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Scientific Investigations Report 2012–5002


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Evaluation of Long-Term Water-Level Declines in Basalt Aquifers near Mosier, Oregon


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Figure 31. A conceptual model of repairs to a single confining unit in the Mosier, Oregon, study area. The connecting pipe represents the commingling well effect. (A) No commingling well, (B) well commingling all aquifers, (C–F) repair of each confining unit.

First posted March 1, 2012

For additional information contact:
Director, Oregon Water Science Center
U.S. Geological Survey
2130 SW 5th Avenue
Portland, Oregon 97201
http://or.water.usgs.gov

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