Frequency domain electromagnetic induction (EMI) data collected within and adjacent to the Little Wind River, Riverton, WY, USA

The electrical conductivity of the earth is used to help infer lithological and pore fluid properties. Various geophysical methods can provide estimates of the distribution of below ground electrical conductivity, with each method having certain limitations. This data release presents raw and processed results from land-based and water-based frequency domain electromagnetic induction (EMI) data collected from August 23, 2017 to August 28, 2017. The raw data consist of .csv files from the Geophex GEM-2 unit. Data were primarily collected by walking with the instrument at approximately 1 m off the ground in horizontal coplanar (ski flat) mode. A survey along a section of the Little Wind River in a kayak (with about 0.3 m of elevation above the water surface) was also collected.

Data e Risorse

Campo Valore
accessLevel public
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identifier USGS:5bce531fe4b0b3fc5cdc62b9
metadata_type geospatial
modified 20200826
old-spatial -108.40390, 42.98460, -108.39170, 42.99465
publisher U.S. Geological Survey
publisher_hierarchy Department of the Interior > U.S. Geological Survey
resource-type Dataset
source_datajson_identifier true
source_hash 89a4dd2ef44a2dc036cb37bb3fc8e38792495f93
source_schema_version 1.1
spatial {"type": "Polygon", "coordinates": [[[-108.40390, 42.98460], [-108.40390, 42.99465], [ -108.39170, 42.99465], [ -108.39170, 42.98460], [-108.40390, 42.98460]]]}
theme {geospatial}
Gruppi
  • AmeriGEOSS
  • National Provider
  • North America
Tag
  • amerigeo
  • amerigeoss
  • ckan
  • electromagnetic-surveying
  • environment
  • geo
  • geophysics
  • geoscientific-information
  • geoss
  • groundwater
  • hydrogeology
  • hydrology
  • inlandwaters
  • little-wind-river
  • national
  • north-america
  • riverton
  • surface-water
  • united-states
  • usgs-5bce531fe4b0b3fc5cdc62b9
  • wyoming
isopen False
license_id notspecified
license_title License not specified
maintainer Neil Terry
maintainer_email nterry@usgs.gov
metadata_created 2025-11-20T22:16:16.393009
metadata_modified 2025-11-20T22:16:16.393013
notes The electrical conductivity of the earth is used to help infer lithological and pore fluid properties. Various geophysical methods can provide estimates of the distribution of below ground electrical conductivity, with each method having certain limitations. This data release presents raw and processed results from land-based and water-based frequency domain electromagnetic induction (EMI) data collected from August 23, 2017 to August 28, 2017. The raw data consist of .csv files from the Geophex GEM-2 unit. Data were primarily collected by walking with the instrument at approximately 1 m off the ground in horizontal coplanar (ski flat) mode. A survey along a section of the Little Wind River in a kayak (with about 0.3 m of elevation above the water surface) was also collected.
num_resources 2
num_tags 21
title Frequency domain electromagnetic induction (EMI) data collected within and adjacent to the Little Wind River, Riverton, WY, USA