作者: Seulgi Moon , C Page Chamberlain , Kimberly Blisniuk , Nathaniel Levine , Dylan H Rood
DOI: 10.1038/NGEO1159
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摘要: Erosion in the Washington Cascades Mountains was dominated by glacier activity until end of Last Glacial Maximum, when fluvial incision and mass wasting became dominant drivers. An analysis millennial-scale rates denudation range suggest erosion is sensitive both to spatial variations precipitation inherited topography.