Where rocks are parched into a dome,erosion produces a circular arrangement of rock layers outward from the center of the dome.

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This statement describes the formation of a geological feature known as a dome or anticline, which is characterized by the upward displacement of rock layers, resulting in a circular or elliptical pattern that spreads away from the center. Erosion can expose these layers and reveal the dome structure, which can be observed in various places around the world, such as the Black Hills of South Dakota or the mountains of Oman.

Where Rocks Are Parched into a Dome,erosion Produces a Circular