Gestión del Riesgo
Permanent URI for this collectionhttps://dspace.ueb.edu.ec/handle/123456789/44
Browse
Item Estudio de factores de susceptibilidad (topográfico, geologico, hidrologico, geomorfologico, desarrollo social y economico) de la quebrada situada al flanco suroeste del cerro Susanga, ante la posible reactivación del macrodeslizamiento, durante el periodo de noviembre Del 2012.(Universidad Estatal De Bolivar Facultad De Ciencias De La Salud Y Del Ser Humano Escuela De Administración Para Desastres Y Gestión Del Riesgo, 2012) Naranjo Garcés, Ernesto Mongomery; Acosta Arias, EnriqueThen we stop to examine relevant concepts to be used in the development of this thesis. Amenaza.- The threat is a condition with the potential to cause a consequence undesirable. A description of threat of landslides should include features these, the volume or areas of movement, the depths, and the speeds probability of occurrence. The threat is the probability of a landslide to occur particularly at a given time. (SUAREZ, 2009 p. 528) Nivel.- curves is called contour lines that marked on the ground to develop a horizontal path. Therefore we can define a line level represents the intersection of a surface with the ground level. On one level the Contours are drawn to represent height intervals are equidistant on a reference plane. Rift which. Joint fracture or on the body of a rock occasionally I produced by tectonic forces, presented definite directions which are called joints systems. The joints are especially important in modeling since it facilitates land erosion. The jointing is controlled by the structure geological and tectonic deformation. Drain. Design or stroke is effected by runoff or river shape the landscape. The set of these designs or lines are called "patterns drain. "The analysis and study of drainage patterns helps determine the nature, structure and texture of the rocks and the tectonics of the region (faults, folds, etc.).