Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Karoo Supergroup

Named Rock Formations and Groups

The Karoo Supergroup is the most widespread stratigraphic unit in Africa south of the Kalahari Desert, made up predominantly of shales and sandstones that accumulated over roughly 120 million years from the Late Carboniferous through the Early Jurassic. It covers nearly two-thirds of present-day southern Africa, encompassing all of Lesotho, nearly all of South Africa's Free State province, and large parts of the Eastern Cape, Northern Cape, Mpumalanga and KwaZulu-Natal provinces, with further outcrops in Namibia, Eswatini, Zambia, Zimbabwe, Malawi and other former Gondwana localities. Its sedimentary layers reach a maximum cumulative thickness of 12 kilometers, with the overlying basaltic lavas of the Drakensberg Group adding at least another 1.4 kilometers on top. The Supergroup is internationally renowned for its fossil record of plants, insects, fish and diverse tetrapods, especially therapsids, along with temnospondyl amphibians, dinosaurs and trace fossils, and its biostratigraphy serves as the international standard for correlating nonmarine strata from the Permian through the Jurassic worldwide. This entity documents the Karoo Supergroup specifically as a geological formation, a vast southern African sedimentary and volcanic sequence.

Connections

Caused By

Source Karoo Supergroup (Wikipedia)

In Discipline

Source Karoo Supergroup (Wikipedia)
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Sources
Karoo Supergroup (Wikipedia)
  • In Discipline: Stratigraphy, Lead paragraph
    The Karoo Supergroup is the most widespread stratigraphic unit in Africa south of the Kalahari Desert
  • Caused By: Sedimentation, Lead section (caused-by Sedimentation)
    The supergroup consists of a sequence of units, mostly of nonmarine origin, deposited between the Late Carboniferous and Early Jurassic, a period of about 120 million years.
View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.