Géosciences Rennes, UMR 6118, CNRS, Université Rennes, Rennes, 35000, France
Ching-Chung Cheng
Department of Civil Engineering, National Chiao Tung University, Hsinchu, 30010, Taiwan
Jean-Paul Boy
Institut de Physique du Globe de Strasbourg, CNRS – Université de Strasbourg UMR 7516 – Ecole et Observatoire des Sciences de la Terre, Strasbourg, 67084 CEDEX, France
Institut de Physique du Globe de Strasbourg, CNRS – Université de Strasbourg UMR 7516 – Ecole et Observatoire des Sciences de la Terre, Strasbourg, 67084 CEDEX, France
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Total article views: 2,945 (including HTML, PDF, and XML)
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Land erosion creates sediment particles that are redistributed from mountains to oceans through climatic, tectonic and human activities, but measuring the mass of redistributed sediment is difficult. Here we describe a new method combining gravity and photogrammetry measurements, which make it possible to weigh the mass of sediment redistributed by a landslide and a river in Taiwan from 2015 to 2017. Trying this method in other regions will help us to better understand the erosion process.
Land erosion creates sediment particles that are redistributed from mountains to oceans through...
