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Dixon Canyon Dam |
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Power Generation Narration
Geology The damsite at Dixon Canyon is the center one of three damsite along the East Side if Horsetooth Reservoir. The canyon was formed by the erosion of a narrow notch through the north-south ridge of tilted Dakota sandstone. The formations involved are the same as those at Spring Canyon and Soldier Canyon, i.e. the Sundance, Morrison and Dakota. There are some differences in the thicknesses and intervals especially in the Dakota group. The rock floor under the dam is mostly Morrison shales and thin limestones with some on the lower and middle Dakota sandstones under the down stream face. The formations are all dipping downstream at an angle of 23 degrees. Bedrock is covered by a strip of alluvium down to the bottom of the canyon approximately 200 feet wide. It widens too more than 400 feet upstream from the centerline. Nearly all of the slopes on each side are conferred with gravel, soil and boulders except where the harder rocks crop out. Links | Recreation | | Dams Located by State | USBR Colorado Dams | South Great Basin Region Dams | | Owner: Bureau of Reclamation, Eastern Colorado Area Office, | Operator: Northern Colorado Water Conservancy District, | Top |
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