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• W2024101911 abstract "Terra Nova, 22, 18–25, 2010 Abstract We report in-situ produced 10Be data from the Gorge du Diable (French Western Alps) to date and quantify bedrock gorge incision into a glacial hanging valley. We sampled gorge sidewalls and the active channel bed to derive both long-term and present-day incision rates. 10Be ages of sidewall profiles reveal rapid incision through the late Holocene (ca 5 ka) at rates ranging from 6.5 to 13 mm yr−1. Present-day incision rates are significantly lower and vary from 0.5 to 3 mm yr−1 within the gorge. Our data imply either delayed initiation of gorge incision after final ice retreat from internal Alpine valleys at ca 12 ka, or post-glacial surface reburial of the gorge. Our results suggest that fluvial incision rates >1 cm yr−1 into crystalline bedrock may be encountered in transient landscape features induced by glacial-interglacial transitions." @default.
• W2024101911 created "2016-06-24" @default.
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• W2024101911 date "2010-02-01" @default.
• W2024101911 modified "2023-09-23" @default.
• W2024101911 title "Dating bedrock gorge incision in the French Western Alps (Ecrins-Pelvoux massif) using cosmogenic¹⁰Be" @default.
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• W2024101911 doi "https://doi.org/10.1111/j.1365-3121.2009.00911.x" @default.
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