Corfu Slide: Difference between revisions
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The '''Corfu Slide ''' is a geologic feature located on the north slope of the [[Saddle Mountain]]s near the [[Columbia river]] in eastern [[Washington]]. It covers aproximately 13 square kilometers and contains a volume of material of about 1 cubic kilometer. It is thought to have occured 13,000 to 15,000 years ago as the result of undercutting which occurred during the [[Missoula Floods]] associated with the retreat of glaicers during the last [[ice age]]. |
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==References== |
==References== |
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Revision as of 19:47, 6 April 2007
The Corfu Slide is a geologic feature located on the north slope of the Saddle Mountains near the Columbia river in eastern Washington. It covers aproximately 13 square kilometers and contains a volume of material of about 1 cubic kilometer. It is thought to have occured 13,000 to 15,000 years ago as the result of undercutting which occurred during the Missoula Floods associated with the retreat of glaicers during the last ice age.
References
The Corfu landslide: Analog to giant landslides on Mars. Lewis, S. W.; Baker, V. R. In NASA. Washington Rept. of Planetary Geology Program, 1983 p 230 (SEE N84-23431 13-91
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| Ice Age Glacial Floods |  | |
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| Glacial Lakes | ||
| Temporary Lakes | ||
| Ice Age Floods Glacial Residue | ||
| Ice Age Floods Erosion & Deposition Features | ||
| Related contemporaneous events | ||