast of El Paso. Because of its proximity to El Paso, geothermal water in the Hueco Tanks area could be a significant resource.
Hueco Bolson is an asymmetric graben. A new USGS study investigates how concentrations of arsenic in three drinking-water supply wells change at daily, seasonal, and yearly time scales. Arsenic variability and related factors identified have potential implications for human health.
Arsenic is a naturally occurring element, but long-term exposure can cause cancer in people. Six samples of spring water from the northern side of the Tularosa Basin (Fig. 2A) were provided by Bruce Allen from the New Mexico Bureau of Geology and Mineral Resources; these spring waters were sampled in February of and stored at room temperature until August of Cited by: The Laguna El Fresnal, located in the state of Chihuahua, northern Mexico (), occupies an apparently level valley with a surface area of about 50 km 2 with a mean elevation of m above sea level (m a.s.l.).It is bounded by mountain ranges: the Sierra El Fresnal to the west and the Sierra Los Borregos and Cerro El Venado to the by: 5.
Full text of "Alamogordo regional water supply project: final environmental impact statement" See other formats. EPA/// December IDENTIFICATION OF SOURCES OF GROUND-WATER SALINIZATION USING GEOCHEMICAL TECHNIQUES by Bernd C.
Richter and Charles W. Kreitler Bureau of Economic Geology The University of Texas at Austin Austin, Texas Cooperative Agreement No. CR Project Officer Bert E. Bledsoe Extramural Activities.
Oliver Lee Memorial State Park is a state park of New Mexico, United States, whose two tracts preserve a canyon in the Sacramento Mountains and Oliver Lee's historic 19th-century ranch house. The acre ( ha) park is located in Otero County at an elevation of 4, feet (1, m).
It is situated at the base of Dog Canyon and provides opportunities for camping, hiking, Location: Otero County, New Mexico, United States.
Existing Interpretations of Colorado and New Mexico Volcanism. Cenozoic volcanism in Colorado and New Mexico is extensive and fairly continuous, and volcanism may not necessarily be an indicator of rift activity (Corti et al., ), thus using the history of volcanism to deduce the onset of rifting is challenging.
Rather than using the Author: Alyssa L. Abbey, Alyssa L. Abbey, Nathan A. Niemi. Full text of "Alamogordo regional water supply project: draft environmental impact statement" See other formats. USGS National Water Census Water Budget Data Resources for the Upper Gila - HUC (Turn off compatibility view settings in IE if having problems viewing this site) EPA - Watershed Assessment, Tracking and Environmental Results (WATERS) for the Upper Gila - HUC cross cut by basin-forming normal faults.
Although the area is structurally complex, no faults have been mapped cutting basin-fill sediments in the Bingham Cienega area. Unexposed faults may exist in the underlying basement rocks. Generalized depth-to-bedrock contours suggest that the bedrock surface below the valley-fill.
en, Socorro, New Mexico; New Mex-ico Museum of Natural History and Science, Albuquerque, New Mexico. Why we live where we live: the im-pact of karstic water resources on settlement patterns in southeastern New Mexico.
An introductory earth science course at New Mexico State University-Carlsbad. Veni also organized or co-File Size: 8MB. Book reviews Book reviews This book is intended for the practicing geologist who has had no previous contact with statistics and indeed, only an elementary knowledge of mathematics.
The book has 10 chapters with the following headings: (1) words numbers and pictures, (2) coin tossing and stratigraphy, (3) one and two sample testing, (4) nominal scale.
New Mexico and exits the basin in Texas at the south end of the Franklin Mountains. The low land along the river is known as the Mesilla Valley (U.S. Army ). The aquifer in the Mesilla Bolson has been subdivided into four fresh water zones.
resources upon water quality and effects on the environment because both were key policy priority areas. Whereas the Seattle proj ect viewed ASR by itself, the Portland approach is more holistic. It regarded ASR as another option for its water supply needs.
Any new decision framework should include metrics that allow comparisons of ASR to. The climate in the American southwest would have been colder and drier than present (COHMAP Project Members ).
During full glacial conditions at Chaco Canyon in the San Juan Basin, New Mexico, ponderosa pine, limber pine, and spruce populations expanded and were located in lower altitudinal zones than today (Hall ). Multisource geological data mining and its utilization of uranium resources exploration.
NASA Astrophysics Data System (ADS) Zhang, Jie-lin. Nuclear energy as one of clear energy sources takes important role in economic development in CHINA, and according to the national long term development strategy, many more nuclear powers will be .1 Chapter 7 The Mesilla Basin Aquifer System of New Mexico, West Texas, and Chihuahua An Overview of Its Hydrogeologic Framework and Related Aspects of Groundwater Flow and Chemistry Introduction John W.
Hawley 1, John F. Kennedy 1, and Bobby J. Creel 1 Our brief overview of the hydrogeology and geohydrology of basin-fill aquifers in the Mesilla Basin .