![]() |
|
|
Tieton Dam |
![]() |
|
Statistics |
|
|
|
|
|
|
Power Generation Narration
Geology The geologic structure of the basin has a base of shale and sandstone sediments which were subsequently overlain by the basalt flows of the Columbia River lava. As the Cascade Mountains uplifted, stream erosion cut deep canyons through the basalt and underlying rock. Subsequent to the uplift, lava flows completely covered the upper ends of the stream valleys and partly filled sections of the stream with andesite. The andesite in the canyons was later eroded away leaving the upper end of the valley still deeply buried. Glacial material and soil covers much of the valley floors and occassional terraces line the valley side. Miscellaneous Links | Current Reservoir Storage, plus other storage Units within the Yakima River Basin | Links | Recreation | | Dams Located by State | USBR Washington Dams | Pacific Northwest Region Dams | | Owner: Bureau of Reclamation, Upper Columbia Area Office, | Operator: Bureau of Reclamation, Upper Columbia Area Office, |
|
|
|
Dams | Projects | Powerplants | Contact Us | Maps | Glossary | FAQ´s | Links |