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History of Parque Nacional Canaima


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The only form of relief are the tepuies, that are plateaus which are unique features, among which are its vertical and nearly flat tops, although there are several tepuies that do not meet these rules. Geologically are remnants of a sedimentary cover composed of very ancient sandstone that is superimposed on a base of igneous rocks (mainly granite) that is even older (nearly 3000 million years). On its summit is home to a very substantial amount of very specific endemic species, both plant and animal. Some endemic plant species are categorized as "carnivorous", which are thus the food supply (mainly insects) that are so scarce in the mountains. These have a geological formations ranging between 1500 and 2000 million years, which makes them one of the oldest formations in the world. The best known tepuies are: the Auyantepuy (where it follows the Angel Falls), the Roraima, the Kukenan and the Chimant� among many others.

Canaima National Park is located in the south-east of Venezuela in Bol�var State close to the borders with Brazil and Guyana. The park protects the north-western section of the Guayana Shield, an ancient geological formation shared with Brazil, the Guianas and Colombia. The park was established in 1962 with an area of 10,000km2, but its size was increased to 30,000km2 in 1975 in order to safeguard the watershed functions of its river basins. At that time it became the world's largest national park, its area being equivalent to that of Belgium in Europe, or larger than the State of Maryland. In recognition of its extraordinary scenery and geological and biological values, the park was conceded World Heritage Status in 1994, forming one of a select list of 126 natural and natural-cultural World Heritage Sites worldwide. Canaima actually fulfilled all four of UNESCO's criteria for qualification as a World Heritage property. Ironically, the name of the park, which derives from the novel "Canaima" by Venezuelan author R�mulo Gallegos, means "spirit
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