World Library  
Flag as Inappropriate
Email this Article

Gulf of Izmit

Article Id: WHEBN0016244678
Reproduction Date:

Title: Gulf of Izmit  
Author: World Heritage Encyclopedia
Language: English
Subject: Sea of Marmara, Turkish Navy, Argonautica
Collection:
Publisher: World Heritage Encyclopedia
Publication
Date:
 

Gulf of Izmit

"Propontis" redirects here. For the Liberian cargo ship, see SS Propontis.
Sea of Marmara
Coordinates

40°41′12″N 28°19′7″E / 40.68667°N 28.31861°E / 40.68667; 28.31861Coordinates: 40°41′12″N 28°19′7″E / 40.68667°N 28.31861°E / 40.68667; 28.31861

Basin countries Turkey
Surface area 11,350 km2 (4,380 sq mi)
Average depth 494 m (1,621 ft)
Max. depth 1,370 m (4,490 ft)
Water volume 3,378 km3 (810 cu mi)
Islands Adalar, etc.
Settlements Istanbul, Bursa, Çanakkale, Kocaeli, Tekirdağ, Sakarya and their towns.



The Sea of Marmara /ˈmɑrmərə/ (Turkish: Marmara Denizi, Greek: Θάλασσα του Μαρμαρά), also known as the Sea of Marmora or the Marmara Sea, and in the context of classical antiquity as the Propontis (Greek: Προποντίς), is the inland sea, entirely within the borders of Turkey that connects the Black Sea to the Aegean Sea, thus separating Turkey's Asian and European parts. The Bosphorus strait connects it to the Black Sea and the Dardanelles strait to the Aegean. The former also separates Istanbul into its Asian and European sides. The Sea has an area of 11,350 km² (280 km x 80 km)[1] with the greatest depth reaching 1,370 m.

Geography

The surface salinity of the sea averages about 22 parts per thousand, which is slightly greater than that of the Black Sea but only about two-thirds that of most oceans. However, the water is much more saline at the sea-bottom, averaging salinities of around 38 parts per thousand — similar to that of the Mediterranean Sea. This high-density saline water, like that of the Black Sea itself, does not migrate to the surface. Water from the Susurluk, Biga (Granicus) and Gonen Rivers also reduces the salinity of the sea, though with less influence than on the Black Sea. With little land in Thrace draining southward, almost all of these rivers flow from Anatolia.

There are two major island groups known as the Princes' and Marmara islands (including Avşa and Paşalimanı).

The south coast of the sea is heavily indented, and includes the Gulf of Izmit (Turkish: İzmit Körfezi), the Gulf of Gemlik (Turkish: Gemlik Körfezi) Gulf of Bandırma (Turkish: Bandırma Körfezi) and the Gulf of Erdek (Turkish: Erdek Körfezi). During a storm on December 29, 1999, the Russian oil tanker Volgoneft broke in two in the Sea of Marmara, and more than 1,500 tonnes of oil were spilled into the water.

The North Anatolian fault, which has triggered many major earthquakes in recent years, such as the August and November 1999 earthquakes in Izmit and Düzce, respectively, runs under the sea.

Extent

The International Hydrographic Organization defines the limits of the Sea of Marmara as follows:[2]

On the West. The Dardanelles limit of the Ægean Sea [A line joining Kum Kale (26°11'E) and Cape Helles].
On the Northeast. A line joining Cape Rumili with Cape Anatoli (41°13'N).

Name

The sea takes its name from the island of Marmara, which is rich in sources of marble, from the Greek μάρμαρον (marmaron), "marble".[3]

The sea's ancient Greek name Propontis derives from pro (before) and pont- (sea), deriving from the fact that the Greeks sailed through it to reach the Black Sea. In Greek mythology, a storm on Propontis brought the Argonauts back to an island they had left, precipitating a battle where either Jason or Heracles killed King Cyzicus, who mistook them for his Pelasgian enemies.[4]

Towns and cities

Towns and cities on the Marmara Sea coast include:

See also

  • 1509 Istanbul earthquake
  • Turkish Straits
  • Montreux Convention Regarding the Regime of the Turkish Straits
  • Canal Istanbul

Gallery

References

External links

  • Encyclopædia Britannica
  • SCIENCE FOCUS – SeaWiFS, Sea of Marmara: Where Ancient Myth and Modern Science Mix
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and USA.gov, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for USA.gov and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
 
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
 
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.
 



Copyright © World Library Foundation. All rights reserved. eBooks from World Library are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.