Impacts on Crab Creek
 
Generalized ground-water-flow pattern in the Columbia Plateau aquifer system.
 
 
 
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Columbia Institute for Water Policy

IMPACTS ON CRAB CREEK


Pumping from Odessa Aquifers is also causing surface water depletion.  The Odessa basalt aquifer system feeds Upper Crab Creek, an intermittent stream which is deeply incised into the Columbia basalts.   According to the local watershed assessment, Crab Creek receives a substantial portion of its flow from the Wanapum basalt aquifers.  It is unknown to what extent the groundwater pumping is contributing to low flows and complete de-watering of Crab Creek, however, the Odessa Subarea Aquifers do discharge to Crab Creek and other small streams in the area.  Their decline in basalt aquifer levels is likely having some effect on streamflow.

Map of Crab Creek, (source:  WRIA 43 Upper Crab-Wilson, Washington Dept of Ecology

WEB:  Coulee cross section, conceptual drawing of flow (WRIA 43 TA Report)
Links:  Dep’t of Ecology’s Crab Creek website
http://www.ecy.wa.gov/apps/watersheds/wriapages/43.html
WRIA 43 Technical Assessment of Crab Creek (Kennedy Jenks 2005)
http://mapdata.info/wria43/phase2.htm


USGS diagram of Columbia basalts. To enlarge diagram, click here.  (Source:  Whiteman, K. J.; Vaccaro, J. J.; Gonthier, J. B.; Bauer, H. H., The hydrogeologic framework and geochemistry of the Columbia Plateau Aquifer System, Washington, Oregon, and Idaho,  U.S. Geological Survey Professional Paper No. 1413-B (1994))http://www.ecy.wa.gov/apps/watersheds/wriapages/43.htmlhttp://www.ecy.wa.gov/apps/watersheds/wriapages/43.htmlhttp://mapdata.info/wria43/phase2.htmhttp://www.waterplanet.ws/pdf/wpoa20061018.pdfhttp://pubs.er.usgs.gov/usgspubs/pp/pp1413Bshapeimage_4_link_0shapeimage_4_link_1shapeimage_4_link_2shapeimage_4_link_3shapeimage_4_link_4