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Anderson Ranch Dam |
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Statistics |
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Power Generation
Geology Anderson Ranch Dam is located near the southwestern edge of Idaho Batholith which is composed of composed of a series of closely related, coarse-grained intrusions. Major normal faulting in the region includes faults in and adjacent to the batholith, faults bounding the northeast and southwest margin on the adjacent Snake River Plain, and faults forming Camas Prairie Basin east of the dam. These faults show a low to moderate seismic activity level. The dam is located in a narrow steep-sided valley cut through several hundred of igneous extrusive and extrusive rock. In the dam foundation, the rock was found to be intensely fractured and cut by numerous shears and fractures of varying widths. Several dikes were also found normal to the canyon axis. The dikes present a reduction of fractures and shears reducing the foundation permeability and making a tight foundation. Materials within the canyon include talus, colluvium, alluvium, residual soil and intact rock. These materials form the foundation of the dam And have performed well with respect to deformation and seepage.
Links | Recreation |Anderson Ranch Reservoir - Boat Ramp Elevations | | Dams Located by State | USBR Idaho Dams | Pacific Northwest Region Dams | Owner: Bureau of Reclamation, Snake River
Area Office - West, Operator: Bureau of Reclamation, Snake River
Area Office - West,
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