Columbia River Plateau

From Wikipedia, the free encyclopedia

(Redirected from Columbia Plateau)
Jump to: navigation, search
The Columbia River Plateau covers much of the Columbia River Basalt Group, shown in green on this map. The Washington cities of Spokane, Yakima and Pasco, and the Oregon city of Pendleton, lie on the Columbia River Plateau.
The Columbia River Plateau covers much of the Columbia River Basalt Group, shown in green on this map. The Washington cities of Spokane, Yakima and Pasco, and the Oregon city of Pendleton, lie on the Columbia River Plateau.

The Columbia River Plateau is a geologic and geographic region that lies across parts of the U.S. states of Washington, Oregon, and Idaho. It is a wide flood basalt plateau between the Cascade and Rocky Mountains, cut through by the Columbia River. In common usage, the term 'Columbia Basin' refers to more or less the same area as the Columbia Plateau.[1]

Contents

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 (the Columbia River Basalt Group).[2] 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).[2] As the molten rock came to the surface, the earth's crust gradually sank into the space left by the rising lava.[2]

The subsidence of the crust produced a large, slightly depressed lava plain now known as the Columbia Basin or Plateau.[2] 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.[2] Entities that have been found in these lake beds are fossil leaf impressions, petrified wood, fossil insects, and bones of vertebrate animals.[2]

The Washington cities in the Columbia Plateau include:

Oregon cities in the Columbia Plateau include:

Major tourist attractions include lava flows that were created by the eruptions of the Pliocene and Miocene eras, the Blue Mountains, and the Columbia River.

  1. ^ Floyd, Ben, et al. "Glossary". (1998) Hanford Reach Protection and Management Program Interim Action Plan. Prosser, Washington: Benton County Planning Department.
  2. ^ a b c d e f Description: Columbia Plateau Columbia River Basalt. United States Geologic Survey, accessed October 9, 2007.

Advanced Search
Included Web Search Engines


Safe Search

close

Top Matching Results

Occasionally Search.com will highlight specialized results that are based on the context of your query. Examples of specialized results include specific links to news, images, or video.

Top Matching Results may highlight information from other Search.com pages, content from the CNET Network of sites, or third party content. The listings are based purely on relevance. Search.com does not receive payment for listings in this section but our partners that provide this data may get paid for listing these products.

Sponsored Links

This section contains paid listings which have been purchased by companies that want to have their sites appear for specific search terms and related content. These listings are administered, sorted and maintained by a third party and are not endorsed by Search.com.

Search Results

Search.com sends your search query to several search engines at one time and integrates the results into one list which has been sorted by relevance using Search.com's proprietary algorithm. You can customize the list of search engines included in your metasearch from the preferences.

The search engines that are used in your metasearch may allow companies to pay to have their Web sites included within the results. To view the Paid Inclusion policy for a specific search engine, please visit their Web site. Search.com does not accept payment or share revenue with any search engine partner for listings in this section.