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Titlebook: Atlas of the Deep-Water Seabed; Ireland Boris Dorschel,Andrew J. Wheeler,Koen Verbruggen Book 2010 Springer Science+Business Media B.V. 201

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期刊全稱Atlas of the Deep-Water Seabed
期刊簡(jiǎn)稱Ireland
影響因子2023Boris Dorschel,Andrew J. Wheeler,Koen Verbruggen
視頻videohttp://file.papertrans.cn/165/164556/164556.mp4
發(fā)行地址Provides a unique insight into the deep-water seabed.Uses full colour imagery, including deep-sea photography.Illustrates and describes the morphological features along the continental margin of the N
圖書封面Titlebook: Atlas of the Deep-Water Seabed; Ireland Boris Dorschel,Andrew J. Wheeler,Koen Verbruggen Book 2010 Springer Science+Business Media B.V. 201
影響因子.Presented in an accessible, user-friendly format, this atlas sets out all the major features revealed during one of the largest ever deep-sea mapping campaigns. A unique insight into the morphology of the seabed along the continental margin of the North-East Atlantic, it reveals for the first time many features that have hitherto been hidden beneath the waves. It is organised both thematically and by region, with the sea floor and its biological hotspots – areas of high biodiversity such as seamounts – shown at a resolution not possible before. The atlas presents everything from submarine canyons to coral carbonate mounds, using digital terrain models generated from multibeam data and photographs taken from unmanned deep-water vehicles (ROVs).. .The full-colour imagery includes digital three-dimensional seabed maps as well as the photographs, with concise text descriptions and topic boxes used to highlight and explain the geological, biological and hydrographical features, in addition to their importance and context in the deep-sea realm. Alongside the wealth of background information and topic boxes on special highlights, extensive on-line resources link the reader to full data s
Pindex Book 2010
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Below the Irish Seabedthat Pangea started to split apart creating a series of rift valleys. Eventually, this rifting split all the way through the continental crust and a new ocean basin was formed with two new smaller continents on either side: the North Atlantic, Europe and North America respectively. The gross morphol
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Above the Irish Seabedmasses occurring at distinct water depth intervals. As a result of this stratification, the water in the ocean can flow in different directions at different depths. Individual water-masses can be characterised by their physical properties with the temperature and salinity (concentration of salt in s
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Escarpmentsting. The specific reasons why escarpments form on the seabed can be many fold (although faulting is no longer an active process on the Irish margin). Escarpments can form as a result of strong, slope-parallel bottom currents, or as the scars left following submarine (land)slides. In addition, they
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