Flattop Mountain, a Synclinal Mountain

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Section across the Livingston and Lewis ranges, with the Flattop Mountain, a synclinal mountain, and Chief Mountain, a remnant of an overthrust fault block. The strata are more complexly folded than is here shown.

Source

Amadeus W. Grabau A Textbook of Geology (Boston: D.C. Heath & Co., 1920) 599

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