2015
DOI: 10.3133/cir1359
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The quality of our Nation's waters: groundwater quality in the Columbia Plateau and Snake River Plain basin-fill and basaltic-rock aquifers and the Hawaiian volcanic-rock aquifers, Washington, Idaho, and Hawaii, 1993-2005

Abstract: For more information on the USGS-the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment-visit http://www.usgs.gov or call 1-888 -ASK-USGS.For an overview of USGS information products, including maps, imagery, and publications, visit http: //www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by… Show more

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Cited by 3 publications
(3 citation statements)
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References 31 publications
(42 reference statements)
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“…Wells in the Piedmont and Blue Ridge are generally shallower (median 108 m compared with 142 m) and much more likely to produce modern water; also, some layers of the Columbia Plateau basalt can act as confining layers. 69 Of the two interior sandstone PASs, the areal proportion for the Colorado Plateau (12.1%) is the lowest of any PAS and more consistent with previous NAWQA results 9 than that of the Cambrian− Ordovician (39.5%). Because wells in the Cambrian− Ordovician typically are deeper (median 267 m compared with 147 m), with more common confinement and production of premodern water, this difference in the rate of detection likely is driven by much greater pesticide loading on the predominantly agricultural land (73%) overlying the Cambrian−Ordovician relative to the Colorado Plateaus (2% agricultural land).…”
Section: ■ Results and Discussionsupporting
confidence: 86%
See 1 more Smart Citation
“…Wells in the Piedmont and Blue Ridge are generally shallower (median 108 m compared with 142 m) and much more likely to produce modern water; also, some layers of the Columbia Plateau basalt can act as confining layers. 69 Of the two interior sandstone PASs, the areal proportion for the Colorado Plateau (12.1%) is the lowest of any PAS and more consistent with previous NAWQA results 9 than that of the Cambrian− Ordovician (39.5%). Because wells in the Cambrian− Ordovician typically are deeper (median 267 m compared with 147 m), with more common confinement and production of premodern water, this difference in the rate of detection likely is driven by much greater pesticide loading on the predominantly agricultural land (73%) overlying the Cambrian−Ordovician relative to the Colorado Plateaus (2% agricultural land).…”
Section: ■ Results and Discussionsupporting
confidence: 86%
“…Of the two metamorphic/igneous PASs, the Piedmont and Blue Ridge crystalline aquifers have a higher areal proportion (53.6%) than the Columbia Plateau basaltic aquifer (35.6%). Wells in the Piedmont and Blue Ridge are generally shallower (median 108 m compared with 142 m) and much more likely to produce modern water; also, some layers of the Columbia Plateau basalt can act as confining layers . Of the two interior sandstone PASs, the areal proportion for the Colorado Plateau (12.1%) is the lowest of any PAS and more consistent with previous NAWQA results than that of the Cambrian–Ordovician (39.5%).…”
Section: Resultssupporting
confidence: 83%
“…For instance, water stress due to droughts and flooding has increasingly focused attention on how watershed ecosystems are being impacted by food production, specifically by agricultural runoff containing fertilizers and pesticides. In Idaho, excess application of fertilizers has been reported to impact groundwater quality in the Eastern Snake Plain Aquifer, which is the source of drinking water for over 300,000 residents of southern Idaho [ 87 ]. While fertilizers increase crop yield, the return flow of irrigated water delivers contaminants and sediment to the shallow groundwater system, which impacts the supply of drinking and urban use water.…”
Section: State Case Studiesmentioning
confidence: 99%