Geomorfología y dinámica fluvial para el análisis de amenaza por inundaciones en la zona de confluencia de los ríos Sumapaz y Magdalena, Ricaurte-Cundinamarca.
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El municipio de Ricaurte en el departamento de Cundinamarca presenta aumento en los niveles de los ríos circundantes, especialmente en su área urbana limítrofe, donde se ubican asentamientos no planificados, y conjuntos residenciales a lo largo de la ronda de los ríos Magdalena y Sumapaz. Estos ríos, según datos recopilados, han generado varios eventos de inundación en épocas de altas precipitaciones, sobre áreas urbanizadas tales como los barrios Villa Carolina y San Martín, además del condominio Puerto Peñalisa.
Estas áreas se encuentran sobre la zona de confluencia de los ríos Sumapaz y Magdalena; área que presenta evidencias morfológicas históricas de procesos morfodinámicos de dinámica fluvial muy activa, que, durante distintos periodos de tiempo, ha moldeado geoformas de génesis aluvial.
En este trabajo se busca integrar información base de diferentes fuentes, para dar paso a la construcción de un modelo que pueda ser empleado como instrumento primario en la comprensión de la amenaza por inundación asociada a la dinámica natural de los cuerpos hídricos en épocas de altos caudales.
The municipality of Ricaurte in the Department of Cundinamarca has increased the levels of the surrounding rivers, especially in the bordering urban area, where unplanned settlements and residential complexes are located along the Magdalena and Sumapaz rivers. These rivers, according to the data collected, have generated several flood events, in times of high winter, over urbanized areas such as Villa Carolina and San Martin neighborhoods, as well as the Puerto Peñalisa condominium. These areas are located on the confluence zone of the Sumapaz and Magdalena rivers, which presents historical morphological evidence of morphodynamic processes of very active fluvial dynamics during different periods, to a situation that has molded geoforms of alluvial genesis. In this work, we seek to integrate base from different sources to make the construction of a useful model as a primary instrument in the understanding of flood associated with the natural dynamics of water bodies in times of high flows.
The municipality of Ricaurte in the Department of Cundinamarca has increased the levels of the surrounding rivers, especially in the bordering urban area, where unplanned settlements and residential complexes are located along the Magdalena and Sumapaz rivers. These rivers, according to the data collected, have generated several flood events, in times of high winter, over urbanized areas such as Villa Carolina and San Martin neighborhoods, as well as the Puerto Peñalisa condominium. These areas are located on the confluence zone of the Sumapaz and Magdalena rivers, which presents historical morphological evidence of morphodynamic processes of very active fluvial dynamics during different periods, to a situation that has molded geoforms of alluvial genesis. In this work, we seek to integrate base from different sources to make the construction of a useful model as a primary instrument in the understanding of flood associated with the natural dynamics of water bodies in times of high flows.