Gulf of Corinth

The Gulf of Corinth or the Corinthian Gulf (Greek: Κορινθιακός Κόλπος, romanized: Korinthiakós Kólpos, Greek pronunciation: [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 Rion Strait 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 tectonic movement across the gulf is comparable to parts of Iceland and Turkey, growing by 10 mm (0.39 in) per year.

Gulf of Corinth
Κορινθιακός Κόλπος (Greek)
Gulf of Corinth
Gulf of Corinth Gulf of Corinth Gulf of Corinth
Coordinates	38°12′N 22°30′E
Type	gulf
Part of	Ionian Sea (Mediterranean)
Basin countries	Greece
Max. length	130 km (81 mi)
Max. width	32 km (20 mi)
Min. width	8.4 km (5.2 mi)
Surface area	2,400 km2 (930 sq mi)
Max. depth	935 m (3,068 ft)

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.

Geology

Main article: Gulf of Corinth basin

Gulf of Corinth as seen from the mountains near upper Ziria. To the right of the photo we can see the Trizonia island

The gulf was created by the expansion of a tectonic rift due to the westward movement of the Anatolian Plate, and expands by 10 mm (0.39 in) per year. 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).

Nature

Striped dolphins jumping in the gulf

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

Gulfs and bays

• Alkyonides Gulf, east
• Crissaean Gulf (Gulf of Crissa), north
• Bay of Antikyra, north
• Dombraina (Domvrena), north
• Rion Strait, links the Gulf to the Ionian Sea

Islands

• Trizonia (the only inhabited), Alkyonides Islands (group of islets), Ampelos (islet), Fonias (islet), Prasoudi (islet)

Bridges

• Rio–Antirrio bridge

Cities and towns

Gulf of Corinth from Acrocorinth

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

• Aetolia-Acarnania: Antirrio, Nafpaktos
• Phocis: Galaxidi, Itea, Kirra
• Boeotia: Antikyra, Paralia Distomou
• West Attica
• Corinthia: Loutraki, Corinth, Assos, Vrachati, Velo, Kiato, Kato Diminio, Xylokastro
• Achaea: Aigeira, Diakopto, Aigio, Rododafni, Agios Vasileios, Aktaio

Tributaries

Corinth Canal

All tributaries are listed west to east.

Northern

• Mornos
• Pleistos

Southern

• Selemnos
• Volinaios
• Foinikas
• Selinountas
• Vouraikos
• Krathis
• Krios
• Zacholitikos
• Fonissa
• Sythas
• Elissonas
• Asopos

External links

• The Corinth Rift Observatory