Columbia Plateau Essay

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Columbia Plateau The Columbia Plateau, also known as the Columbia Basalt Plain, is the uneven geographic feature of the interior Columbia River Basin. Its northern border is marked by the Columbia River and the mouth of the Okanagan River. The Columbia River makes a looping S-curve through the central Washington part of the Columbia Plateau. In a river basin that is mostly mountains and steep valleys, the Columbia Plateau is an area of flat land and gently rolling hills cut by the steep river canyons of the Columbia and its streams. It is a roughly triangular-shaped area about 250 miles on a side. On its fringes the elevation of the plateau is about 4,000 feet above sea level, and at its lowest point it is about 400 feet. The journals of Lewis and Clark briefly note the Plateau. The Columbia plateau formed between 6 million and 16 million years ago as the result of successive flows of basalt. The Columbia Plateau province is enclosed by one of the world’s largest accumulations of lava. Over 500,000 square kilometers of the Earth's surface is covered by it. The topography here is dominated by geologically young lava flows that flooded the countryside with amazing speed, all within the last 17 million years. Over 170,000 cubic kilometers of basaltic lava, known as the Columbia River basalts, covers the western part of the area. These tremendous flows erupted between 17-6 million years ago. Most of the lava flooded out in the first 1.5 million years -- an extraordinarily short time for such an outpouring of molten rock. The Columbia plateau formed between 6 million and 16 million years ago as the result of successive flows of

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