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Guiana Highlands

File:Map_of_the_Guiana_shield.png · Wikimedia Commons · See Wikimedia Commons

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Guiana Highlands

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Also known as Guyana Highlands, Guyanese Highlands

higher elevations on the Guiana Shield

Key facts

Region
South America

via Wikipedia infobox

Wikidata facts

Instance of
highland
Country
Colombia
Located in
Guyana
Elevation
348
Highest point
Pico da Neblina
Image
Kukenan Tepuy at Sunset.jpg
Said to be same as
Guiana Shield
Show 6 more facts
partially coincident with
Guiana Shield
different from
Guiana Shield
Commons gallery
Guiana Highlands
topic's main category
Category:Guayana Highlands
Commons category
Guiana Highlands
on focus list of Wikimedia project
Wikipedia:Vital articles/Level/4
Sources (1)

via Wikidata · CC0

~6 min read

Encyclopedic overview

Cerros de Mavecure, Guainía department, Colombia Devil's Canyon in the Canaima National Park, Venezuela Map of the Guianas The Guiana Shield (French: Plateau des Guyanes, Bouclier guyanais; Dutch: Hoogland van Guyana, Guianaschild; Portuguese: Planalto das Guianas, Escudo das Guianas; Spanish: Escudo guayanés) is one of the three cratons of the South American Plate. It is a 1.7 billion-year-old Precambrian geological formation in northeast South America that forms a portion of the northern coast. The higher elevations on the shield are called the Guiana Highlands, which is where the table-like mountains called tepuis are found. The Guiana Highlands are also the source of some of the world's most well-known waterfalls such as Angel Falls, Kaieteur Falls, and Cuquenan Falls.

The Guiana Shield underlies Guyana (previously British Guiana), Suriname (previously Dutch Guiana), and French Guiana (or Guyane), much of southern Venezuela, most of Brazil north of the Amazon River, and parts of eastern Colombia. The first three are called The Guianas, and most of the Guiana Shield coincides with Guiana Island. The rocks of the Guiana Shield consist of metasediments and metavolcanics (greenstones) overlain by sub-horizontal layers of sandstones, quartzites, shales and conglomerates intruded by sills of younger mafic intrusives such as gabbros.

Excerpted from Wikipedia’s “Guiana Highlands” article, available under the CC BY-SA 4.0 licence.

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