Erosional and chemical denudation rates in the Southwestern Idaho batholith
Annual erosional denudation (ED) and chemical denudation (CD) rates are determined on four forested watersheds located in the Idaho batholith, Idaho, U.S.A. Bedrock in the study area is a coarse‐grained quartz monzonite. Annual sediment yields are computed from sediment collected in settling ponds a...
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Veröffentlicht in: | Earth surface processes and landforms 1986-07, Vol.11 (4), p.389-400 |
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Format: | Artikel |
Sprache: | eng |
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