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The large anticlines form the fold mountain and the dome mountains. This is usually as a result of jointing, folding and faulting.

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Large anticlines form ridge-like mountains with a U or V-shaped profile. These mountains typically have an elongated shape due to the folding of rock layers, with the oldest rocks found in the center of the fold. Examples include the Appalachian Mountains in North America and the Zagros Mountains in the Middle East.

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Q: Large anticlines form what kind of mountains?
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