Guiana Shield
Sign in to savegeological formation in northeast South America
In the Vinony graph
Within Vinony's link graph, Guiana Shield is referenced by 455 other articles, and connects out to Andean Volcanic Belt, Amazonas and quartzite.
The entry is geolocated on the map.
It sits within the topics Commons link is locally defined, Flora of northern South America and Geographical regions of Venezuela.
Its subject is documented across 31 Wikipedia language editions.
Key facts
- Region
- South America
via Wikipedia infobox
Wikidata facts
- Instance of
- shield
- Part of
- Amazonian Craton
- Named after
- Guyanas
- Country
- France
- Highest point
- Pico da Neblina
- Image
- Kukenan Tepuy at Sunset.jpg
Show 3 more facts
- different from
- Guiana Highlands
- partially coincident with
- Guiana Highlands
- Commons category
- Guiana Shield
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 Shield” article, available under the CC BY-SA 4.0 licence.