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Titlebook: Geology of Holocene Barrier Island Systems; Richard A. Davis Book 1994 Springer-Verlag Berlin Heidelberg 1994 Barrier Islands.Coast.Coasta

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发表于 2025-3-21 17:46:39 | 显示全部楼层 |阅读模式
书目名称Geology of Holocene Barrier Island Systems
编辑Richard A. Davis
视频video
图书封面Titlebook: Geology of Holocene Barrier Island Systems;  Richard A. Davis Book 1994 Springer-Verlag Berlin Heidelberg 1994 Barrier Islands.Coast.Coasta
描述Barrier islands represent a complex coastal system that includes a number of different sedimentary depositional environments; nearshore zone, beach, dunes, washover fans, marshes, tidal flats, estuaries, lagoons, and tidal inlets. The morphodynamics of these fragile coastal systems provide a further complication to this coastal type. Although barrier islands comprise only 15% of the world‘s coastline, they have received a far greater proportion of attention from the scientific and engineering community, and more recently, from coastal managers and environmentalists. Modern barrier islands are arguably the most expensive and most vulnerable of all coastal environments. Pressure from developers for residential, industrial, and recreational development has caused most of our barriers to become significantly impacted by human activity, especially over the past few decades. These pres­ sures have led to extensive preservation of natural barriers through efforts from all levels of government and also by private organizations. Governments have also formed coastal management programs that help to control any future de­ velopment with the intent being to keep human activity compatible with
出版日期Book 1994
关键词Barrier Islands; Coast; Coastal Geology; Küstengeologie; Sediment; Sedimentologie; Stratigraphie; Stratigra
版次1
doihttps://doi.org/10.1007/978-3-642-78360-9
isbn_softcover978-3-642-78362-3
isbn_ebook978-3-642-78360-9
copyrightSpringer-Verlag Berlin Heidelberg 1994
The information of publication is updating

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发表于 2025-3-21 21:35:08 | 显示全部楼层
Digital Design from the VLSI Perspectivehis condition combined with the broad range in tidal prism and the human influence have produced a unique coastal complex. Another important aspect of this coast is the rapid change which commonly takes place under such pronounced low-energy conditions.
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Barriers of the Florida Gulf Peninsula,his condition combined with the broad range in tidal prism and the human influence have produced a unique coastal complex. Another important aspect of this coast is the rapid change which commonly takes place under such pronounced low-energy conditions.
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Book 1994unes, washover fans, marshes, tidal flats, estuaries, lagoons, and tidal inlets. The morphodynamics of these fragile coastal systems provide a further complication to this coastal type. Although barrier islands comprise only 15% of the world‘s coastline, they have received a far greater proportion o
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,Barrier Island Systems — a Geologic Overview,me that do not. It is further complicated by such variables a sea level change, sediment supply and the relative influence of wave- and tide-dominated processes..Fortunately, there is also a great deal of predictability to barrier island geology and stratigraphy. The nature and relative positions of
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The Outer Banks of North Carolina, microtidal (0.9 m tidal range) high wave energy (1.7m average wave height) hydrographic setting. Holocene sedimentation and coastal evolution have been a function of five major depositional processes: (1) eustatic sea-level rise and barrier-shoreline transgression; (2) lateral tidal inlet migration
发表于 2025-3-23 02:52:08 | 显示全部楼层
Texas Barriers,a dominant westerly flow in the northern Gulf of Mexico (LeBlanc and Hodgson 1959). This westerly flow and the regional distribution of barrier islands led some early workers to conclude that Texas barrier islands were deposited by littoral drift reworked from the Mississippi River. More recent geol
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