Kamma, Pantelleria Aeroporto, Scauri, Bagno Dell'Acqua, Bonsulton, Buccaram Di Sopra, Bugeber, Campobello, Contrada Venedise, Cufurà, Gadir, Garitte Karuscia, Khaddiuggia, Khamma Fuori, Località Cimillia, Località Mursia, Località Punta Fram, Località Roncone - Salerno, Località Ziton, Madonna Delle Grazie, Martingana, Mordomo, Penna, San Michele, San Vito, Santa Chiara, Scauri I, Siba - Roncone, Villaggio Tre Pietre
Pantelleria (Italian pronunciation:[pantelleˈɾiːa];[3]Sicilian: Pantiḍḍirìa; [pandɪɖɖɪˈɾiːa]), known in ancient times as Cossyra or Cossura, is an Italian island and comune in the Strait of Sicily in the Mediterranean Sea, 106 kilometres (55 nautical miles) southwest of Sicily and 68 km (35 nmi) east of the Tunisian coast. On clear days Tunisia is visible from the island. Administratively Pantelleria's comune belongs to the Sicilian province of Trapani.
With an area of 83 km2 (32 sq mi), Pantelleria is the largest volcanic satellite island of Sicily. The last eruption occurred below sea level in 1891, and today phenomena related to volcanic activity are present, such as hot springs and fumaroles. The highest peak, the Montagna Grande, reaches 836 m (2,743 ft) above sea level. The islanders speak Pantesco, a dialect of Sicilian influenced by Arabic.
Names
Cossura bronze coin showing a portrait of Isis with Punic legend (23 mm, 12.18 g)
The original Arab name for the island was Bint al-Riyāḥ (Arabic: بنت الرياح and Maltese: Bint l-Irjieħ), meaning "Daughter of the Winds" after the strong gales that can arise off the north coast of Africa.
Its Sicilian name is Pantiddirìa, which gave rise to the present Maltese name Pantellerija.
History
One of the sesi (burial tombs) on Pantelleria.
The earliest evidence of human activity dates to the Neolithic period distinguished for its use of obsidian tools and construction of stone structures and tombs known locally as "Sese".[8][9][10]
The original population of Pantelleria did not come from Sicily, but were of Iberian or Ibero-Ligurian ancestry. After a considerable interval, during which the island probably remained uninhabited, the Carthaginians took possession of it, no doubt owing to its importance as a station on the way to Sicily. This probably occurred around the beginning of the 7th centuryBC. Their acropolis was the twin hill of San Marco and Santa Teresa, 2 km (1+1⁄4 mi) south of the present town of Pantelleria. The town has considerable remains of walls made of rectangular blocks of masonry and also of a number of cisterns. Punic tombs have been discovered, and the votive terra-cottas of a small sanctuary of the Punic period were found near the north coast.
The Romans occupied the island as the Fasti Triumphales record in 255BC, lost it again the next year, and recovered it in 217BC. It struck bronze coins, originally with a Punic inscription but changing to Latin by the 1st centuryBC.[6] Under the empire, it served as a place of banishment for prominent persons and members of the imperial family. The town enjoyed municipal rights.
In AD700, Arabs conquered the island. In 1123, Roger II of Sicily took the island, and in 1311 an Aragonese fleet under the command of Lluís de Requesens won a considerable victory here. Requesens's family became princes of Pantelleria until 1553, when the Turks captured the island.[citation needed] A naval battle took place near the island in July 1586 when an armed English merchant fleet of five ships managed to repel an attack by eleven Spanish and Maltese galleys.
A Siculo-Arabic dialect similar to Maltese was the vernacular of the island until the late 18th century, when the RomanceSicilian superseded it. The modern Sicilian language in Pantelleria contains many Arabic loanwords, and most of the island's place names are of Semitic origin.
During the Napoleonic Wars, the British considered the possibility of taking over Pantelleria (together with Lampedusa and Linosa) so as to be able to supply Malta, but a royal commission stated in an 1812 report that there would be considerable difficulties in this venture.[11]
Pantelleria's capture was regarded as crucial to Operation Husky, the Allied invasion of Sicily in 1943 as planes based on Pantelleria could readily reach Sicily. In Operation Corkscrew the Allies bombarded Pantelleria heavily from air and sea in the days before the invasion. The garrison surrendered as the landing troops approached. Pantelleria then became a vital base for Allied aircraft during the assault on Sicily.
Archaeological sites
A Middle Bronze Age village was on the west coast, 3 km (2 mi) southeast of the harbour, with a rampart of small blocks of lava, about 7.5 m (25 ft) high, 10 m (33 ft) wide at the base and 5 m (16 ft) at the top, upon the undefended eastern side. Remains of huts were found there, with pottery, tools of obsidian, and other artifacts. These objects are in the museum at Syracuse.
To the southeast, in the district known as the Cunelie, are many tombs, known as sesi. They are similar in character to the nuraghe of Sardinia, though of smaller size, and consist of round or elliptical towers with sepulchral chambers in them, built of rough blocks of lava. Fifty-seven of them can still be traced. The largest is an ellipse of about 18 m × 20 m (59 ft × 66 ft), but most of the sesi have a diameter of only 6–7 m (20–23 ft). The identical character of the pottery found in the sesi with that found in the prehistoric village proves that the former are the tombs of the inhabitants of the latter.
The island has scattered typical one-level buildings called dammuso of unknown but probably remote origins. A dammuso is a dry stone building with thick walls that usually appear black due to the extensive use of volcanic rock. They have characteristic domes on top painted white to avoid overheating. The domes collect rainwater that is directed to a large tank (usually below the building) or to the nearby soil for use in the dry season.
Most of the other constructions were destroyed during the Second World War. One notable exception is the castle Barbacane, a renaissance building formed by an irregularly quadrangular plan with internal court joined to a squared base tower.
Geology
Volcanic rocks in Pantelleria
The island of Pantelleria is located above a drowned continental rift in the Strait of Sicily and has been the focus of intensive volcano-tectonic activity. The 15 kilometre-long (9.3 mi) island is the emergent summit of a largely submarine edifice.[12] Two large Pleistocenecalderas dominate the island, the older of the two formed about 114,000 years ago and the younger Cinque Denti caldera formed about 45,000 years ago.[13] The eruption that formed the Cinque Denti caldera produced the distinctive green tuff deposit that covers much of the island, and is found across the Mediterranean, as far away as the island of Lesbos in the Aegean Sea.[14]Holocene eruptions have constructed pumice cones, lava domes, and short, blocky lava flows.[15]
Later activity constructed the cone of Monte Gibele, part of which was subsequently uplifted to form Montagna Grande. Several vents are located on three sides of the uplifted Montagna Grande block on the southeast side of the island. A submarine eruption in 1891 from a vent off the northwest coast is the only confirmed historical activity.[16]
Currently the island is subsiding, and Montagna Grande is slowly sinking. This is thought to be caused by the magma beneath the volcano cooling and degassing.[17] There are numerous hot springs and fumaroles on the island due to an active hydrothermal system. Favara Grande, in the south east of the island, is one of the best examples. The island is releasing a small amount of CO2 through passive degassing.[18]
Total carbon stock in the first 30 cm (12 in) of soil of Pantelleria is about 230,000 tonnes.[19]
The island is the type locality for peralkalinerhyolitic rocks, pantellerites.
Climate
Pantelleria has a subtropicalMediterranean climate (Köppen: Csa) characterized by very warm to hot, almost rainless and humid summers, very mild and frost-free winters, a powerful seasonal lag and a small diurnal temperature range. The constant sea breezes moderate the daytime summer temperatures. Coastal Pantelleria (along with Lampedusa, Kasos, Karpathos, and coastal Malta) is one of the very few areas along the Mediterranean Sea coast that has never recorded frost. Below freezing temperatures and snow only occur, and sporadically, at Montagna Grande and higher elevations on the island. Despite the very dry summers and the fairly low annual precipitation, the dry season is noticeably short at four months, and the rainy season lasts at least eight months.
Pantelleria National Park (Italian: Parco Nazionale dell'Isola di Pantelleria) was established in 2016, and covers an area of 66.4 km2 (25+5⁄8 sq mi), or 80% of the island.[23]
Specchio di Venere (literally "Venus' mirror") is a natural lake formed in an extinct volcanic crater, and fed by rain and hot springs. The lake is 12 m (39 ft) deep and is popular for swimming, hot springs, and mud bathing.
Other natural attractions are paths to the sea, a large network of trekking paths, hot springs, and a popular natural sauna fed by vapours filtering through rocks in a small cave. Also situated on the Island is Laghetto delle Ondine ("Pond of the ripples" or "Pond of the wavelets") a seawater lake which has developed into a very desired swimming hole.[24]
Pantelleria is noted for its sweet wines, Moscato di Pantelleria and Moscato Passito di Pantelleria, both made from the local Zibibbo grape.[26] In 2014, the traditional agricultural practice of cultivating the vite ad alberello (head-trained bush vines) of the community of Pantelleria was inscribed on the Representative List of the Intangible Cultural Heritage of Humanity of UNESCO.[27]
Transport
The island is served by Pantelleria Airport,[28] which is served by DAT, connecting Trapani and Palermo and other companies in summer, connecting the island with Italian cities such as Milan, Rome, Venice and others. Ferries reach the island from Trapani, and it is near the main east–west route through the Mediterranean Sea.
^Margari, V.; D.M. Pyle; C. Bryant; P.L. Gibbard (1 June 2007). "Mediterranean tephra stratigraphy revisited: Results from a long terrestrial sequence on Lesvos Island, Greece". Journal of Volcanology and Geothermal Research. 163 (1–4): 34–54. Bibcode:2007JVGR..163...34M. doi:10.1016/j.jvolgeores.2007.02.002. ISSN0377-0273.
^D'Alessandro, W. (2007). Final report of Research Unit V3_7/02. Palermo, Italy: Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo. hdl:2122/4911.
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