By R. W. G. Carter, C. D. Woodroffe, Orson van de Plassche
This e-book assesses how coastlines switch and the way they've got advanced during the last few thousand years. It introduces the various most modern innovations in coastal morphodynamics, spotting that coasts boost via co-adjustment of strategy and shape. The authors learn specific sorts of coasts--deltas, estuaries, reefs, lagoons and polar coasts--in element with conceptual types built at the foundation of well-studied examples. as well as being a textual content for graduate-level scholars, it is a finished resource for geologists, engineers, environmental scientists, planners and coastal managers.
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Additional info for Coastal Evolution: Late Quaternary Shoreline Morphodynamics
For example, Young & Bryant (1992) consider that they have been able to identify an event, around 100000 years ago, which devastated the coast of southeast Australia. They believe this may have been caused by a massive submarine landslip in the Hawaiian Islands 105000 years BP, creating a group of tsunami waves which radiated circumferentially across the southwest Pacific. Young & Bryant are able to point to a wide range of what at first appear to be anomalous shore features, including rock channels across headlands, scoured and fluted rock platforms at a variety of levels, poorly-sorted high-level boulder deposits (some boulders weigh over 100 tonnes), and hummocky 'dump' deposits in sheltered areas.
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Marine ice-sheet decoupling as a mechanism for rapid, episodic sea level change; the record of such events and their influence on sedimentation. Sedimentary Geology, 70, 87-104. Andrade, C. (1992). Tsunami generated forms in the Algarve Barrier Islands. Science of Tsunami Hazards, 10, 21-4. F. (1987). Evidence for great Holocene earthquakes along the outer coast of Washington State. Science, 236, 942-4. F. L. (1992). A tsunami about 1000 years ago in Puget Sound, Washington. Science, 258, 1614-17.