The Stratigraphy of the Great Unconformity
The Great Unconformity is a major stratigraphic discontinuity in the geologic record that represents an interruption in the deposition of sedimentary rocks. It is a feature of considerable importance in the stratigraphic interpretation of sedimentary basins and is found around the world in many different geological settings. The Great Unconformity can represent millions of years of missing geologic time and has been the subject of numerous studies. The Great Unconformity was first described in the late 19th century by the American geologist James Hall. He noticed that there was an unconformity between the Cambrian and Precambrian strata in the Appalachian Mountains. Hall initially used the term ‘Great Unconformity’ to describe the unconformity in the Appalachians (Hall, 2019). The Great Unconformity is now recognized as the most significant unconformity in the geologic record and has been used to divide the Paleozoic and Precambrian eras (Geology.com, 2020). Cont…
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