File:Map_of_the_Guiana_shield.png · Wikimedia Commons · See Wikimedia Commons
Guiana Highlands
Sign in to saveAlso 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.