Snake River Plain FORGE Site Characterization Data McLing at al 2016 paper on wellbore and groundwater temp distribution in ESRP

The site characterization data used to develop the conceptual geologic model for the Snake River Plain site in Idaho, as part of phase 1 of the Frontier Observatory for Research in Geothermal Energy (FORGE) initiative. This collection includes data on seismic events, groundwater, geomechanical models, gravity surveys, magnetics, resistivity, magnetotellurics (MT), rock physics, stress, the geologic setting, and supporting documentation, including several papers. Also included are 3D models (Petrel and Jewelsuite) of the proposed site.

Data for wells INEL-1, WO-2, and USGS-142 have been included as links to separate data collections.

These data have been assembled by the Snake River Geothermal Consortium (SRGC), a team of collaborators that includes members from national laboratories, universities, industry, and federal agencies, lead by the Idaho National Laboratory (INL). Other contributors include the National Renewable Energy Laboratory (NREL), Lawrence Livermore National Laboratory (LLNL), the Center for Advanced Energy Studies (CEAS), the University of Idaho, Idaho State University, Boise State University, University of Wyoming, University of Oklahoma, Energy and Geoscience Institute-University of Utah, US Geothermal, Baker Hughes

Campbell Scientific Inc., Chena Power, US Geological Survey (USGS), Idaho Department of Water Resources, Idaho Geological Survey, and Mink GeoHydro. McLing et al, 2016. "Wellbore and Groundwater Temperature Distribution Eastern Snake River Plain, Idaho: Implications for Groundwater Flow and Geothermal Potential." A map of groundwater temperatures from the Eastern Snake River Plain (ESRP) regional aquifer can be used to identify and interpret important features of the aquifer, including aquifer flow direction, aquifer thickness, and potential geothermal anomalies. The ESRP is an area of high heat flow, yet most of this thermal energy fails to reach the surface, due to the heat being swept downgradient by the aquifer to the major spring complexes near Thousand Springs, ID, a distance of 300 km.

Data and Resources

Metadata Source

Additional Info

Field Value
Citation Date 2016-04-06T00:00:00-06:00

Harvest Information

Original ID f0000025-58cc-4372-a567-000000000793
Index Date 2018-08-14T16:05:10-06:00
Original Format ISO-USGIN
Original Version 1.2

Author

Name Robert Podgorney
Position primary contact
Organization Idaho National Laboratory
Email robert.podgorney@inl.gov

Geographic Extent

North Bound 44.256214279793
South Bound 42.37652175934
East Bound -111.31162109375
West Bound -114.7658203125