Gulf of Corinth explained

Gulf of Corinth
Coordinates:38.2°N 52°W
Type:gulf
Part Of:Ionian Sea (Mediterranean)
Basin Countries:Greece
Length:130km (80miles)[1]
Min Width:8.4km (05.2miles)
Width:32km (20miles)
Area:2400sqkm
Max-Depth:935m (3,068feet)
Pushpin Map:Greece#Mediterranean#Europe

The Gulf of Corinth or the Corinthian Gulf (Greek, Modern (1453-);: Κορινθιακός Κόλπος|Korinthiakós Kólpos, in Greek, Modern (1453-); pronounced as /koɾinθiaˈkos ˈkolpos/) is a deep inlet of the Ionian Sea, separating the Peloponnese from western mainland Greece. It is bounded in the east by the Isthmus of Corinth which includes the shipping-designed Corinth Canal and in the west by the Strait of Rion which widens into the shorter Gulf of Patras (part of the Ionian Sea) and of which the narrowest point is crossed since 2004 by the Rio–Antirrio bridge. The gulf is bordered by the large administrative divisions (regional units): Aetolia-Acarnania and Phocis in the north, Boeotia in the northeast, Attica in the east, Corinthia in the southeast and south and Achaea in the southwest. The gulf is in tectonic movement comparable to movement in parts of Iceland and Turkey, growing by 10mm per year.

In the Middle Ages, the gulf was known as the Gulf of Lepanto (the Italian form of Naupactus).

Shipping routes between the Greek commercial port Piraeus (further away from ultimate destinations but larger and better connected to the south than the north-western Greek port of Igoumenitsa) to western Mediterranean and hemisphere ports pass along this gulf. A ferry crosses the gulf to link Aigio and Agios Nikolaos, towards the western part of the gulf.[2]

Geology

See main article: Gulf of Corinth basin. The gulf was created by the expansion of a tectonic rift due to the westward movement of the Anatolian Plate, and expands by 10mm per year.[3] The surrounding faults can produce earthquakes up to magnitude around 6.5, though they are relatively uncommon. On June 15, 1995, an earthquake of magnitude 6.2 occurred near the city of Aigion. A large part of the northern margin of the gulf is characterized by gentle gradients (between 10 and 20 degrees). The southern margin of the gulf is largely characterized by steep gradients (between 30 and 40 degrees).[4]

Nature

Cetaceans such as fin whales[5] or dolphins are known to enter the Corinthian gulf occasionally.[6]

Gulfs and bays

Islands

Bridges

Cities and towns

The main cities and towns that lie next to the gulf are, from the northwest clockwise, and grouped by regional unit:

Antirrio, Nafpaktos

Galaxidi, Itea, Kirra

Antikyra, Paralia Distomou

Loutraki, Corinth, Assos, Vrachati, Velo, Kiato, Kato Diminio, Xylokastro

Aigeira, Diakopto, Aigio, Rododafni, Agios Vasileios, Aktaio

Tributaries

All tributaries are listed west to east.

Northern

Southern

External links

Notes and References

  1. Thalassographica, Institute of Oceanographic and Fisheries Research, vol. 11-15, page 35, (1988)
  2. Web site: Greece's first electric ferry announced . Plugboats . 19 December 2019.
  3. Ambraseys, N.N. & Jackson, J.A. 1997. Seismicity and strain in the Gulf of Corinth (Greece) since 1694. Journal of earthquake engineering, 1, 433-474.
  4. Frostick, L & Steel, Ronald. (2009). Tectonic Signatures in Sedimentary Basin Fills: An Overview. International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts. 31. 1-9.10.1002/9781444304053.ch1
  5. Web site: Fin Whale in the Gulf of Korinth. https://ghostarchive.org/varchive/youtube/20211221/qAx1JhuX_-0 . 2021-12-21 . live. nefarius03. 19 May 2013. 13 April 2018. YouTube.
  6. Keep Talking Greece. 2011. Trapped Whale in Greece (video) . Retrieved on November 6. 2014