At destructive collision plate boundaries eg Alps (collision of African and Eurasian plates)
fold mountains form
Volcanic activity can form fold mountains or block mountains. Fold mountains are formed when tectonic plates collide. Block mountains are formed when fault block shifts.
Fold mountain or mountain chains are formed by the collisions between continental plates.
types of fold mountains are.1.symmetricla fold2.asymetrical fold3.over fold4.recumbent fold5.over thrust fold
Two kinds of mountains are volcanic mountains, which form from volcanic activity, and fold mountains, which form from tectonic plate collisions causing the Earth's crust to fold and create mountain ranges.
Volcanic activity can form fold mountains or block mountains. Fold mountains are formed when tectonic plates collide. Block mountains are formed when fault block shifts.
By the means of plate tectonics at a zone of collision fold mountains are formed. At a zone of collision two continental plates collide and since they are of equal densities no subduction will take place but the two will collide and crumble and fold to form fold mountains.
The appalachain mountains are fold mountains
young fold mountains are like Himalayas, the Alps and man other.
The Himalayan mountain range of Tibet was formed when the Indian Plate and the Eurasian Plate collided nearly 50 million years ago. It is the world's current mountain range and includes the world's tallest mountain, Mount Everest.
The five basic types of mountains in the world are fold mountains, fault-block mountains, dome mountains, volcanic mountains, and plateau mountains. Fold mountains form through the folding of rock layers, fault-block mountains result from the movement of tectonic plates, dome mountains are created by the uplifting of rock layers, volcanic mountains form from volcanic activity, and plateau mountains are elevated flat surfaces.
The Jura mountains in France, and the Zagros mountains in Iran & Iraq are both examples of fold mountains.