| Table Mountain | |
|---|---|
South face of Table Mountain and Columbia River fromJohn B. Yeon State Scenic Corridor | |
| Highest point | |
| Elevation | 3,417 ft (1,042 m) NGVD 29[1] |
| Prominence | 377 ft (115 m)[1] |
| Coordinates | 45°41′26″N121°59′01″W / 45.690672°N 121.983694°W /45.690672; -121.983694[2] |
| Geography | |
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| Location | Skamania County,Washington, U.S. |
| Parent range | Cascade Range |
| Topo map | USGS Bonneville Dam |
| Geology | |
| Mountain type | Basalt |
Table Mountain is a peak rising on the north side of theColumbia River inWashington state, about 4 miles (6.4 km) north-northwest ofBonneville Dam. It is one of the most spectacular landmarks of theColumbia River Gorge. Its southeast face drops 2,400 feet (730 m) in less than one horizontal mile (1.6 km.), and is topped by an almost vertical 800-foot (240 m) cliff.[3] Table Mountain is joined by the similarGreenleaf Peak to the northeast, and also byHamilton Mountain to the southwest, which is lower, (2,438 ft or 743 m), but similarly steep and much closer to the Columbia. Together these peaks form an impressive group on the Washington side of the Gorge.
Between 1425 and 1450 AD the south side of Table Mountain sheared off and dammed theColumbia River in an event known as theBonneville Slide.[4]
The river soon carved a new bend around to the south, but for a whileNative Americans living in the area could walk across. This led to the legend known as theBridge of the Gods.[5]
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