Tyrrhenian Sea Explained

Tyrrhenian Sea
Etymology:From the ancient people of Tyrrhenians
Image Bathymetry:Tyrrhenian Sea map.png
Caption Bathymetry:Tyrrhenian Sea
Location:Mediterranean Sea
Coords:40°N 12°W
Type:Sea
Basin Countries:Italy, France
Area:275000-2NaN-2
Depth:20000NaN0
Max-Depth:37850NaN0

The Tyrrhenian Sea (;[1] Italian: Mar Tirreno pronounced as /it/ or pronounced as /it/)[2] 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).[3] The Tyrrhenian Sea also includes a number of smaller islands like Capri, Elba, Ischia, and Ustica.[4] The maximum depth of the sea is 3785m (12,418feet).

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:[5]

Exits

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

Exit Location Width Connected Sea
Corsica Channel between Tuscany and Corsica 42.8333°N 54°W about 80km (50miles) Ligurian Sea
11km (07miles) Mediterranean Sea (proper)
no name about 290km (180miles) Mediterranean Sea (proper)
3km (02miles) 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.[6]

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. Episodes of fast and slow trench retreat formed first the Vavilov basin and, then, the Marsili basin.[7] 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.[8] [9] [10] [11] [12] The Etruscans lived along the coast of modern Tuscany, Latium and Campania, and referred to the water as the "Sea of the Etruscans".

Islands

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. There is also Bastia, located in Corsica.

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 42miles to the northwest of Rome.[14]

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.[15]

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 and References

  1. Book: Longman . J.C. . Longman Pronunciation Dictionary . 2008 . Pearson Education ESL . 978-1405881173 . 3.
  2. French: Mer Tyrrhénienne pronounced as /fr/ Latin: Tyrrhēnum mare, Sardinian: Mare Tirrenu, Corsican: Mari Tirrenu, Sicilian: Mari Tirrenu, Neapolitan: Mare Tirreno
  3. Encyclopedia: Tyrrhenian Sea . . July 18, 2017 . Chisholm . Hugh . Hugh Chisholm . . ((The Editors of Encyclopaedia Britannica)).
  4. Web site: Tyrrhenian Sea - Map & Details . World Atlas . July 18, 2017.
  5. Book: Limits of Oceans and Seas . 172 . 3rd . 1953 . . May 2, 2020 . 17 . 28. 1953Natur.172R.484. . 10.1038/172484b0 . 36029611 .
  6. Sartori . Renzo . The Tyrrhenian back-arc basin and subduction of the Ionian lithosphere . . 2003 . 26 . 3 . 217–221 . https://web.archive.org/web/20081219151730/http://www.episodes.org/backissues/263/10Sartori.pdf . December 19, 2008 . University of Bologna. 10.18814/epiiugs/2003/v26i3/011 . free .
  7. 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. 10.1016/s0012-821x(01)00280-1. 0012-821X. 2001E&PSL.187..105F.
  8. Hesiod, Theogony 1015.
  9. Book: Barker . Graeme . Graeme Barker. Rasmussen . Tom . Tom Rasmussen . 2000 . The Etruscans . The Peoples of Europe. English . Oxford . Blackwell Publishing . 44 . 978-0-631-22038-1 .
  10. Book: Turfa. Jean MacIntosh . Jean MacIntosh Turfa. 2017. The Etruscans. Farney. Gary D. . Bradley . Gary . The Peoples of Ancient Italy . Berlin . De Gruyter. 637–672 . 10.1515/9781614513001 . 978-1-61451-520-3 .
  11. Book: De Grummond . Nancy T.. Nancy Thomson de Grummond. 2014 . Ethnicity and the Etruscans. McInerney . Jeremy . A Companion to Ethnicity in the Ancient Mediterranean . Chichester, UK . John Wiley & Sons, Inc . 405–422 . 10.1002/9781118834312 . 9781444337341 .
  12. Book: Shipley . Lucy . 2017. Where is home? . The Etruscans: Lost Civilizations. en . London . Reaktion Books . 28–46 . 9781780238623 .
  13. Web site: Map of Tyrrhenian Sea - Tyrrhenian Sea Map, History Facts, Tyrrhenian Sea Location - World Atlas. www.worldatlas.com. 20 March 2018.
  14. Web site: Civitavecchia (Port of Rome) Rome for Visitors . 2024-03-28 . europeforvisitors.com.
  15. Web site: 2014-07-27 . Costa Concordia comes home to die . 2024-03-27 . The Telegraph . en.