Hydrogeologic Model for the Gable Gap Area, Hanford Site

Bjornstad, Bruce N. ; Thorne, Paul D. ; Williams, Bruce A. ; Last, George V. ; Thomas, Gregory S. ; Thompson, Michael D. ; Ludwig, Jami L. ; Lanigan, David C.

关键词: AQUIFERS;    BASALT;    COLUMBIA RIVER;    FLOODS;    GEOLOGIC HISTORY;    LAKES;    TECTONICS Gable Gap;    Hanford Site;    Gable Mountain;    Gable Butte;    geology;   

DOI  :  10.2172/992820
RP-ID  :  PNNL-19702
PID  :  OSTI ID: 992820
Others  :  Other: 830403000
Others  :  TRN: US201112%%129

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来源: SciTech Connect

【 摘 要 】

Gable Gap is a structural and topographic depression between Gable Mountain and Gable Butte within the central Hanford Site. It has a long and complex geologic history, which includes tectonic uplift synchronous with erosional downcutting associated with the ancestral Columbia River during both Ringold and Cold Creek periods, and by the later Ice Age (mostly glacial Lake Missoula) floods. The gap was subsequently buried and partially backfilled by mostly coarse-grained, Ice Age flood deposits (Hanford formation). Erosional remnants of both the Ringold Formation and Cold Creek unit locally underlie the high-energy flood deposits. A large window exists in the gap where confined basalt aquifers are in contact with the unconfined suprabasalt aquifer. Several paleochannels, of both Hanford and Ringold Formation age, were eroded into the basalt bedrock across Gable Gap. Groundwater from the Central Plateau presently moves through Gable Gap via one or more of these shallow paleochannels. As groundwater levels continue to decline in the region, groundwater flow may eventually be cut off through Gable Gap.