The Appalachian Mountains are a good example of anticlines and synclines.

Name: The Appalachian Mountains are a good example of anticlines and synclines.
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The Appalachian Mountains are a prime example of an orogenic belt that was formed by the compressional forces of tectonic plates. The mountain range features a series of fold structures, including anticlines and synclines, which are created by the upward and downward bending of rock layers.

The Appalachian Mountains Are a Good Example of Anticlines and Synclines