Columbia River Gorge
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The Columbia River Gorge is a spectacular canyon of the Columbia River in the Pacific Northwest of the United States. Up to 4,000 feet (1300 m) deep, the canyon stretches for over 80 miles (130 km) as the river winds westward through the Cascade Range forming the boundary between the State of Washington to the north and Oregon to the south. The Columbia Gorge American Viticultural Area is located in both states.
Extending roughly from the confluence of the Columbia with the Deschutes River down to eastern reaches of the Portland metropolitan area, the gorge furnishes the only navigable route through the Cascades. In 1805, the route was used by the Lewis and Clark Expedition to reach the Pacific Ocean.
The gorge today holds federally protected status as a National Scenic Area and is a popular recreational destination.
[edit] Description and history
Over the eons, the Columbia River has worn a deep gash into the volcanic rock of the Cascades, nearly down to sea level. The last major erosion occurred during the Missoula Floods during the ice age approximately 13,000 years ago. The most recent geological event was the Bonneville Slide in the 1700s, an event remembered in the local legends of the Native Americans as the Bridge of the Gods. Frequent rain nourishes a lush rain forest and replenishes the waters that cascade over the sheer basalt cliffs.
The western gorge is dominated by conifers, Bigleaf Maple, Cottonwood, Oregon Ash, and Vine Maple. The eastern gorge is home to Bigleaf Maple and Garry Oak. The wide range of elevation and precipitation in the gorge creates a diverse collection of ecosystems from the temperate rain forest at Oneonta Gorge (with an average annual precipitation of 75 inches [1900 mm]) to the Celilo grasslands (with average annual precipitation 12 inches [300 mm]). A large variety of endemic wildflowers thrives throughout the gorge.
The gorge has supported human habitation for over 13,000 years. Evidence of the Folsom and Marmes people, who crossed the Bering land bridge from Asia, were found in archaeological digs. Excavations near Celilo Falls, a few miles east of The Dalles, show humans have occupied this ideal salmon-fishing site for more than 10,000 years.
In addition to its natural beauty, the gorge also provides a critical transportation corridor and one of the most popular recreational locations in the Pacific Northwest. Atmospheric pressure differentials east and west of the Cascades create a wind tunnel effect in the deep cut of the gorge, generating 35 mph (56 km/h) winds that make it one of the finest and best-known windsurfing and kiteboarding locations in the world.
The gorge also contains the greatest concentration of waterfalls in the Pacific Northwest, with over 77 waterfalls on the Oregon side of the gorge alone. Many are along the Columbia River Highway, including the notable Multnomah Falls, which, at 620 feet (188 m), is often claimed (erroneously) to be the second tallest year-round waterfall in the United States.
In November 1986, Congress recognized the unique beauty of the gorge by making it first U.S. National Scenic Area and establishing the Columbia River Gorge Commission as part of an interstate compact.
[edit] See also
- Beacon Rock
- Bridal Veil Falls
- Portland Women's Forum
- Horsetail Falls
- Latourell Falls
- Oneonta Gorge
- Rooster Rock
- Shepperd's Dell
- Wahkeenah Falls
[edit] External links
- Columbia River Gorge National Scenic Area Act
- Columbia River Gorge National Scenic Area
- Columbia River Gorge Commission
- Historic Columbia River Highway
| Glacial Lake Missoula | Missoula Floods | Channeled scablands | Grand Coulee | Dry Falls | Drumheller Channels | Columbia River Plateau | Wallula Gap | Touchet Formation | Lake Lewis | Columbia River Gorge | Columbia River Basalt Group | Palouse Falls | Sims Corner Eskers and Kames | Moses Coulee | Withrow Moraine | Crab Creek
