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Geological Formation

Cerro Autana

Named Rock Formations and Groups

Cerro Autana is a tepui, a flat-topped table mountain, on the western edge of the Guiana Shield in Amazonas state, Venezuela, near the Colombian border, rising to about 1,220 meters with a narrow base, nearly vertical walls and a flat summit. The mountain is the eroded remnant of a once much larger sandstone plateau that formerly covered the granite basement rock between the northern Amazon Basin and the Orinoco River. Water percolating along joints and bedding planes dissolves the silica cement holding the sandstone together, causing quartzite blocks to disaggregate and collapse; this process has carved extensive cave systems through the mountain and produced dramatic waterfalls along its scarps.

Facts
Classification
Protected Status
National Monument or Landmark 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Cerro Autana

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Cerro Autana
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Found In

Also in Geography Atlas: where this subject is found.

Also in Geography Atlas: where this subject is found.

Source Wikidata: Cerro Autana
Sources
1. Wikidata: Cerro Autana
  • Wikidata Q2119868, class allow-list match (w-wdresolver-0926)
  • Lead section
    Cerro Autana was declared a natural monument in 1978, including part of the Autana River and Lake Leopoldo.
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