Water-table altitude of the unconfined aquifer, Wood River Valley aquifer system, south-central Idaho, October 2012.

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.

Data e Risorse

Campo Valore
accessLevel public
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catalog_describedBy https://project-open-data.cio.gov/v1.1/schema/catalog.json
identifier USGS:2d82988d-6d4a-4405-8886-2f40aeb9ef0d
metadata_type geospatial
modified 20201117
old-spatial -114.415615, 43.299454, -114.048488, 43.778278
publisher U.S. Geological Survey
publisher_hierarchy Department of the Interior > U.S. Geological Survey
resource-type Dataset
source_datajson_identifier true
source_hash 127f4249eae5b0cd17bf57ef9e108ea39cf5d6c1
source_schema_version 1.1
spatial {"type": "Polygon", "coordinates": [[[-114.415615, 43.299454], [-114.415615, 43.778278], [ -114.048488, 43.778278], [ -114.048488, 43.299454], [-114.415615, 43.299454]]]}
theme {geospatial}
Gruppi
  • AmeriGEOSS
  • National Provider
  • North America
Tag
  • amerigeo
  • amerigeoss
  • aquifer
  • bellevue
  • big-wood-river
  • blaine-county
  • ckan
  • confined-aquifer
  • gannett
  • geo
  • geoss
  • ground-water-level
  • hailey
  • hydrogeology
  • idaho
  • inland-waters
  • inlandwaters
  • ketchum
  • national
  • north-america
  • picabo
  • potentiometric-surface-altitude
  • potentiometric-surface-altitude-change
  • silver-creek
  • sun-valley
  • u-s-geological-survey
  • unconfined-aquifer
  • united-states
  • usgs
  • usgs-2d82988d-6d4a-4405-8886-2f40aeb9ef0d
  • water-table-altitude
  • water-table-altitude-change
  • wood-river-valley
  • wood-river-valley-aquifer-system
isopen False
license_id notspecified
license_title License not specified
maintainer James R. Bartolino
maintainer_email jrbartol@usgs.gov
metadata_created 2025-11-22T09:31:11.949041
metadata_modified 2025-11-22T09:31:11.949046
notes 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.
num_resources 2
num_tags 34
title Water-table altitude of the unconfined aquifer, Wood River Valley aquifer system, south-central Idaho, October 2012.