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Vega Dam |
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Power Generation Narration
Geology Collbran Project is located along the northeastern slope of Grand Mesa. The mesa is composed of horizontally bedded, tertiary rocks belonging to the Wasatch and Green River formations and capped by lave flow of Quaternary basalt. During Pleistocene times, sheet-like glaciers covered the mesa. Glacial scouring produced the many small mesa lakes and the heterogeneous deposits of glacial debris, which mantle a large part of the surface rock. These glacial deposits cover the lava in varying depths from one hundred to several hundred feet. The Vega Damsite is in an erosional narrows cut across the toe of a large fan. Overburden debris covers bedrock at the damsite to a depth of 135 feet, becoming progressively deeper to the south. The fan is composed of clayey silt containing basalt boulders. It is compact and seepage tests indicate that it is watertight. Even with a high water table, little or no slumping of side slopes has occurred, and other field evidence indicates good stability. Links | Recreation | | Dams Located by State | USBR Colorado Dams | Upper Colorado Region Dams | | Owner: Bureau of Reclamation, Western Colorado Area Office, | Operator: Collbran Conservancy District,
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