Using AVIRIS Hyperspectral Imagery to Study the Role of Clay Mineralogy in Colorado Plateau Debris-Flow Initiation
The debris-flow initiation variable of clay mineralogy is examined for Holocene age debris-flow deposits across the Colorado Plateau. A Kolmogorov-Smirnov two-sample test between 25 debris-flow producing shale units and 23 shale units rated as not producing debris-flows found a highly significant d...
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| Language: | EN |
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The University of Arizona.
2005
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| Online Access: | http://hdl.handle.net/10150/194515 |