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574,725 km 2 (221,903 sq mi) 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. It is slightly smaller than Bosnia and ...
Costa Rica map of Köppen climate classification. Costa Rica borders the Caribbean Sea to the east, and the Pacific Ocean to the west. Costa Rica also borders Nicaragua to the north and Panama to the south. The highest point in the country is Cerro Chirripó, at 3,819 metres (12,530 ft).
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Not to be confused with Hallelujah. Alajuela ( Spanish pronunciation: [alaˈxwela]) is a district in the Alajuela canton of the Alajuela Province of Costa Rica. As the seat of the Municipality of Alajuela canton, it is awarded the status of city. By virtue of being the city of the first canton of the province, it is also the capital of the ...
Costa Rica supports an enormous variety of wildlife, due in large part to its geographic position between North and South America, its neotropical climate, and its wide variety of habitats. Costa Rica is home to more than 500,000 species , which represent nearly 5% of the species estimated worldwide, making Costa Rica one of the 20 countries ...
Costa Rican Central Valley. / 9.917°N 84.067°W / 9.917; -84.067. 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.
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 ...
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 ...