– the peculiar rock formation is caused by erosion. from top of Mt. Roraima These
table-top mountains are the remains of a large
sandstone plateau that once covered the
granite basement complex between the north border of the
Amazon Basin and the
Orinoco, between the Atlantic coast and the
Rio Negro. This area is part of the remnants of the supercontinent
Gondwana. Throughout the course of the
history of Earth, the plateau began to erode and fragment about 300 million years ago (mya), and about 70 mya the tepuis were formed from the remaining
monadnocks. There are 115 such mesas in the
Gran Sabana in the southeast of Venezuela on the border with
Guyana and
Brazil, where the highest concentration of tepuis is found. The precipitous tablelands tower over the surrounding area by up to . Tepuis range in elevation from . The total surface area of all 115 tepuis is approximately . Because of their great age, some tepuis exhibit surface features and caves typical of
karst topography, formed in more water-soluble rocks such as
limestone. Caves include the
Abismo Guy Collet, the deepest quartzite cave in the world. Some of the
mesas are pocked with giant
sinkholes up to in diameter and with sheer walls up to deep. These sinkholes are formed when the roofs of tunnels carved by underground rivers collapse. Berry, Huber, et al. (1995) sort the tepuis into four districts defined by geographical criteria (
drainage basins) and floristic affinities. • the Eastern Pantepui District is located east of the
Caroni River in eastern Venezuela, western Guyana, and
Roraima state of northern Brazil. It includes
Mount Roraima,
Auyan-tepui, and the
Pacaraima Mountains. They are drained by the Caroni River, the
Mazaruni and
Essequibo rivers of Guyana, and the
Rio Branco of Brazil. • the Western Pantepui District in southwestern Venezuela bounded by the
Caura, Orinoco, and
Ventuari rivers. Mountains are of sandstone and granite with summits reaching between 1,300 and 2,350 meters elevation. It includes the granite
Sierra Maigualida (1,800 to 2,350 m.). The Yutajé Subdistrict includes the
Cerro Guanay,
Cerro Yaví, Cerro Coro Coro, and
Cerro Yutajé, with diverse shrublands and summits from 1,800 to 2,300 m. The
Cuao-Sipapo Massif includes the westernmost tepuis, made of sandstone and granite and reaching 1,400 and 2,000 m. • the Central Pantepui District includes Cerro Guaiquinima, Cerro Duida, Cerro Marahuaka, Cerro Huachamacari, and Cerro Yapacana. • the Southern Pantepui District includes the mountains along Venezuela's southern border with Brazil's
Amazonas state and includes
Cerro de la Neblina,
Cerro Aracamuni, and
Cerro Avispa. == Flora and fauna ==