Reconnaissance stream-sediment geochemistry of Death Valley National Monument, California

Cover of: Reconnaissance stream-sediment geochemistry of Death Valley National Monument, California |

Published by U.S. Geological Survey in Denver, CO .

Written in English

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Subjects:

  • River sediments -- Death Valley National Monument (Calif. and Nev.),
  • Geochemistry -- Death Valley National Monument (Calif. and Nev.)

Edition Notes

Book details

Other titlesReconnaissance stream sediment geochemistry of Death Valley National Monument, California.
Statementby A.H. Hofstra ... [et al.].
SeriesOpen-file report -- 93-698., U.S. Geological Survey open-file report -- 93-698.
ContributionsHofstra, Albert H., Geological Survey (U.S.)
The Physical Object
Pagination14, A88 leaves :
Number of Pages88
ID Numbers
Open LibraryOL17105127M
OCLC/WorldCa32035466

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Get this from a library. Reconnaissance stream-sediment geochemistry of Death Valley National Monument, California. [Albert H Hofstra; Geological Survey (U.S.);]. A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California (USGS Water Supply Paper Y) (*) Effect of ground-water developmenmt on the pool level in Devil's Hole, Death Valley National Monument, Nye County, Nevada (USGS Open-File Report ) (*).

Reconnaissance stream-sediment geochemistry of Death Valley National Monument, California Open-File Report By: Albert H. Hofstra, D.L. Fey, J.M. Motooka. geochemical survey of Death Valley National Monument, excluding the part in Nevada, was conducted in September of The major features of Death Valley are shown on a shaded relief map (Figure 2) from Chalfant ().

The Monument covers a large part of theAuthor: Albert H. Hofstra, D.L. Fey, J.M. Motooka, B.H. Roushey, Lee-Ann Bradley. Reconnaissance Stream-Sediment by A.H. Hofstra, D.L. boundary Streams Elevations above and below sea level Geochemistry of Death Valley National Monument, California Fey, J.M.

Motooka, Bal-I. Roushey, SCALE 10 10 KILOMETRES and L.A. Bradley MILES DEATH VALLEY NATIONAL MONUMENT Stream Sediment Sample Sites. Field and laboratory California book are presented for sediment samples from the Goldfield Quadrangle, California; Nevada. The samples were collected by Savannah River Laboratory; laboratory analysis and data reporting were performed by the Uranium Resource Evaluation Project at Oak Ridge, Tennessee.

A Brief Geologic and Hydrologic Reconnaissance of the Furnace Creek Wash Area, Death Valley National Monument California By M. PISTRANG and FRED KUNKEL CONTRIBUTIONS TO THE HYDROLOGY OF THE UNITED STATES GEOLOGICAL SURVEY WATER-SUPPLY PAPER Y Prepared in cooperation with the National Park Service, Department of the InteriorCited by: 9.

A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California() The Publications California book does not have links to digital versions of this publication at this time.

Regional-scale variations in soil geochemistry were investigated in a 20,km 2 study area in northern California that includes the western slope of the Sierra Nevada, the southern Sacramento Valley and the northern Coast Ranges.

Over archival soil samples collected from the late s to in El Dorado, Placer, Sutter, Sacramento, Yolo and Solano counties were analyzed for 42 Cited by: Published Soil Surveys for California.

Current, official soil survey information is on the Web Soil Survey. The Web Soil Survey allows you to create custom reports by selecting a specific area of interest. In the table below, clicking on a survey area that is listed as "current" takes you to the Web Soil Survey.

A regional gravity survey of the state of Baja California shows the peninsula to be generally in isostatic adjustment. The Bouguer anomaly map reveals a gravity high that extends down the west coast from the Agua Blanca fault to at least lat 28° N.

If we consider the geologic formations that make up the national parks (N.P.), national monuments (N.M.) (excluding small historical or archaeological ones), Monument Valley, San Rafael Swell, and Glen Canyon National Recreation Area, all in the Colorado Plateau, it becomes apparent that certain formations or groups of formations play starring.

koenig, g. / the lost death valley ‘49er journal of louis nusbaumer, death valley,cl, 80 pages, - 2 - $ 69 koeppel, e. / the california gold country, highway 49 revisited, being an account of the life and times of the people and mining camps of the california gold rush,pb, pages, - 1 - $ PINTO BASIN, JOSHUA TREE NATIONAL MONUMENT, RIVERSIDE COUNTY, CALIFORNIA By FBED KUNKEL ABSTRACT Pinto basin, in the north-central part of Riverside County, Calif., is a typical desert valley formed by downfaulting along several major fault zones.

The valley is filled with alluvium, and ground water in the alluvium discharges asCited by: 4. Hydrogeochemical and Stream Sediment Reconnaissance Basic Data Report for Las Vegas NTMS Quadrangle, Arizona, California, and Nevada One of 3, reports in the series: Atomic Energy Commission Reports available on this : B.

Qualheim. Hydrogeochemical and Stream Sediment Reconnaissance Basic Data Report for Las Vegas NTMS Quadrangle, Arizona, California, and Nevada: Data Tables One of 3, datasets in the series: Atomic Energy Commission Reports available on this : B.

Qualheim. A broad west-to-east increase of many metal concentrations has been found in stream sediments during a reconnaissance investigation conducted in conjunction with geologic studies in the Santa Renia Fields and Beaver Peak 7–1/2 minute quadrangles near the northern end of the Carlin trend of gold deposits in the Tuscarora Mountains.

This regional increase in metal concentrations coincides with. National Uranium Resource Evaluation Program Title: Supplement to hydrogeochemical and stream-sediment reconnaissance basic data reports K/UR.

Mines and mineral deposits in Death Valley National Monument, California (Special report - California Division of Mines and Geology ; ) [Evans, James R] on *FREE* shipping on qualifying offers. Mines and mineral deposits in Death Valley National Monument, California (Special report - California Division of Mines and Geology ; )Author: James R Evans.

Glacial Reconnaissance of Sequoia National Park California SELECTED REFERENCES Alden, W. C.,Physiography and glacial geology of eastern Montana and adjacent areas: U.S. Geol. Survey Prof. Paperp. Isotopic and mineralogic data from an m thick section of the Great Valley sequence, northern California, indicate that changes in the δ 18 O values of authigenic minerals resulted from the conversion of smectite to a 10 Å clay-mineral as temperature increased with burial in the Jurassic- Cretaceous outer-arc basin.

The clay-mineral assemblage in mudstone is characterized by a Cited by: Survey made a geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity (fig.

In July R. Dale made a brief survey of the area and proposed a test site for a "water well near Captain Jack's Stronghold at the northern boundary of the national monument.

In October ^ C. Berkstresser supervised drilling,Cited by: 4. Hydrogeochemical and stream sediment reconnaissance: National Uranium Resource Evaluation program. Savannah River Laboratory semi-annual report, October March Savannah River Laboratory semi-annual report, October March Pinto basin, in the north-central part of Riverside County, Calif., is a typical desert valley formed by downfaulting along several major fault zones.

The valley is filled with alluvium, and ground water in the alluvium discharges as subsurface outflow through an alluvium-filled gap at the east end of the valley. Occasionally surface water from cloudburst floods also discharges in a wash.

Technical Report: Hydrogeochemical and stream-sediment reconnaissance basic data for Boise Quadrangle, Oregon; Idaho. Uranium Resource Evaluation Project. Mines and mineral deposits in Death Valley National Monument, California Item Preview remove-circle some content may be lost due to the binding of the book.

Addeddate Call number TN24 C3 A33 No Camera Canon EOS 5D Mark II External-identifierPages: Savannah River Laboratory hydrogeochemical and stream sediment reconnaissance.

Raw data release II. Orientation studies in Alabama. National Uranium Resource Evaluation Program. [National Uranium Resource Evaluation Program]. Lava Beds National Monument is on the Modoc Plateau in Modoc and Siskiyou Counties.

The principal geologic units in the vicinity are volcanic rocks, which in places are highly permeable and poorly permeable lake sedimentary deposits, all probably post-Oligocene in age. Yields and specific capacities of wells in the unconfined water body within volcanic rocks and lake deposits range widely, but.

As part of a general hydrologic study by the National Park Service, J. Lewis prepared a map, showing the extent of alluvial deposits and the locations of wells and springs (written communication, ), and a report discussing the water resources of Joshua Tree National Monument and vicinity (written communication, ).

The San Joaquin Basin is one of the largest of the many basins on the west slope of the Sierra Nevada, whose rivers drain into the Great Valley of California (fig.

It lies immediately southeast of the scenic central part of the range, which is mostly in Yosemite National Park. Books by Language Additional Collections Journal of materials engineering.

Journal of paediatric dentistry. Ryan, Pahrump, and Stewart Valley minute quadrangles and High Peak minute quadrangle, Inyo County, California" See other formats.

mf [miscellaneous field] maps # - (part 4) mf b / mineral resource potential map of the roadless areas and the santa lucia wilderness in the los padres national forest, southwestern california, $ 10 mf / reconnaissance surficial geologic map of northern death valley, nevada, $ Kersten M, Forstner U.

Speciation of trace elements in sediments. In: Balley GE, editor. Trace element speciation: analytical methods and problems. Florida: CRC Press, Kreamer DK, Hodge VF, Rabinowitz I, Johannesson KH, Stetzenbach KJ. Trace element geochemistry in water from selected springs in Death Valley National Park, by: Reconnaissance soil geochemistry at the Riverton Uranium Mill Tailings Remedial Action Site, Fremont County, Wyoming Article (PDF Available) January with 35 Reads How we measure 'reads'.

A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California Add to Downloads U.S. Geological Survey (USGS) | July 1, The δ 34 S values of two dominant xerophytes, Atriplex hymenehytra and Larrea tridentata, in Death Valley, California, vary similarly from +7 to +18‰, corresponding isotopically to sulfate in the water supplies at a given radially outwards, tree ring data from a phreatophyte tree, Tamarix aphylla, show a distinct time dependence, with δ 34 S values increasing from + to Cited by: Owens Valley Hydrogeology.

Welcome to the U.S. Geological Survey (USGS) Owens Valley Hydrogeology website. Reconnaissance of the borax deposits of Death Valley and Mojave Desert: U.S.

Geological Survey Bulletin23 p. Death Valley National Monument, California: U.S. Geological Survey Water-Supply Paper Y, 35 p. ii Groundwater Geology and Hydrology of Death Valley National Park, California and Nevada NPS /, December The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the.

Book/Textbook (1) Bulletin (2) Conference proceedings (1) Guidance Document (1) Journal Article (2) Model (13) Report (30) Research Article (1) Science Panel Report (1) Technical Report (2) Topic.

Agriculture (1) Basic Information (1) Ecosystem & Species Mgt (4) Fisheries (1) Flood Management (1) Geohydrology (1) Groundwater. Department of Geosciences The University of Arizona Theses and Dissertations completed after Spring, Latta, John Stephen, IV Geochemistry and petrology of the ash flows of Chiricahua National Monument, Arizona, and their relation to the Turkey Creek caldera M.S.

Death Valley, California M.S. 30p. Interbasin flow (ground-water flow between ground-water basins through bedrock mountain ranges) in the Great Basin has been established by scientific studies during the past century (Eakin,Winograd and Thordarson,Harrill et al., ).Interbasin flow, though it does not occur uniformly between all basins, occurs commonly and is a function of the hydraulic gradient between basins Cited by: Audio Books & Poetry Community Audio Computers & Technology Music, Arts & Culture News & Public Affairs Non-English Audio Spirituality & Religion.

Librivox Free Audiobook. Podcasts. Featured software All software latest This Just In Old School Emulation MS-DOS Games Historical Software Classic PC Games Software Library.Maps derived from a subset of the National Uranium Resource Evaluation Hydrogeochemical and Stream Sediment Reconnaissance data.

Samples are from streams, lakes, ponds, springs, playas, and soils. Includes Na, Ti, Fe, Cu, Zn, As, Ce, Hf, Pb, Th, and U. Info: Geochemistry of soils in the US from the RASS database.

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