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The formations are separated by steep escarpments that dramatically interrupt the rolling hills.

Both are rife with karst topography and form long, flat plains.

The igneous and volcanic rocks extend at depth under the relatively thin veneer of Paleozoic sedimentary rocks and form the basal crust of the entire region.

A major unconformity in the region attests that the Ozarks was above sea level for several hundred million years from the time of the volcanism in the Precambrian until the mid-Cambrian with an erosionally produced relief of up to 1500 feet.

By the early 20th century, the Ozarks had become a generic term.

Geographic features include limestone and dolomite glades, which are rocky, desert-like area on hilltops.

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