At destructive collision plate boundaries eg Alps (collision of African and Eurasian plates)
At a convergent boundary
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.
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 mountains
The appalachain mountains are fold mountains
the mountains in northern Ethiopia's fold mountains
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 large anticlines form the fold mountain and the dome mountains. This is usually as a result of jointing, folding and faulting.
The MacGillycuddy's Reeks in County Kerry are a prominent range of fold mountains in Munster. These mountains include Ireland's highest peak, Carrauntoohil. The mountains were formed by the collision of tectonic plates, leading to the folding and uplifting of rock layers.
young fold mountains are like Himalayas, the Alps and man other.
The main fold mountains found in the Caribbean region are the Greater Antilles, which include mountains like the Sierra Maestra in Cuba, the Blue Mountains in Jamaica, and the Cordillera Central in the Dominican Republic. These mountains were formed by the tectonic activity between the North American and Caribbean plates.