SciELO - Scientific Electronic Library Online

 
 número45Fallamiento neotectónico de la Península de Nicoya y su relación con el escape tectónico delantearco CentroamericanoProgreso y retos de la geocronología 40Ar/39Ar en Costa Rica y Nicaragua índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • No hay articulos similaresSimilares en SciELO

Compartir


Revista Geológica de América Central

versión On-line ISSN 0256-7024versión impresa ISSN 0256-7024

Resumen

ULLOA, Andrés; AGUILAR, Teresita; GOICOECHEA, Carlos  y  RAMIREZ, Ronald. Description, Classification and Geological Aspects of the Karstic Regions of Costa Rica. Rev. Geol. Amér. Central [online]. 2011, n.45, pp.53-74. ISSN 0256-7024.

In Costa Rica the karstic phenomenon affects mainly carbonate rocks, constituting 0.85% of the country’s surface, with an approximate area of 431 km2. There are documented at least 9 episodes of carbonate deposition from the Late Cretaceous to Holocene, which include eleven stratigraphic units. These events are related to various geological-tectonic processes, changes in sea level, subsidence and changes in the sediment input. Ten karstic zones and four limestone sites have been defined: 1) North Pacific, 2) Tempisque, 3) South Zone, 4) Central Pacific, 5) Cabo Blanco and Malpaís, 6) Turrialba and Pacuare, 7) Talamanca, 8) Venado , 9) Central Valley, 10) Limón and the isolated karst areas: A) Garza, B) Cerro Huevo Frito, C)Cerro Morro and D) Playa Panama. These karstic features have morphologies which can be exo-karstic, including lapiaz, ‘mogotes’, karstic-towers, sinkholes and conical karst. The best known endokarstic phenomena are caves, in which it is common the development of speleothems. such as stalactites, stalagmites, columns, flowstones, draperies, calcareous pearls, etc. Serpiente Dormida (Sleeping Snake) cave is the deepest in the country, with -172 m, the longest is the Bruja - Rectangle - Tururún - Corredores system, with 3872 m in length. At least 258 caves in limestone have been registered, of which 41% have been mapped (100 caves). 88% of the caves in Costa Rica are found in karst areas of the Southern Zone (61%), Tempisque (17%) and Venado (10%), while the remaining 12% of caves are distributed in other karstic areas. These areas have special environmental and hydrogeological conditions that must be taken into account as to infrastructure development, and could also be exploited by tourism.

Palabras clave : Costa Rica; karst; carbonate rocks; karst regions; limestones; caves.

        · resumen en Español     · texto en Español     · Español ( pdf )

 

Creative Commons License Todo el contenido de esta revista, excepto dónde está identificado, está bajo una Licencia Creative Commons