
Aquifer Characterization
Seismic refraction and resistivity surveys at Michigan’s Wyoming field station traced its unusually productive well, up to 150 gallons a minute, to a gravel layer feeding fractured bedrock below, recharged by a nearby mountain stream.
Working on a small field team at the University of Michigan’s research station in Wyoming, we used seismic refraction and electrical resistivity tomography to investigate why the camp’s well produces up to 150 gallons per minute, far more than neighboring wells. Our data, as well as geomorphic surveying in the area, pointed to a two-layer system with a permeable gravel layer feeding water down into fractured bedrock below, recharged by a nearby mountain stream. Our findings supported the case for the camp’s ongoing expansion project.
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