Mountain ranges formed by terrane accretion are often associated with continent-continent convergent boundaries, such as the Appalachian/Caledonide Mountains and the Andes Mountains.
Mountain ranges formed due to terrane accretion are often associated with continent-continent convergent boundaries. A prime example of this type of mountain formation is the Appalachian/Caledonide Mountains, which resulted from multiple tectonic events over millions of years. The Andes Mountains in South America are an example of a volcanic mountain range formed from a volcanic arc at an ocean-continent convergent boundary.
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