Andean-type mountain building involves the convergence of two oceanic plates. Given Statement are true.
The Andes Mountains are a chain of extremely high plateaus topped by even higher peaks that form an unbroken rampart stretching 5,500 miles (8,900 kilometers) from South America's southernmost tip to the continent's northernmost coast on the Caribbean.
The Andes were formed by tectonic activity, which occurs when one plate (oceanic crust) subducts beneath another plate (continental crust). It is unusual to find such a high mountain chain in a subduction zone setting, which emphasizes the importance of determining when and how it occurred.
Mountain formations are classified under the following categories:
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