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4 edition of Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon found in the catalog.

Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon

Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon

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Published by U.S. Dept. of the Interior, U.S. Geological Survey, Books and Open-File Reports Section [distributor] in Boise, Idaho, Denver, CO .
Written in English

    Subjects:
  • Aquifers -- Snake River Plain (Idaho and Or.),
  • Snake River Plain (Idaho and Or.)

  • Edition Notes

    Statementby G.F. Lindholm
    SeriesU.S. Geological Survey open-file report -- 91-98
    ContributionsGeological Survey (U.S.)
    The Physical Object
    FormatMicroform
    Paginationv, 62 p.
    Number of Pages62
    ID Numbers
    Open LibraryOL13616955M
    OCLC/WorldCa30698873

    Add to Book Bag Remove from Book Bag. Saved in: Multilevel groundwater monitoring of hydraulic head and temperature in the Eastern Snake River Plain Aquifer, Idaho National Laboratory, Idaho, / by: Twining, Brian V. Published: () Iodine in the Snake River Plain Aquifer at and near the Idaho National Laboratory, Idaho, Geohydrologic framework of the Snake River Plain regional aquifer system, Idaho and eastern Oregon / by: Whitehead, R. L., Published: () Hydrogeology of the southeastern coastal plain aquifer system in Mississippi, Alabama, Georgia, and South Carolina / by: Renken, Robert A., Published: ().


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Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon Download PDF EPUB FB2

Summary of the Snake River plain Regional Aquifer-System Analysis in Idaho and eastern Oregon Professional Paper A By: G.F. Lindholm. Summary of the Snake River Plain Regional Aquifer-System Analysis in Idaho and Eastern Oregon on *FREE* shipping on qualifying offers. Summary of the Snake River Plain Regional Aquifer-System Analysis in Idaho and Eastern OregonManufacturer: ment Printing Office.

Summary of the Snake River Plain Regional Aquifer-System Analysis in Idaho and Eastern Oregon (Regional Aquifer-System Analysis--Snake River Plain, Idaho) [Gerald F.

Lindholm] on *FREE* shipping on qualifying : Gerald F. Lindholm. Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon (SuDoc I ) [Gerald F. Lindholm] on *FREE* shipping on qualifying : Gerald F. Lindholm.

Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon (OCoLC) Material Type: Government publication, National government publication, Internet resource: Document Type: Book, Internet Resource: All Authors / Contributors: Gerald F Lindholm.

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Items of recharge to and discharge from the Snake River Plain regional aquifer are shown in figure 3. Ground water in the eastern part of the plain is chiefly of the calcium magnesium bicarbonate type, with moderate amounts of sodium and sulfate, and is suitable for most uses (Mundorff and others,p.

Cited by: 4. Eastern Snake Plain Aquifer Overview. The Eastern Snake Plain Aquifer (ESPA) is located in southeastern Idaho. It is Idaho’s largest aquifer system, and one of the largest in the United States. The aquifer is composed primarily of basalts and covers approximat square miles.

Eastern Snake River Plain Aquifer Physical Characteristics. The aquifer beneath the eastern Snake River Plain covers an area of approximat square kilometers.

The Eastern Snake River Plain Aquifer (ESRA) system is an extensive and regionally significant source of groundwater in southeast Idaho, as well as a major contributing source of flow to the Snake River.

The ESRA is highly productive and regional groundwater flow is generally from east to west. Check out the Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon.

Map published by the U.S. Geological Survey National Geologic Map Database Product Description Page. General Information. Title: Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon; Author(s. Summary of the Snake River Plain regional Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon book analysis in Idaho and eastern Oregon (DLC) (OCoLC) Material Type: Document, Government publication, National government publication, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: Gerald F Lindholm; Geological Survey (U.S.).

Lindholm, G.F.,Summary of the Snake River plain Regional Aquifer-System Analysis in Idaho and eastern Oregon: U.S. Geological Survey Open-File Report62 p. Superceded by PP A. Lindholm, G.F.,Summary of the Snake River plain Regional Aquifer-System Analysis in.

Zektser et al. () used a Point Count System (PCS) to study the impact of pollution on Snake River aquifer system in eastern Idaho, United States. In this approach also the influence of each. square-mile Snake River Plain is largely in southern Idaho and includes one of the Nation 's major regional aquifers.

A comprehensive investigation of the area 's ground-water resources will be made as part of the U.S. Geological Survey 's Regional Aquifer-System Analysis (RASA) program. The Snake River Plain Aquifer in Eastern Idaho is the largest aquifer in Idaho, and one of the largest and most productive aquifers in the world.

The crystal-clear water of the Snake River Plain Aquifer is also the only source of drinking water for nearlyresidents of Eastern Size: 3MB. The regional aquifer system of the eastern Snake River Plain (hereafter referred to as the aquifer) (fig. 1) is an important component of the hydrologic system in eastern Idaho.

The aquifer was thought to be the largest unified ground-water reservoir on the North American continent (Nace,p. ) but is probably second to theCited by: 5. Lindholm, G.F.,Summary of the Snake River Plain Regional Aquifer Systems Analysis in Idaho and eastern Oregon: U.S. Geological Survey Open File ReportBoise, ID., 62 p.

Newton, G.D.,Application of a simulation model to the Snake plain aquifer: University of Idaho. Buy Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon (SuDoc I ) by Gerald F.

Lindholm (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Gerald F. Lindholm. The Snake River Plain regional aquifer system underlies a large, crescent-shaped lowland that extends from near the western boundary of Yellowstone National Park in eastern Idaho to the Idaho-Oregon border where the Snake River enters Hells Canyon.

The northern and southern boundaries of the Snake River Plain generally coincide with the contact between unconsolidated deposits or Pliocene and.

The western Snake River Plain is a Neogene-aged intracontinental rift basin, about 70 km wide and km long, trending northwest across the southern Idaho batholith. Its southeastern end merges with the northeast-trending eastern plain, a structural downwarp associated with extension along the track of the Yellowstone hot spot.

Aquifers - Snake River Plain (Idaho and Or.) Water use on the Snake River Plain, Idaho and eastern Oregon / by S.A. Goodell ; a contribution of the Regional Aquifer-System Analysis Program - Details. Buy Summary of the Snake River Plain regional aquifer-system analysis in Idaho and eastern Oregon (SuDoc I A) by Gerald F.

Lindholm (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Gerald F. Lindholm.

Get this from a library. Plan of study for the regional aquifer-system analysis of the Snake River plain, Idaho and eastern Oregon. [Gerald F Lindholm; Geological Survey (U.S.)]. Book: Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon.

Up to 90% off Textbooks at Amazon Canada. Plus, free two-day shipping for six months when you sign up for Amazon Prime for : Gerald F.

Lindholm. Buy Summary of the Snake River Plain Regional Aquifer-System Analysis in Idaho and Eastern Oregon (Regional Aquifer-System Analysis--Snake River Plain) by Gerald F.

Lindholm (ISBN: ) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Gerald F. Lindholm. The regional aquifer system of the eastern Snake River Plain is an important component of the hydrologic system in eastern Idaho.

The aquifer was thought to be the largest unified ground-water reservoir on the North American continent but is probably second to the Floridian aquifer in the southeastern United States. Flow in the aquifer is from major recharge areas in the northeastern part Cited by: 5.

Eastern Snake River Plain Aquifer. The Eastern Snake River Plain Aquifer north of the Snake River is a remarkable aquifer of great resource and economic significance. It is not a single homogeneous geologic formation.

Rather it consists of a volcanic pile of the Quaternary Snake River Group basalts. In eastern Idaho, these basalts may be about 1 mile ( km) thick. The individual flows are 20–30 feet (6–9 m) Australia: Gnangara Mound, Great Artesian. The Eastern Snake River Plain Aquifer was designated a sole source aquifer in It provides the sole source of drinking water for nearlypeople in southeastern and south central Idaho.

The aquifer stretches across much of south central Idaho and is Idaho's largest basalt aquifer, covering an area of approximat square miles.

Table 5. Summary of streamflow at two streamflow-gaging stations on the Big Lost River, Idaho. Table 6. Ground-water budget for the conceptual model area for and derived from the Regional Aquifer System Analysis (RASA) model of the Snake River Plain aquifer, Idaho.

This report is available online in Portable Document Format (PDF). Parameter-Estimation Technique to Modeling the Regional Aquifer Underlying the Eastern Snake River Plain, Idaho By S. GARABEDIAN A contribution of the Regional Aquifer-System Analysis Program U.S.

GEOLOGICAL SURVEY WATER-SUPPLY PAPER DEPARTMENT OF THE INTERIORCited by: Buy Plan of study for the regional aquifer-system analysis of the Snake River Plain, Idaho and eastern Oregon (Open-file report / United States Department of the Interior, Geological Survey) by Gerald F Lindholm (ISBN:) from Amazon's Book Store.

Author: Gerald F Lindholm. Get this from a library. Geohydrologic framework of the Snake River Plain regional aquifer system, Idaho and eastern Oregon. [R L Whitehead; Geological Survey (U.S.),]. aquifer is defined in the report, Hydrology and Digital Simulation of the Regional Aquifer System, Eastern Snake River Plain, Idaho, USGS Professional Paper F, excluding areas south of the Snake River and west of the line separating Sections 34 Township 10 South, Range 20 East, Boise Meridian.” This report was one of a.

Turning north at Ontario, the river follows the Idaho-Oregon line through mile-deep Hells Canyon and then past Idaho’s barge port at Lewiston to Pasco, Washington, where it joins the Columbia.

Flowing 1, miles from source to mouth, the Snake is the nation’s thirteenth longest river and the largest tributary to the Columbia. Water sampling and analysis summary: groundwater chemical evolution and flow patterns in the eastern Snake River Plain Aquifer, Idaho.

Geohgical Society of America () Solute Geochemistry of the Snake River Plain Regional Aquifer System, Idaho and Eastern Oregon. Available from Boolu and Open File Report Section CO USGS Open.

Summary of the Snake River Plain Regional Aquifer-System Analysis in Idaho and Eastern Oregon: Gerald F. Lindholm: Books - or: Gerald F. Lindholm. The Snake River is a major river of the greater Pacific Northwest region in the United States. At 1, miles (1, km) long, it is the largest tributary of the Columbia River, in turn the largest North American river that empties into the Pacific Ocean.

The Snake River rises in western Wyoming, then flows through the Snake River Plain of southern Idaho, the rugged Hells Canyon on the Oregon. Geohydrologic framework of the Snake River plain regional aquifer system, Idaho and eastern Oregon,Professional Paper B Geohydrology and water resources of alluvial basins in south-central Arizona and parts of adjacent states,Professional Paper B.

Spinazola JM () Geohydrology and simulation of flow and water levels in the aquifer system in the Mud Lake area of the eastern Snake River Plain, eastern Idaho. U.S. Geological Survey Water-Resources Investigations Report Cited by: 7.Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon () Paper version: In stock and available from the USGS Store; Download citation as: RIS | .References on Idaho Geology Geohydrologic Framework of the Snake River Plain, Idaho and Eastern Oregon, U.S.

Geological Survey Hydrologic Investigations Map HA, scaleGeohydrologic Framework of the Snake River Plain Regional Aquifer System, Idaho and Eastern Oregon, U.S.

Geological Survey Professional Paper B, 32 p.