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Terrestrial and Shallow Marine Geology of the Bahamas and Bermuda 1-1-001-322-4330-322 reflecting changes in climate and

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Description

reflecting changes in climate and regional tectonism

widespread degradation of stream channels in the southwest United States beginning in the late 1800s

occupies a tectonically active half-graben and contains hundreds of meters of Quaternary sediment

The main lessons we learn from the opposing ideas of Werner and Marx on one side and Hutton and Smith on the other are: 1

paleogeographic reconstruction of Late Quaternary landscapes

Terrestrial and Shallow Marine Geology of the Bahamas and Bermuda 1-1-001-322-4330-322 reflecting changes in climate andEditors: H. Allen Curran and Brian White Buy the e book(not available in print) The authors review the current knowledge of the Quaternary geologic history of the Bahaman Archipelago and Bermuda, an area with unique terranes for the study of carbonate rocks, sediments, and environments. The exposed stratigraphic sequences of the islands reveal much about the history of global sea level changes during Quaternary time. The focus is on interpretation of

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