The Appalachian Mountains in North America are an example of old fold mountains. They were formed over 480 million years ago through the collision of tectonic plates and have since undergone erosion and weathering, giving them their characteristic gentle slopes and rounded peaks.
Old fold mountains are characterized by their folded and deformed rock layers, which have been uplifted and eroded over millions of years. They often exhibit steep slopes, rugged terrain, and high elevations. Examples of old fold mountains include the Appalachian Mountains in North America and the Caledonian Mountains in Europe.
Alps, Himalaya
Old fold mountains are mountains that were formed millions of years ago through the process of folding and faulting of the Earth's crust. These mountains have undergone significant erosion and are typically characterized by rounded peaks and deep valleys. Young fold mountains, on the other hand, are mountains that are still actively being formed through tectonic processes, such as the collision of tectonic plates. These mountains tend to have sharp, rugged peaks and steep slopes.
Fold mountains are formed when tectonic plates collide, causing the Earth's crust to crumple and fold. An example of a fold mountain range is the Himalayas in Asia, which were formed by the collision of the Indian and Eurasian plates.
Yes, there are fold mountains in the Caribbean. The islands in the Caribbean were formed by tectonic plate movements that led to the creation of fold mountains. The Greater Antilles, including islands like Cuba, Hispaniola, and Jamaica, have mountain ranges that are examples of fold mountains in the region.
young fold mountains are like Himalayas, the Alps and man other.
Old fold mountains are characterized by their folded and deformed rock layers, which have been uplifted and eroded over millions of years. They often exhibit steep slopes, rugged terrain, and high elevations. Examples of old fold mountains include the Appalachian Mountains in North America and the Caledonian Mountains in Europe.
the western cordilleras are young fold mountains, while the appalachians are old fold mountains.
Caledonian and Hercynian
the Himalayasi need a example of fault block mountains(The himalayas are NOT fault block mountains , they are fold mountains.)
Old fold mountains are mountains that were formed millions of years ago through the process of folding and faulting of the Earth's crust. These mountains have undergone significant erosion and are typically characterized by rounded peaks and deep valleys. Young fold mountains, on the other hand, are mountains that are still actively being formed through tectonic processes, such as the collision of tectonic plates. These mountains tend to have sharp, rugged peaks and steep slopes.
Alps, Himalaya
One of the features of young fold mountains is that these are formed at destructive collision of tectonic plate boundaries. The Earth's crust are pushed to the surface therefore forming a series of fold mountains.
Folded (fold) mountains are the most common.
An example of an collision zone would be types of fold mountains such as the Himalayas.
The appalachain mountains are fold mountains
the mountains in northern Ethiopia's fold mountains