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Pishkun Dikes |
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Power Generation Narration
Geology Pishkun Reservoir and enclosing dikes are founded on glacial deposits (till) of an outwash plain lying east of the Sawtooth Mountains. The thickness and character of glacial till vary widely over short distances. Till was deposited by advancing ice and runoff fed by melting alpine glacier. The thickness range is suggested by the hummocky topography characterized by rounded hills and undrained or poorly drained depressions. The landscape just west of Pishkun Reservoir is dotted with small lakes and is generally poor drainage. The reservoir and dikes are at the eastern margin of the glacial outwash plain. Locally, erosion has cut through glacial deposits exposing shale and sandy shale of the Two Medicine formation. The thickness range of glacial deposits under and around the reservoir is not well known but may range up to 100 feet.
Links | Recreation | | Dams Located by State | USBR Montana Dams | North Great Plains Region Dams || Owner: Bureau of Reclamation, Montana Area Office,PO Box 30137, Billings, MT 59107-0137, (406) 247-7664 | Operator: Greenfields Irrigation District,
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