作者: Beth Pratt-Sitaula , Michelle Garde , Douglas W. Burbank , Michael Oskin , Arjun Heimsath
DOI: 10.1016/J.YQRES.2007.03.005
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摘要: About 5400 cal yr BP, a large landslide formed N400-m-tall dam in the upper Marsyandi River, central Nepal. The resulting lacustrine and deltaic deposits stretched N7 km upstream, reaching thickness of 120 m. 14 C dating 7 wood fragments reveals that aggradation subsequent incision occurred remarkably quickly (∼500 yr). Reconstructed volumes (∼0.16 3 ) (∼0.09 indicate bedload-to-suspended load ratio 1:2, considerably higher than ≤1:10 is commonly assumed. At downstream end dam, river incised new channel through ≥70 m Greater Himalayan gneiss, requiring minimum bedrock rate 13 mm/ over last yr. majority presumably fraction this time, suggesting much rates. high bedload from such an energetic mountain particularly significant addition to our knowledge sediment flux orogenic environments. © 2007 University Washington. All rights reserved.