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Differential Synthetic Aperture Radar Interferometry to Investigate Surface Deformation of the Eastern Snake River Plain, Idaho, U.S.A.

The Eastern Snake River Plain (ESRP) is a northeast-trending volcanic basin that marks the track of the Yellowstone hotspot. Subsidence has characterized the ESRP since at least 4 Ma. To test whether subsidence of the ESRP surface is an active process, synthetic aperture radar interferometry has been applied to detect deformation during 1993–2000. Results show that no regionally consistent deformation occurred across the ESRP during the periods of observations. However, local displacements of 1–3-cm magnitude have been detected in the adjacent Basin-Range province. This deformation is not attributed to long-term movement of the ESRP but instead to local tectonic and/or groundwater processes.