In structural geology, a dome is a deformational feature consisting of symmetrically-dipping anticlines; their general outline on a geologic map is circular or oval. The strata in a dome are upwarped in the center; if the top of a dome is eroded off, the result will be a series of concentric strata that grow progressively older from the outside-in, with the oldest rocks exposed at the center. Many geologic domes are too large to be appreciated from the surface, and are apparent only in maps. Well-known regional structural domes include the Llano Uplift and the Ozark Dome.[1]
Localized domes may be formed when magma forms a shallow intrusion warping the overlying strata. An example would be the laccolith domes of the Henry Mountains of southeastern Utah. Salt domes are formed above a diapiric intrusion of low density evaporite rocks.
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