![]() Spokane to Davenport 2 | ||||||||||
Basalt, Buttes and Channeled Scablands
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| "This mega-ripple field covers an area of approximately 60 square kilometers (23 square miles). The wavelength (length of each ripple) of these ripple bedforms range approximately from 60 to 120 meters! Amplitudes (height of ripple) range from 2 to 9 meters. Their stratigraphy (layers) and coarse-grained texture suggests a flood origin...clearly the product of floodwaters moving through the region." [Buchanan] |
[10.5 MM 273]
Loess, extremely fine sand particles blown by the wind in arid or glacial areas, covered the basalt layers and provides the fertile soil in the Palouse hills where dry land farms grow wheat, barley, lentils, bluegrass for lawns, and other farm crops.
Beneath the golden brown loess on this road cut is a sand and fine gravel deposit. We will see this tawny soil in road cuts in a number of places as we travel.
In the NASA image of Mars at right there are shaped islands and channels that are thought to have been caused by a great flood. These shaped channels are similar to those we will be passing through in this part of our trip.
The Mars Pathfinder landed in the Ares Vallis area (center of picture) that has flood channels and flood plains like those we will see later.
As we continue on US 2 for a few more miles we will be on the edge of the Channeled Scablands. At the town of Davenport we will turn south to drive through a flood channel and onto one of these islands.
[24.8 MM 258]
We see basalt exposures in the Scabland channelway. During the Ice Age floods, basalt was ground into depressions where pools now form. This scouring of the basalt can also be seen in and around Spokane as seen in the photo at right. This basalt knob is about 5 feet across.
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When Ice Age glaciers blocked the Columbia River, the Spokane River and the Clark Fork river in Montana they formed Glacial Lake Columbia, Glacial Lake Spokane and Glacial Lake Missoula. The evidence of these lakes can be seen in the lakebeds visible in various road cuts in eastern Washington and lap marks on hills and gravel deposits in Montana. Glacial Lake Missoula, the largest lake, covered some 3000 square miles and was about 2000 feet deep. What happens when 500 cubic miles of water is suddenly released? Find out more on the Channeled Scablands page or continue on to the NEXT page.
Here are some basic terms used on this page. Find more geology terms in the Glossary.
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