Major mountain belts on the earth are generally colored orange to red to grey, rise high above the land around them.
Major mountain belts on the earth are generally colored orange to red to grey, rise high above the land around them and are located around the Pacific Ocean older than smaller mountain belts because they have had enough time to grow large over 10 km high made of granite because it is low density and allows for maximum growth.
Some of the major mountain belts on the Earth are as follows;
Fossil evidence and age dating by means of Carbon-dating indicate the rounded hills of the Appalachian and Ozark Mountains are some of the oldest mountains in the United States.
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