GEOL-106_Lecture_[08]_Paleozoic_Earth

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Oct 30, 2023

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PALEOZOIC EARTH HISTORY GEOL106 Chapter 20
251 Ma 542 Ma Paleozoic
Introduction In 1815, William Smith, a canal builder, published the world’s first geologic map. His hand-painted map represented over 20 years of work.
Introduction England is rich in geologic history. Development of geology proceeded rapidly with the naturalists of the 19th century. The Paleozoic history is well represented there, involving several episodes of mountain building and sea level changes, mostly related to plate tectonics and glaciation.
Continental Architecture: Cratons and MobileBelts Most continents consist of two major components: 1. relatively stable craton over which epeiric seas transgressed and regressed 2. surrounded by mobile belts in which mountain building took place Fig. 20.1, p. 505
Continental Architecture: Cratons and MobileBelts Epeiric seas – shallow seas covering part of the craton Mobile belts – elongate areas of mountain building, primarily created during plate convergence Fig. 20.1, p. 505
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