Large igneous provinces

The Drakensberg (Zulu: uKhahlamba, Sotho: Maloti, Afrikaans: Drakensberge) is the eastern portion of the Great Escarpment, which encloses the central Southern African plateau. The Great Escarpment reaches its greatest elevation – within the border region of South Africa and Lesotho.

mountain range in East Africa

extensive geographical region, covering most of the eastern, southern and central portions of Brazil

plateau in Washington, Oregon, and Idaho in the United States

large igneous province in Siberia

large igneous province located on the Deccan Plateau

oceanic plateau in the southern Indian Ocean

massive volcanic formation resulting from flood basalt eruptions

flood basalt igneous province in south-western China

oceanic plateau in the north-west Pacific Ocean

large igneous province in South America and Africa

huge oceanic plateau located in the southwestern Pacific Ocean, north of the Solomon Islands

accumulation of indigenous rocks

oceanic plateau in the North Atlantic Ocean

Largest continental igneous province on Earth

large igneous province in the North Atlantic, centered on Iceland

continental flood basalt province in the Western United States

oceanic plateau in the Southern Ocean

The Karoo and Ferrar large igneous provinces (LIPs), in Southern Africa and Antarctica respectively, collectively known as the Karoo-Ferrar, Gondwana, or Southeast African LIP, are associated with the initial break-up of the Gondwana supercontinent at . Its flood basalt mostly covers South Africa and Antarctica, but portions extend further into southern Africa and into South America, India, Australia and New Zealand.