Shallow seismic compressional and shear wave refraction and electrical resistivity investigations at Rocky Flats, Jefferson County, Colorado

Hans D. Ackermann

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Shallow seismic compressional and shear wave refraction and electrical resistivity investigations at Rocky Flats, Jefferson County, Colorado

Hans D. Ackermann

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Abstract

Seismic refraction and electrical resistivity investigations at Rocky Flats, Colo., a gravel-capped pediment, indicated an irregular bedrock surface which ranges in depth from 3 to 27 m (10-90 ft). Layers within the gravel that were revealed by interpretation of seismic and electrical data do not correlate, but the combining of results reveals information about water saturation and elastic properties of the overburden. Velocity variations within bedrock affect depth calculations.

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Journal of Research of the U.S. Geological Survey Article

Source-reported bounding extent: 39.82462208372805° to 39.95817509460007° latitude; -105.25657653808594° to -105.08182525634766° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Hans D. Ackermann. 1974. Shallow seismic compressional and shear wave refraction and electrical resistivity investigations at Rocky Flats, Jefferson County, Colorado. https://pubs.usgs.gov/publication/70232460

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