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Seabed

The seabed (also known as the seafloor, sea floor, or ocean floor) is the bottom of the ocean. At the bottom of the continental slope is the continental rise, which is caused by sediment cascading down the continental slope. The seabed has been explored by submersibles such as Alvin and, to some extent, scuba divers with special apparatuses. The process that continually adds new material to the ocean floor is seafloor spreading and the continental slope. The acronym "mbsf" meaning "metres below the seafloor" is a convention used for depths below the seafloor.

See also

References

  1. ^ Flood, Roger D.; Piper, D.J.W., Klaus, A., and Peterson, L.C. (Eds.) (1997). "PREFACE: DEPTH BELOW SEAFLOOR CONVENTIONS". Proceedings of the Ocean Drilling Program, Scientific Results 155: 3. "we follow Ocean Drilling Program (ODP) meters below seafloor (mbsf) convention". 
  2. ^ Parkes, R. John; Henrik Sass (2007). Sulphate-reducing Bacteria Environmental and Engineered Systems Edited by Larry L. Barton University of New Mexico. Cambridge University Press. pp. 329–358. doi:10.1017/CBO9780511541490.012. http://ebooks.cambridge.org/chapter.jsf?bid=CBO9780511541490&cid=CBO9780511541490A018. Retrieved 11 June 2010. "metres below the seafloor (mbsf)" 

External links

Look up seabed in Wiktionary, the free dictionary.

 
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