Changes in the potentiometric-surface altitude of the confined aquifer, Wood River Valley aquifer system, south-central Idaho, October 2006 to October 2012.

Description

Water levels in 93 wells completed in the Wood River Valley aquifer system were measured during October 22–24, 2012; these wells are part of a network established by the U.S. Geological Survey in 2006. Maps of the October 2012 water-table altitude in the unconfined aquifer and the potentiometric -surface altitude of the confined aquifer have similar topology to those on maps of October 2006 conditions. Between October 2006 and October 2012, water-table altitude in the unconfined aquifer rose by as much as 1.86 feet in 6 wells and declined by as much as 14.28 feet in 77 wells; average decline was 2.9 feet. From October 2006 to October 2012, the potentiometric-surface altitude in 10 wells completed in the confined aquifer declined between 0.12 and 20.50 feet; average decline was 6.8 feet.

Resources

Name Format Description Link
55 Landing page for access to the data https://doi.org/10.5066/P9TFZT0D
55 The metadata original format https://data.usgs.gov/datacatalog/metadata/USGS.687e4f12-2048-4d56-9c2e-ede17436eb52.xml

Tags

  • inland-waters
  • water-table-altitude-change
  • idaho
  • ketchum
  • potentiometric-surface-altitude
  • hailey
  • blaine-county
  • silver-creek
  • sun-valley
  • wood-river-valley
  • picabo
  • u-s-geological-survey
  • bellevue
  • inlandwaters
  • big-wood-river
  • water-table-altitude
  • potentiometric-surface-altitude-change
  • hydrogeology
  • usgs
  • unconfined-aquifer
  • usgs-687e4f12-2048-4d56-9c2e-ede17436eb52
  • gannett
  • ground-water-level
  • aquifer
  • wood-river-valley-aquifer-system
  • confined-aquifer

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