Region 1, Western mountain ranges

Foxworthy, B.L.; Hanneman, Debra L.; Coffin, Donald L.; Halstead, E C

doi:10.1130/dnag-gna-o2.25

Cited by 1 publication

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“…The permeability distribution is therefore highly variable. The most dominant feature for groundwater flow is the fractures and faults that formed along with the mountains (e.g., Randall et al [1988] for the Appalachians) as well as the deformed lithology (e.g., Foxworthy et al [1988] for the Cordillera). Water flows mainly through the fractures under gravity drainage from the high elevations to the lower valleys.…”

Section: Bedrock Hydrogeologymentioning

confidence: 99%

Simulating the impact of glaciations on continental groundwater flow systems: 2. Model application to the Wisconsinian glaciation over the Canadian landscape

et al. 2008

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[1] A 3-D groundwater flow and brine transport numerical model of the entire Canadian landscape up to a depth of 10 km is constructed in order to capture the impacts of the Wisconsinian glaciation on the continental groundwater flow system. The numerical development of the model is presented in the companion paper of Lemieux et al. (2008b). Although the scale of the model prevents the use of a detailed geological model, commonly occurring geological materials that exhibit relatively consistent hydrogeological properties over the continent justify the simplifications while still allowing the capture of large-scale flow system trends. The model includes key processes pertaining to coupled groundwater flow and glaciation modeling, such a densitydependent (i.e., brine) flow, hydromechanical loading, subglacial infiltration, isostasy, and permafrost development. The surface boundary conditions are specified with the results of a glacial system model. The significant impact of the ice sheet on groundwater flow is evident by increases in the hydraulic head values below the ice sheet by as much as 3000 m down to a depth of 1.5 km into the subsurface. Results also indicate that the groundwater flow system after glaciation did not fully revert to its initial condition and that it is still recovering from the glaciation perturbation. This suggests that the current groundwater flow system cannot be interpreted solely on the basis of present-day boundary conditions and it is likely that several thousands of years of additional equilibration time will be necessary for the system to reach a new quasi-steady state. Finally, we find permafrost to have a large impact on the rate of dissipation of high hydraulic heads that build at depth and capturing its accurate distribution is important to explain the current hydraulic head distribution across the Canadian landscape.

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Section: Bedrock Hydrogeologymentioning

confidence: 99%