- Guiana Shield
The Guiana Shield [The term "Guiana" or "The Guianas" is often used as a collective name for
Guyana ,Suriname andFrench Guiana , and sometimes even includes the portions ofColombia ,Venezuela andBrazil which are on the Guiana Shield.] ( _es. Guayana) is one of the threecraton s of theSouth American Plate . It is a 1.7 billion year oldPrecambrian geological formation in northeastSouth America that forms a portion of the northern coast. The higher elevations on the shield are called the Guiana Highlands, which is where the impressive and mysterious table-like mountains calledtepui s are found. The Guiana Highlands are also the source of some of the world's most spectacular waterfalls such asAngel Falls ,Kaieteur Falls andKuquenan Falls .The Guiana Shield underlies
Guyana (previously British Guiana),Suriname (previously Dutch Guiana) andFrench Guiana (or Guyane), as well as parts ofColombia ,Venezuela andBrazil . The rocks of the Guiana Shield consist of metasediments and metavolcanics (greenstones ) overlain by quasi-horizontal layers ofsandstones ,quartzites ,shales and conglomerates intruded by sills of younger mafic intrusives such asgabbros .Geomorphology
There are three upland areas of the Guiana Shield.
# TheGuiana Highlands proper are in Venezuela east of the Orinoco and extend across much of westcentral Guyana and into the northernRoraima state in Brazil.
# The Tumucumaque Uplands which are a series of central massifs in an arc from theWilhelmina Mountains of south-central Suriname, along the southern boundary of Suriname and Guyana, forming the Acarai Mountains of Roraima state and theTumuc-Humac Mountains ofPará andAmapá states of Brazil. From this arc, the southern uplands slope gently downwards towards the Amazon River and the northern uplands slope gently downwards towards theAtlantic .
# The Chiribiquete Plateau is a sandstone toppedplateau with an elevation of Convert|900|m|ft|0|abbr=on that forms the western edge of the shield. The plateau is separated from the easternAndes by the thickNeogene sediments of the Sub-Andean Trough that runs along the northern and western rim of the Guiana Shield.The north-central part of the Guiana Highlands is dominated by high flat-topped peaks called
tepui s, of the Roraima supergroup and Quasi-Roraima formation, and the rounded granite peaks of the Parguaza and Imataca complexes to the north and southwestern edges of the area. The highest tepui isMonte Roraima at 2,810 m (9,219 ft), on whose top plateau the Venezuela, Guyana and Brazil border tripoint is located, but the Guiana Shield's highest point isPico da Neblina in Brazil (next to the Venezuelan border) at 2,994 m (9,822 ft). Pico da Neblina is not a tepui but a rather sharp peak, and is located far to the west and south of the area where tepuis are found.Ecology
The Guiana Shield is one of the regions of highest
biodiversity in the world. The Shield has 1400vertebrate species and 1680bird species.Fact|date=March 2008 The Shield is overlain by the largest expanse of undisturbed tropical rain forest in the world. [Hammond, David S. (ed.) (2005) "Tropical Rainforests of the Guianan Shield" CABI Publishing, Wallingford, UK, ISBN ] Guianan rain forest is similar in nature toAmazonian rain forest and known Protected Areas include the Iwokrama Forest of central Guyana and theKanuku National Park of southern Guyana. In Venezuela the forests are partially protected by theCanaima National Park (VE) and theKaieteur National Park (GY).References
See also
*
Tepui
*Canadian Shield
*Caribbean South America
*Monte Roraima
*Pico da Neblina
*Great American Interchange
*Geography of South America
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