Hazard zonation of gravitational processes on the southwestern flank of Pico de Orizaba volcano, Mexico
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...
| Authors: | , |
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| Format: | article |
| Status: | Published version |
| Publication Date: | 2013 |
| Country: | México |
| Institution: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repository: | Investigaciones Geográficas |
| Language: | Spanish |
| OAI Identifier: | oai:ojs.pkp.sfu.ca:article/37004 |
| Online Access: | https://www.investigacionesgeograficas.unam.mx/index.php/rig/article/view/37004 |
| Access Level: | Open access |
| Keyword: | SIG inventario de procesos gravitacionales mapa de peligros de procesos gravitacionales volcán Pico de Orizaba |
| Summary: | 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. |
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