Variaciones morfológicas y texturales de las playas entre Barranquilla y flecha de Galerazamba (1935 - 1996)
DOI:
https://doi.org/10.26640/22159045.90Keywords:
Barranquilla, Bocas de Ceniza, Fecha de Galerazamba, beaches, morphologyAbstract
The results of analysis about the behavior of the beaches in the sector between Barranquilla (Bocas de Ceniza) and flecha de Galerazamba are presented, Twenty-four profiles perpendicular to the coastline were taken between both seasonal periods (dry and humid). On the humid period, under the influence of the westerlies, the beaches lose their berm and experience a significant retrogression on their foreshore, sometimes in the order of tens of meters, exhibiting a con cave profile. On the humid season, when the easterlies weaken, the beaches build up and exhibit a convex profile in their morphology. Between Bocas de Ceniza and Santa Verónica the slopes are soft and are associated with fine sediment, while on the southern sector the gradient and the size of the grain increase on the foreshore.Downloads
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References
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Centro de Investigaciones Oceanográficas e Hidrográficas, Atlas Climatológico para el Caribe, Central de Pronósticos Oceanográficos y Meteorológicos, 3a edición. Cartagena. 138 p, 1997.
Dolan, R, Seasonal variations in beach profiles along the outer banks of North Carolina: Shore and Beach. October, 95p. 1996.
Dolan, R. y J. FERN, Swash processes and beach characteristic: The Professional Geographer, 17(4), pp. 210- 213, 1996.
Folk, R.L. A review of grain-size pararneters: Sedimentology, 6: pp 73-93, 1963.
Giraldo, L. y S. Lonin, Cálculo del Oleaje y Transporte de Sedimentos en la Costa Caribe Colombiana, Bol. Cient CIOH No 18. Cartagena, pp, 1997.
Greenwood, B; Gda, R. Marine Bars and nearshore sedimentary processes, Kouchibouguac Bay, New Brunswick, in Nearhore Sediment Dyrnics and Sedimentation, John Wiley and Sons, pp. 123 - 150, 1975.
IDEAM. Pronóstico de Pleamares y Bajamares Costa Caribe Colombiana, Santafé de Bogotá: 91 p, 1995.
......... , Pronóstico de Pleamares y Bajamares Costa Caribe Colombiana, Santafé de Bogotá: 95 p, 1996.
King, C.A.M, Beaches and coasts. 2nd ed, St. Martins Presa, New York: 570 p, 1972.
Komar, P. D. Nearshore currents and sediment transport, and the Resulting Beach, in Stanley, D.J. and Swift, D.J.P., ed. Marine Sediment Transport and Environmental Management. New York, John Wiley & Sons, pp, 241-254. 1976.
........., Selective longshore Current transport rates at different grain-size fraction with a Beach: journal of Sedimentary Petrology, 47(4). pp. 1444 -1453. 1977,
Martínez, J. O. Cambios en Perfiles de playa y Características Texturales de los sedimentos al Norte de Cartagena. I Congreso Latinoamericano Sobre Ciencias del Mar. 20 p, 1985.
Medina, R. y M. González, Morfodinámica de Playas. Cali Universidades de Cantabria y Valle, Cali: 500 p, 1996,
Molina, A., A. Pelgrain, L. y Giraldo, Suzunaga, J. Comportamiento de la Dinámica Marina en el Sector Costero entre Galerazamba y Cartagena. Bol. CIOH No 17, Cartagena: pp. 73-78. 1996.
Sonu, Bimodal composition and cyclic characteristic of beach sediments in continuosly changing profilesi J. Sediment. Petrol. 42, pp. 85Z-857. 1972, U.S. Army Corps of Engineers SBEACH: Numerical Model for Simulated Storm-lnduced Beach Change. Report 3 User's Manual, Instruction Report CERC-93-2,, Washington DC, 55 p, 1993
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1998-10-01
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How to Cite
Variaciones morfológicas y texturales de las playas entre Barranquilla y flecha de Galerazamba (1935 - 1996). (1998). CIOH Scientific Bulletin, 18, 23-38. https://doi.org/10.26640/22159045.90
