The fold mountains that formed less than about 25 million years back are considered young
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These regions may be prone to Earthquakes and volcanic eruptions because the crust of the Earth is unstable
Fold and thrust mountain ranges can be found at convergent plate boundaries, where two tectonic plates collide. Examples of fold and thrust mountain ranges include the Himalayas in Asia and the Rocky Mountains in North America.
Aravalli range are the oldest fold mountain ranges in India
because it is a fold mountain...some humor is good in life.:)
Fold mountains typically form at convergent plate boundaries, where tectonic forces cause the Earth's crust to fold and uplift. Examples of fold mountain ranges include the Himalayas, Andes, Alps, and Rockies.
Mountain ranges are typically associated with convergent plate boundaries, where two tectonic plates collide. The collision forces the plates to crumple and fold, leading to the uplift of rock layers and the formation of mountain ranges.
A lifted mountain is called a "fold mountain." This type of mountain is formed when two tectonic plates push against each other, causing the Earth's crust to bend and fold, creating elevated mountain ranges.
The Himalayas is considered one of the youngest fold mountain ranges in the world. It was formed by the collision of the Indian tectonic plate with the Eurasian plate, resulting in the uplift of the Himalayan mountain range.
There are no young fold mountains in Africa because the continent lacks active tectonic plate boundaries that would create the necessary conditions for mountain-building processes. Most of Africa's mountains formed millions of years ago and have since eroded down, leaving behind older mountain ranges like the Atlas Mountains and the Drakensberg Mountains.
Some examples of young fold mountains include the Himalayas in Asia, the Andes in South America, and the Rockies in North America. These mountain ranges are still actively being uplifted through tectonic processes, resulting in their rugged, steep topography.
The Great Dividing Range is a major fold mountain range in Australia. It runs parallel to the eastern coast and influences the climate and geography of the region.
Folded mountain ranges form when tectonic plates collide, causing the crust to fold and buckle due to compressional forces. Over time, these folds are uplifted to create mountain ranges with ridges and valleys. Examples include the Himalayas and the Appalachians.
The presence of sharp, rugged peaks and deep, narrow valleys indicates a young fold mountain, formed relatively recently. In contrast, smooth, rounded peaks and wider valleys suggest an older fold mountain that has been eroded over time. Additionally, studying the surrounding geological features and sedimentary layers can help determine the age of a fold mountain.