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Assessment of Coarse Sediment Mobility in the Black Canyon of the Gunnison River, Colorado
Abstract
The frequency of flows mobilizing river bank sediment along a majority of the Gunnison River in the BCNP has significantly declined since 1966, and decreases in the frequency of significant sediment-mobilizing flows were more pronounced for regions within the BC NP where the channel gradient is lower.
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Cited 12 times
References (17)
1 in Knowledge Hub, 16 external
