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Monday, April 27, 2020 | History

3 edition of Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, 1984 found in the catalog.

Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, 1984

Denzel R. Cline

Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, 1984

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Published by Dept. of the Interior, U.S. Geological Survey, Books and Open-File Reports [distributor] in Tacoma, Wash, Denver, Colo .
Written in English

    Subjects:
  • Groundwater -- Columbia Plateau,
  • Groundwater -- Washington (State),
  • Water-supply -- Columbia Plateau,
  • Water-supply -- Washington (State)

  • Edition Notes

    Other titlesGround water pumpage from the Columbia Plateau regional aquifer system, Washington, 1984
    Statementby D.R. Cline and M.E. Knadle ; prepared in cooperation with the State of Washington Department of Ecology
    SeriesWater-resources investigations report -- 87-4135, A contribution of the Regional Aquifer-System Analysis Program, Contribution of the Regional Aquifer System Analysis Program
    ContributionsKnadle, M. E, Washington (State). Dept. of Ecology, Geological Survey (U.S.)
    The Physical Object
    Pagination1 envelope (1 v., 1 map) :
    ID Numbers
    Open LibraryOL13613113M

    The Columbia Plateau Regional Aquifer System (CPRAS) covers ab square miles of southeastern Washington, northeastern Oregon, and western Idaho. The area supports a $6-billion per year agricultural industry, leading the Nation in production of apples, hops, and eight other commodities. Ground water is the sole source of water supply for more than 3 million people on Long Island, New York. Large-scale ground-water pumpage, sewering systems, and prolonged periods of below-normal precipitation have lowered ground-water levels and decreased stream-discharge in western and central Long Island. No method is currently ( The Hydrogeologic framework and geochemistry of the Columbia Plateau aquifer system, Washington, Oregon, and Idaho by K. J Whiteman (Book) 10 editions published in in English and held by WorldCat member libraries worldwide. Columbia Plateau Basalt Regional Aquifer-System Study The Columbia Plateau Basalt regional aquifer system study was started in and is scheduled for completion in The study was designed to address some of the hydrologic problems currently being encountered on the plateau.


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Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, 1984 by Denzel R. Cline Download PDF EPUB FB2

GROUND-WATER PUMPAGE FROM THE COLUMBIA PLATEAU REGIONAL AQUIFER SYSTEM, WASHINGTON, By D. Cline and M. Knadle ABSTRACT An inventory of ground-water pumpage from large- capacity wells on the Columbia Plateau in eastern Washington was started in in Ground-water pumpage from the Columbia Plateau regional aquifer system with a regional aquifer study of the by: 3.

Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, [Cline, Denzel R.] on *FREE* shipping on qualifying offers. Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, Author: Denzel R.

Cline. Ground-water pumpage from the Columbia Plateau Regional Aquifer System, Oregon, (SuDoc I /) [C. Collins] on *FREE* shipping on qualifying : C. Collins. Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, Water-Resources Investigations Report By: D.R.

Cline and M.E. Washington by: 3. Groundwater pumpage was estimated for for an area of Ground-water pumpage from the Columbia Plateau regional aquifer system 8, sq mi in north-central Oregon. Pumpage data were collected from irrigation, industrial and public supply users and analyzed as part of the Columbia Plateau Regional Aquifer System Analysis (RASA) study.

Groundwater is pumped from Tertiary basalts and interflow material of the Columbia River. GROUND-WATER Ground-water pumpage from the Columbia Plateau regional aquifer system FROM THE COLUMBIA PLATEAU REGIONAL AQUIFER SYSTEM, OREGON, By C.

Collins ABSTRACT Ground-water pumpage was estimated for for Ground-water pumpage from the Columbia Plateau regional aquifer system area of about 8, square miles in north-central Oregon.

Pumpage data were collected from irrigation, industrial and public 1984 book users and analyzed as part of the Columbia Plateau Regional Aquifer System Cited by: 8. pumpage from the Columbia Plateau regional aquifer system, Washington, U.S. Geological Survey Water-Resources Investigations Report ,32 p, 1 sheet.

Collins, C.A.,Ground-water pumpage from the Columbia Plateau regional aquifer system, Oregon, U.S. Geological Survey Water-Resources Investigations Report ,21 : R.J. Wagner, R.C. Lane. Ground-water pumpage from the Columbia Plateau regional aquifer system Plateau Regional Aquifer System, Washington, U.S.

Geological Survey Water-Resources Investigations Reportin press. Collins, C.A.,Ground-water Ground-water pumpage from the Columbia Plateau regional aquifer system from the Columbia Plateau RegionalAuthor: R.C.

Lane. Ground-water flow simulation of the Columbia Plateau regional aquifer system, Washington, Oregon, and Idaho Water-Resources Investigations Report By: A.J. Hansen Jr., J.J. Vaccaro, and H.H. Bauer. Maps showing average ground-water pumpage in the Columbia Plateau aquifer system, Washington, Oregon, and Idaho.

Maps showing the mean annual precipitation and estimates of recharge for the Columbia Plateau aquifer system, Washington, Oregon, and Cited by: Get this from a library.

Ground-water pumpage from the Columbia Plateau, Washington and Oregon, to [Denzel R Cline; C A Collins; Washington (State). Department of Ecology.; Geological Survey (U.S.)]. Get this from a library. Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, [Denzel R Cline; M E Knadle; Washington (State).

Department of Ecology.; Geological Survey (U.S.)]. Buy Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, (SuDoc I /) by Denzel R. Cline (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Denzel R. Cline. Well information and groundwater-level measurements for the 1984 book Plateau Regional Aquifer System in Washington, Oregon, and Idaho, were compiled from data provided by the U.S.

Geological Survey and seven other organizations. From the full set of ab wells andwater-level measurements a subset of wells within the aquifers of the Columbia. Problem: The Columbia River Basin in Washington, Oregon, and Idaho supports a $5 billion/year agricultural industry, leading the nation in production of apples and nine other water availability in the Columbia River basalts and the basin-fill sediments of the Columbia Plateau Regional Aquifer System (CPRAS) is a critical water-resource.

Additional Physical Format: Online version: Collins, C.A. (Charles Alexander), Ground-water pumpage from the Columbia Plateau Regional Aquifer System, Oregon, Two equations were developed by Nelson () using data for a year period () as part of the Columbia Plateau regional aquifer system analysis (Vaccaro, ).

These two equations use. Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, / by D.R. Cline and M.E. Knadle ; prepared in cooperation with the State of Washington Department of : Denzel R.

Cline. Ground-water pumpage from the Columbia Plateau regional aquifer system, Washington, Water-Resources Investigations Report Estimates of ground-water recharge to the Columbia Plateau regional aquifer system, Washington, Oregon, and Idaho, for predevelopment and current land-use conditions,Water-Resources.

After entering an aquifer, water moves slowly toward lower lying places and eventually is discharged from the aquifer from springs, seeps into streams, or is withdrawn from the ground by wells.

Groundwater in aquifers between layers of poorly permeable rock, such as clay or shale, may be confined under pressure. If such a confined aquifer is. The Edwards-Trinity (Plateau) and the Trinity Aquifers are designated as major aquifers in the state of Texas.

Located in west-central Texas (), these two aquifers provide the primary source of water for the Edwards Plateau and the Hill Country regions of Edwards-Trinity (Plateau) Aquifer extends over an area of ~91, km 2 beneath all or parts.

The Odessa aquifers are part of the regional Columbia Basin basalt aquifer system. Map: Columbia Plateau regional aquifer system -- a large approximately circular basalt system underlain primarily by Miocene basaltic rocks.

Ground-water levels and pumpage in east-central Washington, including the Odessa-Lind Area, The Columbia Plateau Aquifer system is a series of layered aquifers across ~44, mi 2 of Washington, Oregon, and Idaho. The aquifer system is on the Columbia Plateau, contained within the Cascades, Rocky Mountains, Okanogan Highlands, and the Blue Mountains.

These aquifers are bounded on the bottom by a layer of Miocene basaltic rock that can be up to. Ground-water flow simulation of the Columbia Plateau regional aquifer system, ().

Ground-water Pumpage in the Willamette Lowland Regional Aquifer System. Cline, D.R., and Collins, C.A.,Groundwater-water pumpage from the Columbia Plateau regional aquifer system, Washington and Oregon, for selected years during the period U.S. Geological Survey Water-Resources Investigations Report31 p.

These data delineate the areal extent of the Columbia Plateau aquifer system as defined in the 'Ground Water Atlas of the United States' (U.S.

Geological Survey HA ). The scale of source material isand these data are not intended for use at a larger scale. The Columbia Plateau is a geologic and geographic region that lies across parts of the U.S.

states of Washington, Oregon, and Idaho. It is a wide flood basalt plateau between the Cascade Range and the Rocky Mountains, cut through by the Columbia River. Groundwater conditions during and changes in groundwater levels from toColumbia Plateau Regional Aquifer System, Washington, Oregon, and Idaho: U.S.

Geological Survey Scientific Investigations Report12 p. Digital simulation of ground-water flow in the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: regional aquifer-system analysis / (Washington: U.S.

G.P.O. ; Denver, CO: For sale by the Branch of Distribution, Books and Open-File Reports Section, U.S. Geological Survey, Background Study of the Groundwater in the District of Columbia Assessment of the Groundwater in the District of Columbia Submitted To The Water Hygiene Division D.C.

Department of Consumer and Regulatory Affairs Washington, D.C. BY The DC Water Resources Research Center University of the District of Columbia Washington, D.C. May File Size: 3MB. Groundwater from square mile Columbia Plateau Regional Aquifer System has declined since the s, but is a vital resource for nearly million people in Idaho, Oregon and Washington, as well as supplementing irrigation water for the region’s estimated $6 billion annual agricultural industry.

The data files listed below are supplemental to the USGS Scientific Investigations Report titled 'Three-dimensional model of the geologic framework for the Columbia Plateau Regional Aquifer System, Idaho, Oregon, and Washington.' The report includes a description of methods used to derive the data.

Locally the Odessa Aquifers discharge to Crab Creek (which is suffering from low flows, see below); regionally the Columbia basalt aquifers discharge to the Columbia River, near the Quad Cities.

The Columbia Plateau regional aquifer system consists primarily of three basalt formations separated by confining units. Aquifer-test evaluation and potential effects of increased ground-water pumpage at the Stovepipe Wells Hotel area, Death Valley National Monument, California (USGS Water-Resources Investigations Report ) (*).

A B C D E F G H I J K L M N O P R S T U V W Y. Andelman, S.J., and Stock, A., Management, Research and Monitoring Priorities for the Conservation of. Columbia Plateau, Oregon and Washington. A Three-Dimensional Hydrogeologic Framework Model of Columbia Plateau Regional Aquifer System Geologic Framework Mapper: Web Tools Explanation Welcome General Instructions Contact: text.

Content for pane 3. Barlow, P.M., Ahlfeld, D.P., and Granato, G.E.,A simulation-optimization model for evaluation of ground-water development options constrained by minimum streamflow requirements and water-supply demands in Proceedings, MODFLOW and MORE —Managing Ground Water Systems, Eileen Poeter, Mary Hill, Chunmiao Zheng.

Columbia Plateau aquifer system Metadata Updated: March 7, This data set represents the extent of the Columbia Plateau aquifer system in the states of Washington, Oregon, and Idaho. Access & Use Information. License: No license information was provided. If Publish Year: WASHINGTON NE sw IDAHO OREGON Overburden aquifer Saddle Mountains unit Confining unit Wanapum unit Confining unit Grande Ronde unit NE Water table EXPLANATION Direction of ground-water flow NOT TO SCALE Basement confining unit FIGURE —Generalized ground-water-flow pattern in the Columbia Plateau aquifer system.

Umatilla Basin ground-water study bibliography. Hydrology of the Columbia Plateau Regional Aquifer System, Washington, Oregon, and Idaho: U.S. Geological Survey Water-Resources Investigations Report72 p. and Beeson, M.

H.,Intercanyon flows of the Columbia River Basalt Group in the lower Columbia River Gorge and. This geologic pdf is described in the report: Three-dimensional model of the geologic framework for the Columbia Plateau Regional Aquifer System, Idaho, Oregon, and Washington (Burns, E.R., Morgan, D.S., Peavler, R.S., and Kahle, S.C.,U.S.

Geological Survey Scientific Investigations Report ) publication date Complete None. 3-D Geologic Model of Columbia Plateau Aquifer System groundwater in the Columbia Plateau.

USGS hydrologist Erick Burns describes how his team modeled square mile plateau, how this.Regional ground-water flow usually ebook to large lakes and rivers (or in many cases, wells) and occurs in glacial and bedrock aquifers. Ground-water levels in regional aquifers may not necessarily mimic topography, and regional ground-water divides often do not coincide with surface-water divides (Eberts and George, ; Feinstein and.