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Investigaciones geográficas
versión On-line ISSN 2448-7279versión impresa ISSN 0188-4611
Resumen
LEGORRETA PAULIN, Gabriel y LUGO HUBP, José. Hazard zonation of gravitational processes on the southwestern flank of Pico de Orizaba volcano, Mexico. Invest. Geog [online]. 2014, n.84, pp.20-31. ISSN 2448-7279. https://doi.org/10.14350/rig.37004.
The study area is the river Chiquito-Barranca del Muerto watershed that covers 111 Km2 and lies on the southwestern flank of Pico de Orizaba volcano. The watershed was studied by using aerial photographs of different years and fieldwork with an adaptation of the Landslide Hazard Zonation Protocol of the Washington State Department of Natural Resources, USA. 571 gravitational processes of six types were recognized: shallow, debris-avalanche and deep, debris flows and erthflows, and rock falls. We defined 12 major landforms on which gravitational processes occur: in ner gorges, headwalls, active scarps of deep-seated landslides, meanders, plains, three types of hillslopes classified by its gradient: low, moderate, and high, rockfall slopes, non-ruleidentified inner gorges, non-rule-identified headwalls, and non-rule-identified converging hillslopes. The potential gravitational processes were classified into three hazard ranges: low, high, and very high. Gravitational processes occur primarily in moderate gradient hillslopes, non-rule-identified inner gorges, inner gorges, and low-gradient hillslopes. The stability is low for plains and low gradient hillslopes, high for moderate and steep gradient hillslopes, and very high for the remaining eight landforms.
Palabras llave : GIS; landslide inventory map; landslide hazard map; Pico de Orizaba volcano.