Endogenic Forces and Evolution of Land forms

Endogenic Forces – Internal forces in detail

Endogenic forces a can be classified as slow movements (diastrophic) and sudden movements. Slow movements cause changes very gradually which might not be visible during a human lifetime.

Slow Movements (Diastrophic forces)

Diastrophic forces refer to forces generated by the movement of the solid material of the earth’s crust. All the processes that move, elevate or build portions of the earth’s crust come under diastrophism. Diastrophism includes:

1. orogenic processes involving mountain building through severe folding and affecting long and narrow belts of the earth’s crust.
2. epeirogenic processes involving uplift or warping of large parts of the earth’s crust.
3. earthquakes involving local relatively minor movements.
4. plate tectonics involving horizontal movements of crustal plates.

Slow movements can again be classified as vertical movements and horizontal movements.

Vertical Movements (Epeirogenic movements):

• Vertical movements are mainly associated with the formation of continents and plateaus. They are also called as Epeirogenic movements
• The broad central parts of continents are called cratons and are subject to epeirogeny.
• They do not bring any changes in the horizontal rock strata.
• While they cause upliftment of continent, they can also cause subsidence of continent.
• These movements are originated from the centre of the earth.

Horizontal Movements (Orogenic Movements):

• Horizontal forces acts on the earth’s crust from side to side to cause these movements.
• They are also known as orogenic movements (mountain building).
• They bring a lot of disruptions to the horizontal layer of strata leading to a large structural deformation of earth’s crust.
• They can be classified as forces of compression and forces of tension.

Forces of Compression:

• Forces of compression are the forces which push rock strata against a hard plane from one side or from both sides.
• The compressional forces lead to the bending of rock layers and thus lead to the formation of Fold Mountains.
• Most of the great mountain chains of the world like the Himalayas, the Rockies (N. America), the Andes (S. America), the Alps (Europe) etc are formed in this manner.

Forces of Tension:

• Forces of tension work horizontally, but in opposite directions.
• Under the operation of intense tensional forces, the rock stratum gets broken or fractured which results in the formation of cracks and fractures in the crust.
• The displacement of rock upward or downward from their original position along such a fracture is termed as faulting.
• The line along which displacement of the fractured rock strata take place is called as the fault line.
• Faulting results in the formation of well-known relief features such as Rift Valleys and Block Mountains. (E.g. Vindhya and Satpura Mountains)
• A rift valley is formed by sinking of rock strata lying between two almost parallel faults. (E.g. Valley of Nile, Rift valley of Narmada and Tapti )
• Rift valleys with steep parallel walls along the fault are called as Graben and the uplifted landmass with steep slopes on both sides are called as Horst.
• The very steep slope in a continuous line along a fault is termed as Escarpment.

Sudden Movements

Examples: Volcanoes and earth quakes.