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Geological Formation

Brandberg Mountain

Inselbergs and Crystalline Monoliths

Brandberg Mountain is a massif of granite in the Namib Desert of northwestern Namibia and, at about 2,573 meters, the country's highest point. It formed from a large granite intrusion, or pluton, that crystallized underground roughly 132 million years ago during the tectonic rifting that separated Africa from South America, and was later exposed at the surface as the softer surrounding rock eroded away. The granite dome rises abruptly from the surrounding flat desert plain, and its slopes hold thousands of ancient rock paintings created by San hunter-gatherers, including the well known panel called the White Lady, making the mountain notable both for its granite geology and for its archaeological significance.

Facts
Classification
Protected Status
National Monument or Landmark 1
Connections

Associated With

Cretaceous, Eras
Source Wikipedia: Brandberg Mountain, Wikipedia

Caused By

Rifting, Processes
Source Wikipedia: Brandberg Mountain, Wikipedia
Weathering, Processes

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Source Wikidata: Brandberg Mountain
Sources
1. Wikipedia: Brandberg Mountain, Wikipedia
  • Location and extent
    The core area of 450 square kilometres (170 sq mi) was declared a National Monument in 1951.
  • Associated With: Cretaceous, Article text, age Cretaceous
    It originated during the Early Cretaceous rifting that led to the opening of the South Atlantic Ocean.
  • Caused By: Rifting, Article text, process Rifting
    It originated during the Early Cretaceous rifting that led to the opening of the South Atlantic Ocean.
View the Source
Wikidata: Brandberg Mountain
Wikidata Q897834, class allow-list match (w-wdresolver-0926)View the Source
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