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The seabed (also known as the seafloor, sea floor, ocean floor, and ocean bottom) is the bottom of the ocean. All floors of the ocean are known as 'seabeds'. The structure of the seabed of the global ocean is governed by plate tectonics. Most of the ocean is very deep, where the seabed is known as the abyssal plain. … Meer weergeven
Most of the oceans have a common structure, created by common physical phenomena, mainly from tectonic movement, and sediment from various sources. The … Meer weergeven
Each region of the seabed has typical features such as common sediment composition, typical topography, salinity of water layers … Meer weergeven
• Bottom trawling – Fishing method for fishing trawlers
• Demersal fish – Fish that live and feed on or near the … Meer weergevenSediments in the seabed vary in origin, from eroded land materials carried into the ocean by rivers or wind flow, waste and decompositions of sea creatures, and precipitation … Meer weergeven
Seabed topography (ocean topography or marine topography) refers to the shape of the land (topography) when it interfaces with the … Meer weergeven
Exploration
The seabed has been explored by submersibles such as Alvin and, to some extent, Meer weergeven• Roger Hekinian: Sea Floor Exploration: Scientific Adventures Diving into the Abyss. Springer, 2014. ISBN 978-3-319-03202-3 (print); ISBN 978-3-319-03203-0 (eBook) Meer weergeven
Wikipedia-tekst onder CC-BY-SA-licensie Oceanische spreiding - Wikipedia
WEBOceanische spreiding is het proces dat volgens de theorie van platentektoniek plaatsvindt op divergente grenzen (voornamelijk mid …
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Ocean floor | Britannica
Seafloor Mapping - NOAA Ocean Exploration
WEBOnly slightly more than 23% of the seafloor has been mapped in great detail, and even less has been explored with underwater cameras or submersibles. Mapping the seafloor is the first step in exploring the …
Seabed - Simple English Wikipedia, the free encyclopedia
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