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Costa Rica (UK: / ˌkɒstəˈriːkə /, US: / ˌkoʊstə -/ ⓘ; Spanish: [ˈkosta ˈrika]; literally "Rich Coast"), officially the Republic of Costa Rica, [ 10 ] is a country in the Central American region of North America. Costa Rica is bordered by Nicaragua to the north, the Caribbean Sea to the northeast, Panama to the southeast, and the ...
Geography of Costa Rica. Costa Rica is located on the Central American Isthmus, surrounding the point 10° north of the equator and 84° west of the prime meridian. It has 212 km of Caribbean Sea coastline and 1,016 on the North Pacific Ocean. The area is 51,100 km 2 of which 40 km 2 is water.
Map of Costa Rica. This is a list of islands of Costa Rica. There are about 79 islands in Costa Rica. [1] Islands
Overview. The Constitution of Costa Rica states, "For Public Administration purposes, the national territory is divided into provinces, these into cantons and cantons into districts." The country consists of 7 provinces (provincias), 84 cantons (cantones), and 489 districts (distritos). [2]
Map of Costa Rica. This is a list of airports in Costa Rica, sorted by location.. Costa Rica, officially the Republic of Costa Rica, is a country in Central America, bordered by Nicaragua to the north, Panama to the southeast, the Pacific Ocean to the west, and the Caribbean Sea to the east.
Location in Costa Rica. Corcovado National Park (Spanish: Parque Nacional Corcovado) is a National Park on the Osa Peninsula, in Osa Canton, located on the southwestern regions of Costa Rica (9° North, 83° West), which is a part of the Osa Conservation Area. [1] Corcovado National Park was established on October 24, 1975 and occupies an area ...
Costa Rican Central Valley. The Central Valley (Spanish: Valle Central) is a plateau and a geographic region of central Costa Rica. The land in the valley is a relative plain, despite being surrounded by several mountains and volcanoes, the latter part of the Central Range. The region houses almost three quarters of Costa Ricans, and includes ...
The geology of Costa Rica is part of the Panama Microplate, which is slowly moving north relative to the stable Caribbean Plate. [1] [2] In the late Cretaceous, an oceanic trench or backarc system formed in connection with a subduction zone, situated where the Isthmus of Panama is now located. Into the early Paleogene, deep sea, open ocean ...
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