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The Appalachian Mountains were formed, or more specifically started forming, some 3-400 million years ago during the Ordovician Period by a process of folding and thrust faulting when an oceanic plate collided with the boundary that is the Appalachian area. Though it had always existed at a plate boundary, until this tectonic shift the Appalachian area had been a calm one - called a "passive margin."

To better understand thrust faulting, consider this: imagine a short stack of paper laying flat on a table. If you were to hold one side of the stack firmly to the table, and then push against the opposite edge with your free hand, the pages would crumple back and upwards, or "fold" into a series of peaks and valleys. In this scenario, some of the pages from the bottom now may overlap or jut above pages from the top in an odd, almost unnatural way.

In this analogy, your steady hand and the stack of paper are that active plate boundary of what would later be called the North American Plate, and your free hand is the oceanic plate that collided with it. The folding, faulted paper is - you guessed it - the Appalachian Mountains.

At the time of this collision, which took tens of millions of years longer to happen than it did to explain, the supercontinent of Pangea was also formed. At their newest, it is believed the Appalachians were at least as tall as the Rockies, if not larger. Over the last 300 million years, however, the once rugged peaks of relatively "soft" stone (limestone in particular) were eroded to form the ridges and valleys so characteristic of the mountains we know today.
The Appalachian Mountains are nearly 500 million years old. They were formed by a shift in the tectonic plates in that area, creating a new subduction zone.

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Q: How were the Appalachian Mountains formed?
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