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Woodson Debris Flow - Oregon Department of Geology and Mineral ...

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<strong>Geology</strong><br />

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The bedrock in the slopes above <strong>Woodson</strong> is relatively loose<br />

s<strong>and</strong>stone, which weathers to a s<strong>and</strong>.<br />

There are NO igneous rocks, which tend to weather to boulders.<br />

This is why the debris flow deposit at <strong>Woodson</strong> did not have big<br />

boulders like some other debris flow deposits in <strong>Oregon</strong>.<br />

The <strong>Woodson</strong> debris flow was composed <strong>of</strong> mostly water, s<strong>and</strong>,<br />

<strong>and</strong> woody debris.<br />

Example <strong>of</strong> a Boulder <strong>Debris</strong> <strong>Flow</strong><br />

(Mt. Hood, 2006)<br />

<strong>Woodson</strong> <strong>Debris</strong> <strong>Flow</strong><br />

with Only a Few Boulders<br />

Image credits: Bill Burns, 2006 <strong>and</strong> Scott Burns, 2007<br />

Burns, December 2007

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