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  • 21 Aug, 2019

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Eratosthenes Seamount
The Eratosthenes Seamount or Eratosthenes Tablemount is a seamount in the Eastern Mediterranean, in the Levantine basin about 100 kilometres (60 mi) south of western Cyprus. Unlike most seamounts, it is a carbonate platform, not a volcano. It is a large, submerged massif, about 120 by 80 kilometres (75 by 50 mi). Its peak lies at the depth of 690 metres (2,300 ft) and it rises 2,000 metres (6,600 ft) above the surrounding seafloor, which is located at the depth of up to 2,700 metres (8,900 ft) and is a part of the Herodotus Abyssal Plain. It is one of the largest features on the Eastern Mediterranean seafloor.

In 2010 and 2012 the Ocean Exploration Trust's vessel EV Nautilus explored the seamount looking for shipwrecks. Three were found; two were Ottoman vessels from the 19th century and the third was from the 4th century BC. Such seamounts are considered to be ideal for the preservation of shipwrecks because at depths of around 600 metres (2,000 ft) the areas are not disturbed by trawlers or by sediments coming off land.

Oceanography

The Cyprus eddy is a sustained mesoscale eddy with a diameter about 100 kilometres (62 mi), regularly appearing above Eratosthenes Seamount. It was surveyed by oceanographic cruises notably in 1995, 2000, 2001 and 2009.

Geology

During the Messinian crisis, as the sea level in the Mediterranean dropped by about 1,500 metres (4,900 ft), the seamount emerged.

See also

References

  1. ^ Nations, Food and Agriculture Organization of the United; Mediterranean, General Fisheries Commission for the (2019-01-17). The State of Mediterranean and Black Sea Fisheries 2018. Food & Agriculture Org. p. 123. ISBN 978-92-5-131152-3. Archived from the original on 2023-02-17. Retrieved 2023-02-17. The Eratosthenes Seamount FRA (10 306 km2) is located in the eastern Mediterranean Sea, about 100 km south of Cyprus (GSA 25), between the Levantine platform to the south and the Cyprus margin to the north, near the subduction zone of the African plate
  2. ^ Libby, S.A.; Underhill, J.R. (2015-06-01). "Forward Modelling of Evaporite Kinematics around the Eratosthenes Seamount, Easternmost Mediterranean". 77th EAGE Conference and Exhibition 2015. Netherlands: EAGE Publications BV. doi:10.3997/2214-4609.201413146. ISBN 978-94-6282-146-0. Archived from the original on 2023-02-17. Retrieved 2020-12-06.
  3. ^ Staudigel, H.; Koppers, A.A.P. (2015). "Seamounts and Island Building". In Sigurdsson, H. (ed.). Encyclopedia of Volcanoes (2nd ed.). Amsterdam: Elsevier. p. 409. ISBN 978-0-12-385938-9.
  4. ^ Tudela, Sergi; Simard, François (2004). The Mediterranean Deep-sea Ecosystems: An Overview of Their Diversity, Structure, Functioning and Anthropogenic Impacts, with a Proposal for Their Conservation. IUCN. p. 34. ISBN 978-2-8317-0846-1. Directly adjacent to the Eratosthenes Seamount is a deep (approximately 2750 m) depression, part of the Herodotus abyssal plain.
  5. ^ Learn, Joseph Rapp (9 December 2017). "Wayfarers of the ancient world". New Scientist. Vol. 236, no. 3155. p. 12.
  6. ^ Hayes, D. R.; Zodiatis, G.; Konnaris, G.; Hannides, A.; Solovyov, D.; Testor, P. (June 2011). "Glider transects in the Levantine Sea: Characteristics of the warm core Cyprus eddy". OCEANS 2011 IEEE - Spain. IEEE. pp. 1–9. doi:10.1109/oceans-spain.2011.6003393. ISBN 978-1-4577-0086-6. S2CID 37545137.
  7. ^ Robertson, Alastair H.F. (1998). "FORMATION AND DESTRUCTION OF THE ERATOSTHENES SEAMOUNT, EASTERN MEDITERRANEAN SEA, AND IMPLICATIONS FOR COLLISIONAL PROCESSES" (PDF). Proceedings of the Ocean Drilling Program, Scientific Results. 160: 681. Archived (PDF) from the original on 2023-02-17. Retrieved 2020-11-05.


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