The East African Rift is complex and one of the largest continental rifts on Earth; it extends from north from Lebanon to Ethiopia, running downwards though Kenya from the north to the south. It is slowly splitting the African continent in half.
There are fault-lines that stretch outward from this rift, reaching out across the face of African. One fault-line moves westward extending to Lake Nysas. There is one which runs to east-central Africa near the equator and Lake Victoria. The eastern fault-lines include the Great Rift Valley which runs from Syria in south-western Asia, to Mozambique in south-eastern Africa. Another fault-line lays in north-eastern Africa and extends to the Afar Triangle, part of a mid-ocean ridge. There is also a fault-line which runs between the Somalia and Nubia plates.
It's a Normal Fault.
Folds and faults are both formed from compression on opposite sides due to tectonic movement of the earth's crust. However, in a fold, the crust does not break, it simply is deformed in a curved pattern. In a fault, the rocks in the crust actually shatter, and movement is seen along a fault line, wheby rocks are displaced relative to each other.
Rift Valley
In between Africa and Madagascar there is a tectonic plate fault line this caused Madagascar to break away from Africa
A fault is where to tectonic plates meet but a fault zone is the area around a fault.
fault
A fault
Fault
A fault.
A *fault* is a slip or crack in the earths crust.
a fault
This is known as a fault. A fault is a fracture in the Earth's crust along which movement has occurred. Movement along faults can result in earthquakes.
Fault.
A crack in the Earth's crust that can lead to an earthquake is called a fault.
This is called a fault.== ==
Faults are made up of fractures in the earths crust. One side of the fault moves opposite of the other side.
A crack in the Earth's crust is a fracture where rocks have pulled apart, whereas a fault is a fracture where there has been movement along the fracture plane. In other words, a fault is a type of crack in the Earth's crust that has undergone displacement.