Estudio geológico e hidrológico del Golfo de Urabá
DOI:
https://doi.org/10.26640/22159045.62Keywords:
Colombia, Golfo de Urabá, coastal process, hydrodynamic, geology, erosion, depositionAbstract
The coastal process of different intensity are responsible of effects over the coast line in a region which in a way or another affect their economy. The erosion-deposition balance in the beaches is close related to the hidrodinamics of the sea and the interaction with the atmosphere, completing in this way the sistem coast-sea-air.
Is this document a relatioship between the main results obtained in the study of the hidrodinamic and geological characteristics of the Gulf of Urabá is presented, carried out between 1988 and 1989 with the cooperation of the French Technical Mission.
This study permited to identify the formation of sedimentary accresion prism mainly in the surroundings of the deltas of the Atrato and Turbo rivers, as to define the oceanographical conditions during the humid and dry seasons, and also determine the morphological characteristics of the marine bottom.
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References
CORREA, I, et al. 1980. Proyecto Erosión Litoral entre Turbo y Necoclí, Costa Este del Golfo de Urabá (Antioquia) Resultados Preliminares. Universidad EAFIT.
MOLINA, A. 1992. La Percepción Remota Aplicada para Determinar la Circulación de las Aguas Superficiales del Golfo de Urabá y las Variaciones de su Línea de Costa. Boletín Científico CIOH No. 11.
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