Prolonged seismically induced erosion and the mass balance of a large earthquake

• Published in: Earth and planetary science letters Vol. 304; no. 3; pp. 347 - 355
• Main Authors: Hovius, Niels, Meunier, Patrick, Lin, Ching-Weei, Chen, Hongey, Chen, Yue-Gau, Dadson, Simon, Horng, Ming-Jame, Lines, Max
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 15.04.2011
• Subjects: Belts; earthquake; Earthquake construction; Economics; Erosion; landsliding; mass budget; mountain building; Mountains; Reduction; sediment transport; Sediments; Seismic engineering; Seismic phenomena; landsliding; earthquake; mass budget; sediment transport; mountain building
• ISSN: 0012-821X; 1385-013X
• DOI: 10.1016/j.epsl.2011.02.005

Large earthquakes deform the Earth's surface and drive topographic growth in the frontal zones of mountain belts. They also induce widespread mass wasting, reducing relief. The sum of these two opposing effects is unknown. Using a time series of landslide maps and suspended sediment transport data, we show that the M W7.6 Chi-Chi earthquake in Taiwan was followed by a period of enhanced mass wasting and fluvial sediment evacuation, peaking at more than five times the background rate and returning progressively to pre-earthquake levels in about six years. Therefore it is now possible to calculate the mass balance and topographic effect of the earthquake. The Choshui River has removed sediment representing more than 30% of the added rock mass from the epicentral area. This has resulted in a reduction of surface uplift by up to 0.25 m, or 35% of local elevation change, and a reduction of the area where the Chi-Chi earthquake has built topography. For other large earthquakes, erosion may evolve in similar, predictable ways, reducing the efficiency of mountain building in fold-and-thrust belts and the topographic expression of seismogenic faults, prolonging the risk of triggered processes, and impeding economic regeneration of epicentral areas. ► Mass balance of earthquake calculated from surface deformation and erosion. ► Erosion caused by earthquake has removed >30% of added rock mass. ► Landsliding and sediment transport in epicentral area peaked after earthquake. ► Erosion decayed to background levels in about six years.