Sedimentology and Geomorphology of Quaternary Alluvial Fans with Implications to Growth Strata, Lost River Range, Idaho
Small-radius (<2 km), steep (8-17°), Holocene debris flow dominant alluvial fans are depositing on top of large-radius (~5 km), shallow (2-3°) inactive Pleistocene sheetflood dominant alluvial fans along the western flank of the Lost River Range, Idaho. C...
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| Language: | en |
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2006
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| Online Access: | http://etd.lib.montana.edu/etd/2006/patterson/PattersonS0806.pdf |