Groundwater risk assessment score sheet for the Spokane Valley Aquifer
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Groundwater risk assessment score sheet for the Spokane Valley Aquifer by Wade E. Hathhorn

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Published by State of Washington Water Research Center in Pullman, Wash .
Written in English


  • Groundwater -- Spokane River Valley (Idaho and Wash.) -- Quality,
  • Groundwater -- Pollution -- Spokane River Valley (Idaho and Wash.),
  • Spokane River Valley (Idaho and Wash.)

Book details:

Edition Notes

Statementby Wade E. Hathhorn and Tyler R. Wubbena.
ContributionsWubbena, Tyler R., State of Washington Water Research Center., United States. Dept. of the Interior.
The Physical Object
Paginationiv, 82 p. :
Number of Pages82
ID Numbers
Open LibraryOL17597666M

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Buy Groundwater risk assessment score sheet for the Spokane Valley Aquifer by Hathhorn, Wade E (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Wade E Hathhorn. Spokane Valley-Rathdrum Prairie Aquifer ATLAS; Critical Aquifer Recharge Area (CARA) Water Resource Center. Water Reclamation Facility Tours; Education Programs; Classroom Visits; Resource Library; Research. Groundwater Monitoring; Water Quality Research. Nonpoint Source Phosphorus Assessment; CARA Wastewater Evaluation; Completed Projects. Risk Assessment. Success through Academic Confinement (SAC) School. Spokane Valley-Rathdrum Prairie Aquifer ATLAS. Critical Aquifer Recharge Area (CARA) Little Spokane Groundwater Inventory & Mapping. NPS Assessment. Water Availability Standard. Water Demand Forecast Model. West Plains Geophysical Orientation Survey. WRIA 55 / River in the southwestern portion of the Spokane Valley.2 Groundwater is approximately 70 feet below ground surface, however, this aquifer does not appear to be connected to the main Rathdrum Prairie Aquifer, used for drinking water. The nearest surface water is the Spokane River, located approximately feet down gradient to the south

supplemental remedial soil and groundwater sampling and the Risk Assessment. Based on the The site is located over the Spokane Valley-Rathdrum Prairie Aquifer, the sole source for public March EPA released a fact sheet announcing the second phase of the removal. The site overlies the Spokane Valley-Rathdrum Prairie Aquifer, designated as a sole source of drinking water. Soil overlying the aquifer is highly permeable, facilitating the movement of contaminants into the groundwater. Groundwater within 3 miles of the site provides drinking water to over , people and is used for irrigating croplands. Aquifer & River Recharge: Spokane Valley-Rathdrum Prairie (SVRP) Aquifer and the Spokane River (Ecology Study) Water Use Curtailment in Texas: TCEQ Considers Drought Response (Priority, Riparian Rights & Contingency Plans) TWR # Ap In-Depth Water Articles. The record of decision (ROD) for cleanup of the Bunker Hill Mining and Metallurgical Complex Superfund Facility Operable Unit 3 (OU-3) (EPA ) represents the next step in a long and contentious path for all concerned with human health and the environment in the Silver Valley of northern Idaho, Lake Coeur d’Alene, and the Spokane River down to Upriver Dam.

  However, good quality groundwater available in quantity will have a high socio-economic value, and is also more likely to have a high ecological value. We hope that, by integrating those parameters in our assessment, groundwater ecological value is taken indirectly into account. Risk assessment. DEQ's Mission To protect human health and the quality of Idaho’s air, land, and water. DEQ is a state department created by the Idaho Environmental Protection and Health Act to ensure clean air, water, and land in the state and protect Idaho citizens from the adverse health impacts of pollution. Hydrogeology of, and ground-water flow in, a valley-fill and carbonate-rock aquifer system near Long Valley in the New Jersey Highlands / (West Trenton, N.J.: U.S. Dept. of the Interior, U.S. Geological Survey ; Denver, CO: Earth Science Information Center, Open-File Reports Section, [distributor], ), by R. S. Nicholson, Geological Survey. Evidence that is indicative of aquifer contamination/aquifer intercommunication and an assessment of the potential for offsite migration of contaminants in groundwater within the upper basalt.