Statistical analysis of landslide events in Central America and their run-out distance

被引:46
作者
Devoli G. [1 ,2 ]
De Blasio F.V. [1 ,2 ]
Elverhøi A. [1 ,2 ]
Høeg K. [1 ,2 ]
机构
[1] International Centre for Geohazards, c/o Norwegian Geotechnical Institute, Oslo 0806, Ullevaal Stadion
[2] Department of Geosciences, University of Oslo, Oslo 0316, Blindern
关键词
Central America; Debris flows; Lahars; Landslides; Nicaragua; Run-out distance;
D O I
10.1007/s10706-008-9209-0
中图分类号
学科分类号
摘要
Statistical analyses of landslide deposits from similar areas provide information on dynamics and rheology, and are the basis for empirical relationships for the prediction of future events. In Central America landslides represent an important threat in both volcanic and non-volcanic areas. Data, mainly from 348 landslides in Nicaragua, and 19 in other Central American countries have been analyzed to describe landslide characteristics and to search for possible correlations and empirical relationships. The mobility of a landslide, expressed as the ratio between height of fall (H) and run-out distance (L) as a function of the volume and height of fall; and the relationship between the height of fall and run-out distance were studied for rock falls, slides, debris flows and debris avalanches. The data show differences in run-out distance and landslide mobility among different types of landslides and between debris flows in volcanic and non-volcanic areas. The new Central American data add to and seem consistent with data published from other regions. Studies combining field observations and empirical relationships with laboratory studies and numerical simulations will help in the development of more reliable empirical equations for the prediction of landslide run-out, with applications to hazard zonation and design of optimal risk mitigation measures. © Springer Science+Business Media B.V. 2008.
引用
收藏
页码:23 / 42
页数:19
相关论文
共 57 条
[1]  
Alvarado G.E., Sigaran C., Perez W., Vulcanismo: Sus productos y geoformas, Geologia De Costa Rica. Editorial Tecnológica De Costa Rica, pp. 133-154, (2000)
[2]  
Alvarado G.E., Vega E., Chaves J., Vasquez M., Los grandes deslizamientos (volcánicos y no volcánicos) de tipo debris avalanche en Costa Rica, Rev Geol Am Central, 30, pp. 83-99, (2004)
[3]  
Alvarez A., Devoli G., Chavez G., Mayorga E., Amenazas por Deslizamientos en Ciudad Sandino, Estelí y Ocotal. Chapter III In Amenazas geológicas en Ciudad Sandino, Estelí y Ocotal, Nicaragua Report prepared for the Project: "Elaboración de mapas de riesgos naturales en tres zonas de intervención del PRRAC, Programa Regional De Reconstrucción De America Central (PRRAC), European Union, (2003)
[4]  
Alvarez A., Devoli G., Chavez G., Talavera E., Lahares La Chirca en Octubre de 2002, volcán Concepción, Isla de Ometepe. Rivas, (2003)
[5]  
Blanco F.A., Burgos E.A., Nejia M., Estudio De Amenaza Por Lahar En El Salvador: Revision De Casos Historicos Y Calibracion De Herramientas Para La Evaluacion De Amenaza, (2002)
[6]  
Capra L., Macias J.L., Scott K.M., Abrams M., Garduno-Monroy V.H., Debris avalanches and debris flows transformed from collapses in the Trans-Mexican Volcanic Belt, Mexico - Behavior and implications for hazard assessment, J Volcanol Geotherm Res, 113, pp. 81-110, (2002)
[7]  
Carrasco-Nunez G., Vallance J.W., Rose W.I., A voluminous avalanche-induced lahar from Citlaltépetl volcano, Mexico: Implications for hazard assessment, J Volcanol Geotherm Res, 59, pp. 35-46, (1993)
[8]  
Coe J.A., Godt J.W., Baum R.L., Bucknam R.C., Michael J.A., Landslide susceptibility from topography in Guatemala, Landslides: Evaluation and Stabilization, 1, pp. 69-78, (2004)
[9]  
Connor C., Connor L., Sheridan M., Assessment of October 2005 Debris Flows at Panabaj, Guatemala, and Recommendations for Hazard Mitigation, (2006)
[10]  
Corominas J., The angle of reach as mobility index for small and large landslides, Can Geotech J, 33, pp. 260-271, (1996)