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Regional Assessment of Ground-Water Quality in Principal Volcanic Aquifers of the Western United States

The Western Volcanics study brings together three areas with similar aquifer properties: Columbia Plateau basaltic-rock aquifers, Snake River Plain basaltic-rock aquifers, and Hawaiian volcanic-rock aquifers. These are extensive provinces of layered igneous rocks (mostly basaltic lava flows) that host regional ground-water flow systems. Important sedimentary aquifers (basin-fill aquifers) overlie basalts of the Columbia Plateau and Snake River Plain. In Hawaii, sediments overlie volcanic-rock aquifers along the coastal perimeter of the islands, but the sedimentary aquifers are not used as drinking-water sources.

The volcanic-rock aquifers are highly susceptible to contamination because they are mostly unconfined and are overlain by thin or well-drained soils. All three areas are farmed intensively, were irrigated heavily for most of the 20th century, and have had agricultural fertilizers and pesticides applied. Numerous agricultural and industrial chemicals have been detected in ground water, though most concentrations are below human-health guidelines.

A notable exception is nitrate, a nutrient for which elevated concentrations commonly are ascribed to fertilizer application, animal manure, or nitrogen-fixing plants (legumes) such as alfalfa. In ground-water samples collected by NAWQA (1991-2000), nitrate concentrations in 20 percent of Columbia Plateau wells and 3 percent of Snake River Plain wells were above the U.S. Environmental Protection Agency drinking-water standard of 10 milligrams per liter. No wells in Hawaii had nitrate concentrations above the standard.

The western volcanics study seeks to explain the causes of such similarities and differences through statistical analysis of soil properties, crop types, and other factors. Past trends in water quality also are under study, with an eye toward future forecasting through the use of ground-water modeling.

Topics selected for the assessment of water quality in the principal volcanic aquifers of the Western United States:

  • How does water quality in surficial aquifers compare to water quality in volcanic bedrock aquifers in the Western United States?
  • How does the regional flow system influence the quality of ground water once it has reached the deep volcanic aquifers?
  • How do land-use patterns and chemical-application practices influence water quality?
  • What changes in land use are taking place, and how might these changes affect water quality in the future?

General Information

Informational handout about the principal volcanic aquifers of the Western United States (PDF format, 1Mb)

Detailed information on the hydrogeology of the principal volcanic aquifers of the Western United States can be accessed through the USGS Ground Water Atlas of the United States

For more information, contact:
Charles Hunt, Hydrologist

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Page Last Modified: Wednesday, 27-Aug-2008 10:31:29 EDT