Glacially-induced scaling relations in mountain drainage basins
In glaciated British Columbia, Canada, Quaternary climate changes are responsible for profound spatial reorganization of earth surface processes. These changes have left a landscape characterized by topographic anisotropy associated with a hierarchy of glacial troughs. The evolution of formerly glac...
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| Language: | English |
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2010
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| Online Access: | http://hdl.handle.net/2429/18467 |