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The Channeled Scablands Of Eas

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tern Washington As we enter Washington from the east, we immediately run into the gentle rolling hills of the Palouse country. If we continue to travel westward, we suddenly enter a heavily scarred land of barren rock, channels and canyons. Rugged cliffs, basalt rock basins, concave cliffs and eve ....

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....began to accumulate over the field, eventually producing the rich farmland of the Palouse hills. The silt reaches a maximum depth in the Pullman-Colfax area at 200 feet. The Northern Hemisphere's Ice Age began more then 2 million years ago, but the Scablands history was not yet formed until 100,000 years ago. At this time the great continental glaciers began to make their march from British Columbia to what is now known as northern Washington, Idaho, and Montana. The ice sheet divided its sel....
Number of words: 1010 Approximate pages: 4

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