Abstract
The Arboletes -Punta Rey littoral is a 5.5-km-long stretch of coast located at the southern Caribbean coast of Colombia, 80 km by car (paved road) to Montería . Geologically, it is located at terrains of the Sinú folded belt, a tectonically active sedimentary wedge evolving under the morphogenetic influence of numerous onshore and offshore manifestations of mud diapirism. It has a tropical climate. During the dry season (December–April), the zone is under the influences of the N–NE Trade winds that generate swells with wave periods between 6 and 9 s and significant wave heights up to 2 m. These waves are strongly modified by the serrated contours of the coastline and are rapidly eroding the beaches and littoral rocky formations of the area. During the wet season, the trade winds are replaced by lighter, 2–4 m/s, S to SW winds that generate seas with significant wave heights of up to 0.6 m. Net sand drift during the year in the area is toward the SW. The Arboletes -Punta Rey landscape is configured by an emerged marine terrace, a diapiric dome with active mud volcanoes, and by cliffs and their associated erosional features including caves, arches, stacks, and scarps of mass movements. These features are cut on sedimentary, highly weathered and densely fractured mudstones and shales, and in poorly consolidated diapiric muds. Besides its geomorphological interest, the Arboletes littoral is an interesting example of historical, kilometric-magnitude erosional coastline changes driven by the combination of natural- and man-induced causes including, in a short-term perspective, the poor geotechnical properties of rocks, bioerosion, absence of rainfall and waste waters management, strong wave action, beach sand mining, and inadequate coastal engineering practices.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Andrade CA (2003) Análisis del nivel del mar en la zona costera colombiana. In: Invemar (Santa Marta, Colombia) Definición de la vulnerabilidad de los sistemas biogeofísicos y socioeconómicos debido a un cambio en el nivel del mar en la zona costera colombiana (Caribe, Insular y Pacífico) y medidas para su adaptación. Informe técnico No. 4, 125p
Andrade CA, Barton EC (2000) Eddy development and motion in the Caribbean Sea. J Geophys Res 15(11):26191–26201
Atlas de Mapas Antiguos de Colombia (1992) Siglos XVI a XIX (segunda edición). Editorial Arco, Bogota 187p
Carvajal JH, Geomorphological features of Mud Diapirism. The Central Caribbean Coast, Chapter 3. p 1–23
Correa ID (2006) El litoral antioqueño. In: Hermelin M (ed) Geografía de Antioquia. Fondo Editorial Universidad Eafit, Academia Colombiana de Ciencias Exactas, Físicas y Naturales—capítulo de Antioquia, pp 137–150
Correa ID, Vernette G (2004) Introducción al Problema de la Erosión Litoral en Urabá (Sector Arboletes—Turbo) Costa Caribe Colombiana. Bolet Invest Mar Cost Invemar 33:5–26
Correa ID, Alcántara–Carrió J, González RD (2005) Historial and recent shore erosion along Colombian Caribbean coast. Journal of Coastal Research In: Proceedings of the 2nd Meeting in Marine Science, Valencia, Spain, P 52–57
Correa ID, Acosta S, Bedoya G (2007) Análisis de las causas y monitoreo de la erosión litoral en el Departamento de Córdoba. Convenio de Transferencia Horizontal de Ciencia y Tecnología No. 30 Corporación Autónoma de los Valles del Sinú y San Jorge—CVS–Universidad Eafit, Departamento de Geología (Área de Ciencias del Mar. Fondo Editorial Universidad Eafit, 128 p
Clark JA, Bloom AL (1979) Hydroisostasy and Holocene emergence of South America. In: Suguio K, Fairchild TR, Martin L, Flexor JM (eds) Proceedings of the international symposium on coastal evolution in the quaternary, The Brazilian National Working Group for the IGCP Project 61, pp 41–60
Duque H (1979) Major structural elements and evolution of Northwestern Colombia. In: Watkins JS, Montadert L, Dickerson PW (eds) Geological and geophysical investigations of continental margins. Am Assoc Petr Geol Mem 29:329–351
Duque H (1984) Structural style, diapirism and accretionary episodes of the Sinú—San Jacinto terrane. Southwestern Caribbean borderland. In: Bonini WE, Hargraves R B, Sagham R (eds) The South American—Caribbean plate boundary and regional tectonic. Geol Soc Amer Mem 162:303—316 (Version en español en Boletín Geológico INGEOMINAS Vol. 27 No. 2. Bogota. p. 1–29)
González DA (2007) Erosión litoral en el Sur del Departamento de Córdoba (Minuto de Dios—Santander de la Cruz): magnitudes, factores y estrategias de control y mitigación. MSc thesis in Ciencias de la Tierra, Departamento de Geología Universidad Eafit Medellin. 87 p
González DA, Guarín T, Johan F (2003) Evolución geomorfológica de los acantilados entre Arboletes (Antioquia) y la desembocadura del Río Córdoba (Córdoba). Geology Thesis, Departamento de Geología Universidad Eafit, Medellín. 998 p
Hsu JRC, Silvester R, Xia YM (1987) New characteristics of equilibrium shaped bays. Proceedings of the 8th International Conference on Coastal Engineering, ASCE, p 140–144
Martínez JM (1994) Los sismos del Atrato medio 17 y 18 de octubre de 1992 Noroccidente de Colombia. Rev Ingeominas 4:35–70
Molina A, Chevillot Ph (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 11:43–58
Page WD (1982) Holocene deformation of the Caribbean Coast Northwestern Colombia. Woodward and Clyde Consultants, San Francisco 25 p
Paniagua-Arroyave JF (2013) Migración histórica actualizada y predicción de la posición de la línea de costa en sectores acantilados críticos del litoral antioqueño considerando escenarios de ascenso del nivel del mar. MSc thesis in Ciencias de la Tierra, Departamento de Geología, Universidad Eafit, Medellín. 88 p
Prussmann J (2012) Nuevos elementos para el Manejo Integrado de la Región de Urabá, Costa caribe Colombiana. Base de datos espacial geomorfológica de la Franja Litoral de los Departamentos de Antioquia y Chocó. MSc Tesis in Ciencias de la Tierra, Departamento de Geología, Universidad Eafit, Medellín. 91p
Ramírez JE (1976) Los diapiros del Mar Caribe colombiano. Memorias Primer Congreso Colombiano de Geología, Separata 39 pp
Rangel BN, Correa ID, Anfuso G, Ergin A, Williams AT (2013) Assessing and managing scenery of the Caribbean Coast of Colombia. Tour Manag 35:41–58
Thomas YF, García VC, Cesaraccio M, Rojas X (2007) El Paisaje en el Golfo. In: Garcia-Valencia C (ed) Atlas del Golfo de Urabá, una mirada al Caribe de Antioquia y Choco. Instituto de Investigaciones Marinas y Costeras Invemar y Gobernación de Antioquia, Santa Marta, Colombia, pp 75–127
Toto E, Kellogs J (1992) Structure of the Sinú San Jacinto fold belt—An active acretionary prism in northern Colombia. J S Am Earth Sci 5(2):211–222
Vernette G (1985) La plateforme Continentale Caraȉbe de Colombie. Importance du diapirisme argeliaux Sur la Morphologie et la Sedimentation. These de doctorat Université Bordeaux. Francia. 387
Vernette G, Mauffret A, Bobier C, Briceño L and Gayet J (1992) Mud diapirism, fan sedimentation and strike- slip faulting, Caribbean Colombian Margin. Tectonophysics. p 335–349
Walkden M, Dickson M (2008) Equilibrium erosion of soft rock shores with a shallow or absent beach under increased sea leve rise. Mar Geol 251:75–84
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2016 Springer International Publishing Switzerland
About this chapter
Cite this chapter
Correa Arango, I.D., Paniagua-Arroyave, J.F. (2016). The Arboletes-Punta Rey Littoral, Southern Caribbean Coast. In: Hermelin, M. (eds) Landscapes and Landforms of Colombia. World Geomorphological Landscapes. Springer, Cham. https://doi.org/10.1007/978-3-319-11800-0_4
Download citation
DOI: https://doi.org/10.1007/978-3-319-11800-0_4
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-11799-7
Online ISBN: 978-3-319-11800-0
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)