Geomorfología y susceptibilidad de laderas a movimientos gravitacionales en el Valle del Río Cuevas, entre Quebrada de Matienzo y Curva de la Soberanía Argentina
Cuevas River Valley was profoundly changed by the glaciations of the Pleistocene and its relief continues to be modeled by periglacial processes that result in susceptible slopes to gravitational movement, causing several inconvenience to vehicular traffic by the Cristo Redentor Border Crossing....
Guardado en:
| Publicado en: | Boletín de Estudios Geográficos |
|---|---|
| Autor principal: | |
| Materias: | |
| Acceso en línea: | https://bdigital.uncu.edu.ar/fichas.php?idobjeto=8814 |
| Sumario: | Cuevas River Valley was profoundly changed by the glaciations of the Pleistocene and its relief
continues to be modeled by periglacial processes that result in susceptible slopes to
gravitational movement, causing several inconvenience to vehicular traffic by the Cristo
Redentor Border Crossing. In this paper geomorphology and dynamics slopes of the valley is
studied by a heuristic method to analyze and correlate the distribution of morphogenetic
processes with conditioning variables of stability, in order to zone the susceptibility of the
valley slopes to gravitational movements. |
|---|
