The Catskill Delta: A regional summary of Devonian sedimentation
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The Catskill Delta consists of many lobes shed from the rising Acadia Mountains during the Devonian Period. The delta is composed of a combination of marine and non-marine sediments that accumulated along the western mountain front as the sediments developed along the shoreline of the Kaskaskia Sea. The book attempts to draw together the sedimentary processes which shaped the delta along the western Acadian Mountains.
Chapter 1 summarizes the Acadian Orogeny, its paleogeography including the...
Chapter 1 summarizes the Acadian Orogeny, its paleogeography including the...























