Mozambique Belt
Quick Summary
The Mozambique Belt is a geological region in eastern Africa, primarily in Mozambique, that formed between 1 billion and 500 million years ago. It is part of the Pan-African orogenic belts, which are characterized by significant tectonic activity and mountain-building processes.1
This belt consists largely of highly metamorphosed gneisses, which are rocks that have been transformed by heat and pressure deep within the Earth's crust. These rocks were deformed by thrust faults, similar to those found in the Himalayas, indicating immense compressional forces. The Mozambique Belt extends from Ethiopia down through Kenya and Tanzania. In Madagascar, similar-aged gneisses were brought to the surface due to the extensional collapse of the orogenic belt.1
Ask Britannica AI about this topic
Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.
PrecambrianOccurrence and distribution of Precambrian rocks…Proterozoic age include the Limpopo, Mozambique, and Damaran belts in Africa, the Labrador Trough in Canada, and the Eastern Ghats belt in India. Several small relict areas, spanning a few hundred kilometres across, exist within or against Phanerozoic orogenic belts and include the Lofoten islands of Norway
Read More…Proterozoic age include the Limpopo, Mozambique, and Damaran belts in Africa, the Labrador Trough in Canada, and the Eastern Ghats belt in India. Several small relict areas, spanning a few hundred kilometres across, exist within or against Phanerozoic orogenic belts and include the Lofoten islands of Norway
Read More
PrecambrianOrogenic beltsThe Mozambique belt is one of the many Pan-African orogenic belts that formed in the period between 1 billion and 500 million years ago. It extends along the eastern border of Africa from Ethiopia to Kenya and Tanzania. It consists largely of highly metamorphosed, mid-crustal gneisses…
Read MoreThe Mozambique belt is one of the many Pan-African orogenic belts that formed in the period between 1 billion and 500 million years ago. It extends along the eastern border of Africa from Ethiopia to Kenya and Tanzania. It consists largely of highly metamorphosed, mid-crustal gneisses…
Read More