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One clue that a mountain is young is if it has sharp, jagged peaks and steep slopes. This indicates that the mountain has undergone recent tectonic activity, such as uplift or faulting. In contrast, an old mountain would have more rounded peaks and gentle slopes due to erosion over time.

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What are the names of young fold mountains of world?

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.


How can we tell whether a fold mountain is young or old?

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.


What are the physical features of young fold mountain?

The features of a young fold mountain are: Distinctive layers of rock that lie slightly slanted; High, then low points of the mountain range; They run along a plate boundary


Mountains similar to those in Greenland and western Europe?

Some mountain ranges similar to those in Greenland and Western Europe include the Rocky Mountains in North America, the Himalayas in Asia, and the Alps in Europe. These mountain ranges are known for their rugged and towering peaks, as well as for being geologically young and active. They also provide habitats for unique flora and fauna adapted to high altitudes and cold climates.


How would you tell the age of a mountain?

One method is to examine the rock composition and structure of the mountain to determine its age. Another way is to study the erosion patterns on the mountain, as older mountains tend to have more rounded features due to weathering over time. Additionally, scientists can use radiometric dating techniques on rocks found on the mountain to estimate its age.

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