By Eric Bird
This precise richly-illustrated account of the landforms and geology of the world’s coasts, offered in a country-by-country (state-by-state) series, assembles an unlimited quantity of information and photographs of an endangered and more and more populated and constructed landform. a world panel of 138 coastal specialists offers info on “what is where” on every one quarter of coast, including motives of the landforms, their evolution and the alterations happening on them. in addition to delivering information at the coastal gains of every kingdom (state or county) the compendium can be utilized to figure out the level of specific gains alongside the world’s coasts and to enquire comparisons and contrasts among a number of international areas. With greater than 1440 colour illustrations and pictures, it's relatively important as a resource of data ahead of gaining knowledge of or simply vacationing a region of coast. References are supplied to the present literature on coastal evolution and sea coast changes.
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Extra resources for Encyclopedia of the World's Coastal Landforms
Example text
C. de Andrei Selivanov† Yurii Shuisky Physical Geography Department Mechnikov’s National University of Odessa 2 Dvoryanskaya St. net Scott Smithers School of Earth and Environmental Sciences Faculty of Science and Engineering James Cook University Queensland 4810 Australia Rodman E. ee J. Turenne Centre d’Ile-de-France 32, avenue Henri Varagnat 93143 Bondy cedex France C. R. B. 1017 Uyo, Akwa Ibom State Nigera Don Vermeer Louisiana State University Baton Rouge, LA 70803 USA H. bn Dai Zhijun State Key Lab.
In that area permafrost, with its included ice wedges, affects the character and amount of coastal erosion. In the zone of discontinuous permafrost, coastline erosion frequently exposes relict permafrost patches. Along the north coast of Alaska, permafrost that formed during lower sea stands is present in nearshore, sub-sea locations. Except for a few glaciers present in the Brooks Range of northern Alaska, glaciers today are confined to southern Alaska where many still impact the coastline. Most of the Alaska coast, even during the period of maximum glacial extent, was untouched directly by glaciers.
Southeast Alaska, tectonically active since the early Palaeozoic, is presently being uplifted at one of the fastest rates in the world (Skelkregg 1974–1976). 5 cm/year, a rate that helps account for the presence of glaciomarine deposits at heights of 230 m above sea level near Juneau. Some of this uplift is thought to be the result of rebound that occurs with deglaciation. Although general rebound is still occurring, localised rebound is partially responsible for a rapid uplift that is being recorded near retreating glaciers (Hicks and Shofnos 1965).