Tyrrhenian Sea
Tyrrhenian Sea
LocationMediterranean Sea
Coordinates40°N 12°E / 40°N 12°E / 40; 12
TypeSea
EtymologyFrom the ancient people of Tyrrhenians
Basin countriesItaly, France
Surface area275,000 km2 (106,200 sq mi)
Average depth2,000 m (6,562 ft)
Max. depth3,785 m (12,418 ft)

The Tyrrhenian Sea (/tɪˈriːniən, -ˈreɪ-/, tih-REE-nee-ən ,-RAY-;[1] Italian: Mar Tirreno [mar tirˈrɛːno] or [-ˈreː-], French: Mer Tyrrhénienne [mɛʁ tiʁenjɛn])[note 1] is part of the Mediterranean Sea off the western coast of Italy. It is named for the Tyrrhenian people identified with the Etruscans of Italy.

Geography

The sea is bounded by the islands of Corsica and Sardinia (to the west), the Italian Peninsula (regions of Tuscany, Lazio, Campania, Basilicata, and Calabria) to the north and east, and the island of Sicily (to the south).[2] The Tyrrhenian Sea also includes a number of smaller islands like Capri, Elba, Ischia, and Ustica.[3]

Amalfi Coast, Positano
Cala Goloritzé, Baunei, Sardinia

The maximum depth of the sea is 3,785 metres (12,418 ft).

The Tyrrhenian Sea is situated near where the African and Eurasian Plates meet; therefore mountain chains and active volcanoes, such as Mount Marsili, are found in its depths. The eight Aeolian Islands and Ustica are located in the southern part of the sea, north of Sicily.

Extent

The International Hydrographic Organization defines the limits of the Tyrrhenian Sea as follows:[4]

Exits

There are four exits from the Tyrrhenian Sea (north to south):

ExitLocationWidthConnected Sea
Corsica Channelbetween Tuscany and Corsica 42°50′N 9°45′E / 42.833°N 9.750°E / 42.833; 9.750about 80 kilometres (50 mi)Ligurian Sea
Strait of Bonifaciobetween Corsica and Sardinia11 kilometres (6.8 mi)Mediterranean Sea (proper)
no namebetween Sardinia and Sicilyabout 290 kilometres (180 mi)Mediterranean Sea (proper)
Strait of Messinabetween Sicily and Calabria on the toe of Italy3 kilometres (1.9 mi)Ionian Sea

Basins

The Tyrrhenian Basin is divided into two basins (or plains), the Vavilov plain and the Marsili plain. They are separated by the undersea ridge known as the Issel Bridge, after Arturo Issel.[5]

Geology

The Tyrrhenian Sea is a back-arc basin that formed due to the rollback of the Calabrian slab towards South-East during the Neogene.[5] Episodes of fast and slow trench retreat formed first the Vavilov basin and, then, the Marsili basin.[6] Submarine volcanoes and the active volcano Mount Stromboli formed because trench retreat produces extension in the overriding plate allowing the mantle to rise below the surface and partially melt. The magmatism here is also affected by the fluids released from the slab.

Name

Its name derives from the Greek name for the Etruscans, first mentioned by Hesiod in the 8th century BC who described them as residing in central Italy alongside the Latins.[7][8][9][10][11] The Etruscans lived along the coast of modern Tuscany, Latium and Campania, and referred to the water as the "Sea of the Etruscans".

Islands

Lipari, Aeolian Islands, Sicily

Islands of the Tyrrhenian Sea include:

Ports

The main ports of the Tyrrhenian Sea in Italy are: Naples, Palermo, Civitavecchia (Rome), Salerno, Trapani, and Gioia Tauro. In Corsica, the most important port is Bastia.

Note that even though the phrase "port of Rome" is frequently used, there is in fact no port in Rome. Instead, the "port of Rome" refers to the maritime facilities at Civitavecchia, some 68 km (42 miles) to the northwest of Rome.

Giglio Porto is a small island port in this area. It rose to prominence, when the Costa Concordia ran aground near the coast of Giglio and sank. The ship was later refloated and towed to Genoa for scrapping.

Winds

In Greek mythology, it is believed that the cliffs above the Tyrrhenian Sea housed the four winds kept by Aeolus. The winds are the Mistral from the Rhône valley, the Libeccio from the southwest, and the Sirocco and Ostro from the south.

Notes

  1. ↑ Latin: Tyrrhēnum mare, Sardinian: Mare Tirrenu, Corsican: Mari Tirrenu, Sicilian: Mari Tirrenu, Neapolitan: Mare Tirreno

References

  1. ↑ Longman, J.C. (2008). Longman Pronunciation Dictionary (3 ed.). Pearson Education ESL. ISBN 978-1405881173.
  2. ↑ The Editors of Encyclopaedia Britannica. "Tyrrhenian Sea". In Chisholm, Hugh (ed.). Encyclopedia Britannica. Cambridge University Press. Retrieved July 18, 2017.
  3. ↑ "Tyrrhenian Sea - Map & Details". World Atlas. Retrieved July 18, 2017.
  4. ↑ Limits of Oceans and Seas (PDF). Vol. 172 (3rd ed.). 1953. p. 17. Bibcode:1953Natur.172R.484.. doi:10.1038/172484b0. S2CID 36029611. Retrieved May 2, 2020. {{cite book}}: |work= ignored (help)
  5. 1 2 Sartori, Renzo (2003). "The Tyrrhenian back-arc basin and subduction of the Ionian lithosphere" (PDF). Episodes. University of Bologna. 26 (3): 217–221. doi:10.18814/epiiugs/2003/v26i3/011. Archived from the original (PDF) on December 19, 2008.
  6. ↑ Faccenna, Claudio; Funiciello, Francesca; Giardini, Domenico; Lucente, Pio (2001). "Episodic back-arc extension during restricted mantle convection in the Central Mediterranean". Earth and Planetary Science Letters. 187 (1–2): 105–116. Bibcode:2001E&PSL.187..105F. doi:10.1016/s0012-821x(01)00280-1. ISSN 0012-821X.
  7. ↑ Hesiod, Theogony 1015.
  8. ↑ Barker, Graeme; Rasmussen, Tom (2000). The Etruscans. The Peoples of Europe. Oxford: Blackwell Publishing. p. 44. ISBN 978-0-631-22038-1.
  9. ↑ Turfa, Jean MacIntosh (2017). "The Etruscans". In Farney, Gary D.; Bradley, Gary (eds.). The Peoples of Ancient Italy. Berlin: De Gruyter. pp. 637–672. doi:10.1515/9781614513001. ISBN 978-1-61451-520-3.
  10. ↑ De Grummond, Nancy T. (2014). "Ethnicity and the Etruscans". In McInerney, Jeremy (ed.). A Companion to Ethnicity in the Ancient Mediterranean. Chichester, UK: John Wiley & Sons, Inc. pp. 405–422. doi:10.1002/9781118834312. ISBN 9781444337341.
  11. ↑ Shipley, Lucy (2017). "Where is home?". The Etruscans: Lost Civilizations. London: Reaktion Books. pp. 28–46. ISBN 9781780238623.
  12. ↑ "Map of Tyrrhenian Sea - Tyrrhenian Sea Map, History Facts, Tyrrhenian Sea Location - World Atlas". www.worldatlas.com. Retrieved 20 March 2018.
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