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Titlebook: Coastal Sedimentary Environments; Richard A. Davis Book 1985Latest edition Springer-Verlag New York Inc. 1985 Coast.Küste.Sediment.Sedimen

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發(fā)表于 2025-3-21 17:11:12 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Coastal Sedimentary Environments
編輯Richard A. Davis
視頻videohttp://file.papertrans.cn/229/228751/228751.mp4
圖書封面Titlebook: Coastal Sedimentary Environments;  Richard A. Davis Book 1985Latest edition Springer-Verlag New York Inc. 1985 Coast.Küste.Sediment.Sedimen
描述The zone where land and sea meet is composed of a variety of complex environments. The coastal areas of the world contain a large percentage of its population and are therefore of extreme economic importance. Industrial, residential, and recreational developments, as well as large urban complexes, occupy much of the coastal margin of most highly developed countries. Undoubtedly future expansion in many undeveloped maritime countries will also be concentrated on coastal areas. Accompanying our occupation of coasts in this age of technology is a dependence on coastal environments for transportation, food, water, defense, and recreation. In order to utilize the coastal zone to its capacity, and yet not plunder its resources, we must have extensive knowledge of the complex environments contained along the coasts. The many environments within the coastal zone include bays, estuaries, deltas, marshes, dunes, and beaches. A tremendously broad range of conditions is represented by these environments. Salinity may range from essentially fresh water in estuaries, such as along the east coast of the United States, to extreme hypersaline lagoons, such as Laguna Madre in Texas. Coastal environm
出版日期Book 1985Latest edition
關(guān)鍵詞Coast; Küste; Sediment; Sedimentation; biogeochemistry; chemistry; energy; environment; estuaries; evolution;
版次2
doihttps://doi.org/10.1007/978-1-4612-5078-4
isbn_softcover978-1-4612-9554-9
isbn_ebook978-1-4612-5078-4
copyrightSpringer-Verlag New York Inc. 1985
The information of publication is updating

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Estuaries,vergence in our level of understanding? Most inquiry has centered on human needs in an effort to resolve competing demands for use of estuaries, e.g., for shipping and waste disposal as opposed to use as a recreational outlet or food sources. Far more effort has gone into detailed engineering, fishe
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Intertidal Flats and Intertidal Sand Bodies,oping features within this interval that are exposed at low-tide stage. Intertidal sand bodies represent linear shoals or bars deposited by tidal currents that occur in the lower portions of intertidal flats and the nonvegetated intertidal zone. They are exposed also at low tide, in contrast to tida
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Coastal Dunes, of Coos Bay, Oregon (Figure 5-1), the southern end of Lake Michigan (Figure 5-2), and the Cape Cod dune fields southeast of Provincetown (Figure 5-3) and on Sandy Neck (Figure 5-4) are just a few outstanding examples. Smaller sand dune accumulations are an integral part of almost all depositional c
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Beach and Nearshore Zone, The changes to which beaches are subjected may be seasonal or longer in duration; they may be as short as a single tidal cycle or even occur from one crashing wave to the next. Because of the beauty and romance of the beach environment, as well as its scientific interest, literally thousands of res
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Modeling Coastal Environments, profile or map forms a geometric model that provides a framework for more complex theoretical models. Geologic processes that operate within the coastal framework can be reproduced with physical models, such as wave tanks, or with various types of statistical and mathematical models. The effects th
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Book 1985Latest editionmarshes, dunes, and beaches. A tremendously broad range of conditions is represented by these environments. Salinity may range from essentially fresh water in estuaries, such as along the east coast of the United States, to extreme hypersaline lagoons, such as Laguna Madre in Texas. Coastal environm
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