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     Fossils, some whole some fragmented, cemented by a spar matrix (crystalline calcite). Most of the fossils are crinoid stem fragments, but favositid (honeycomb) corals and stromatoporoids are also common.
     A close-up of the left side of the outcrop. Here we begin to see some of the fossils become visisble.

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Last Update: 7/18/00

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