Mountains
are formed in two ways. When the tectonic plates move, they collide against
each other. When the heavy oceanic part of the plate collides with the
continental part, it submerges below it. The Andes, for instance, were formed
in this way. The other way is when two continents collide with the point of
contact and fold up steeply. The Himalayas or the Alps were formed in this way
around 35 million years ago and are counted among the ‘young’ mountains of the
world. Old mountains such as Black Forest or the Harz mountains, are lower
ranges because peaks have been worn down by rain, ice, and wind over time.
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