Columbia Plateau
The Columbia Plateau is a geologic and geographic region that lies across parts of the U.S. states of Washington, Oregon, and Idaho.[1] It is a wide flood basalt plateau between the Cascade Range and the Rocky Mountains, cut through by the Columbia River. In one of its various usages, the term "Columbia Basin" refers to more or less the same area as the Columbia Plateau.[2]
Geology
During late Miocene and early Pliocene times, one of the largest flood basalts ever to appear on the earth's surface engulfed about 63,000 square miles (160,000 km²) of the Pacific Northwest, forming a large igneous province.[3] Over a period of perhaps 10 to 15 million years lava flow after lava flow poured out, eventually accumulating to a thickness of more than 6,000 feet (1.8 km).[3] As the molten rock came to the surface, the earth's crust gradually sank into the space left by the rising lava.[3]
The subsidence of the crust produced the large plateau - a large, slightly depressed lava plain sometimes also known as the Columbia Basin.[3] The ancient Columbia River was forced into its present course by the northwesterly advancing lava. The lava, as it flowed over the area, first filled the stream valleys, forming dams that in turn caused impoundments or lakes.[3] Entities that have been found in these lake beds are fossil leaf impressions, petrified wood, fossil insects, and bones of vertebrate animals.[3]
Geography
The Washington cities in the Columbia Plateau include:
Oregon cities in the Columbia Plateau include:
See also
References
- ^ U.S. Geological Survey Geographic Names Information System: Columbia Plateau
- ^ Floyd, Ben, et al. "Glossary". (1998) Hanford Reach Protection and Management Program Interim Action Plan. Prosser, Washington: Benton County Planning Department.
- ^ a b c d e f Description: Columbia Plateau Columbia River Basalt. United States Geologic Survey, accessed October 9 2007.