Sea of Marmara


The Sea of Marmara (/ˈmɑːrmərə/; Turkish: Marmara Denizi; Ancient Greek: Προποντίς, Προποντίδα), also known as the Sea of Marmora or the Marmara Sea, and in the context of classical antiquity as the Propontis, 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 lands. The Bosphorus strait connects it to the Black Sea and the Dardanelles strait to the Aegean Sea. The former also separates Istanbul into its Asian and European sides. The Sea of Marmara is a small sea with an area of 11,350 km2 (4,380 sq mi), and dimensions 280 km × 80 km (174 mi × 50 mi). Its greatest depth is 1,370 m (4,490 ft).
Name
The sea takes its name from Marmara Island, which is rich in sources of marble, from the Greek μάρμᾰρον (mármaron), "marble".
The sea's ancient Greek name Propontis derives from pro- (before) and pontos (sea), deriving from the fact that the Greeks sailed through it to reach the Black Sea, Pontos. 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.
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. 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, 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.
The sea contains the archipelago of the Prince Islands and Marmara Island, Avşa and Paşalimanı.
The south coast of the sea is heavily indented, and includes the Gulf of İzmit (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:
- On the West. The Dardanelles limit of the Aegean 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).
Towns and cities
Towns and cities on the Marmara Sea coast include:
Istanbul Province | Balıkesir Province | Kocaeli Province
| Yalova Province |
Gallery
The Bosphorus with Istanbul in the background
View of Marmara Sea from Istanbul
Sea of Marmara approaching Yassıada
See also
- 1509 Constantinople earthquake
- 1999 İzmit earthquake
- Black Sea deluge hypothesis
- Kanal İstanbul
- Montreux Convention Regarding the Regime of the Straits
- Turkish Straits
External links
- "Sea of Marmara" at the Encyclopædia Britannica
- "Sea of Marmara: Where Ancient Myth and Modern Science Mix" at SCIENCE FOCUS – SeaWiFS