Missoula Flood & Oneonta, Oregon
Posted by: Groundspeak Premium Member Rose Red
N 45° 35.362 W 122° 04.438
10T E 572233 N 5048842
Before the Missoula Flood, the Columbia River valley walls sloped gently down to the river. Afterwards, the drastically eroded valley walls ended in steep vertical slopes, such as the eroded 200’ Oneonta basalt wall.
Waymark Code: WM17AX
Location: Oregon, United States
Date Posted: 02/10/2007
Published By:Groundspeak Premium Member Blue J Wenatchee
Views: 88


More than 15,000 years ago the Missoula Flood, the largest and most powerful scientifically documented freshwater flood to occur on earth, happened in the Pacific Northwest.

During a period of several thousand years a single large flood, a few, or possibly as many as 100 of these floods scoured the 600-mile path when the glacial ice dam repeatedly reformed, the lake filled up again, and the ice dam broke again. Each flood was separated by decades or centuries.

Before the flood, the Columbia River valley walls sloped gently down to the river. The powerful flood scoured the landscape of vegetation, removed up to 150 feet of topsoil and deeply eroded its volcanic bedrock on both sides of the river. After the flood, the drastically eroded valley walls ended in very steep vertical slopes. The photo shows an eroded 200’ basalt wall of the Columbia Gorge rising almost vertically. It is located immediately east of the mouth of Oneonta Gorge, beginning east of milepost 34.3.

The 125’ straight bore Oneonta Tunnel (1914), one of four tunnels on the Historic Columbia River Highway, was reopened August 19, 2006. For the first time since it was filled with debris in 1948, daylight could be seen through the tunnel.

Instructions for logging waymark: A photograph is required of you (or your GPS receiver, if you are waymarking solo) and Oneonta basalt wall.

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You must actually visit a feature to post a log for it. You must post a picture that you have taken at the feature to have the waymark approved. It has to be in one of the states listed above.
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