Slate shingles cover the Museum's central dome and roof. Slate makes good shingles because it splits easily into thin, durable sheets of solid rock. Why? It contains platelike mica minerals arranged in narrowly spaced layers.
Deformation related to faulting flattened the black fractured rock and its fossil at an angle to the original layers. You can see the result: a long, asymmetric trilobite.
Flowing rocks can be stretched into elongated forms. Compare this specimen and the other piece with the same number. Once, both of these trilobite fossils looked alike.