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Shale is a fine-grained sedimentary rock that forms from the compaction of silt and clay-size mineral particles that we commonly call mud. This composition places shale in a category of sedimentary rocks known as mudstones.
The Utica Shale isopach shows a thickening in the southeastern part of the state. Fine-grained, argillaceous clastics of the Utica Shale were deposited with varying. regional thickness and lithofacies (Hiattt, 1985; Banas, 2011; Howell & Van der Pluijm, 1990, 1999; Sharma et al., 2003; Sharma, 2004; Rancourt, 2009).