| Thasos Περιφερειακή ενότητα / Δήμος Θάσου |
|
|---|---|
| — Regional unit — | |
| Limenas Thasou | |
| Thasos within East Macedonia and Thrace | |
| Coordinates: 40°41′N 24°39′E / 40.683°N 24.650°ECoordinates: 40°41′N 24°39′E / 40.683°N 24.650°E | |
| Country | Greece |
| Region | East Macedonia and Thrace |
| Capital | Thasos town |
| Area | |
| • Total | 379 km2 (146 sq mi) |
| Population (2011) | |
| • Total | 13,770 |
| • Density | 36/km2 (94/sq mi) |
| Postal codes | 640 04 |
| Area codes | 25930 |
| Car plates | ΚΒ |
| Website | www.thassos.gr |
Thasos or Thassos (Greek: Θάσος) is a Greek island in the northern Aegean Sea, close to the coast of Thrace and the plain of the river Nestos but geographically part of Macedonia. It is the northernmost Greek island, and 12th largest by area. Thasos is also the name of the largest town of the island (also known as Limenas Thasou, "Harbour of Thasos"), situated at the northern side, opposite the mainland and about 10 kilometres (6 mi) from Keramoti.
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Lying close to the coast of Eastern Macedonia, Thasos was inhabited from the Palaeolithic period onwards,[1] but the earliest settlement to have been explored in detail is that at Limenaria where Middle and Late Neolithic remains have been found that relate closely to those of the Drama Plain. In contrast, the remains of the Early Bronze Age on the island align it with the culture that developed in the Cyclades and Sporades to the south in the Aegean. At Skala Sotiros[2] for example, a small settlement was encircled by a strongly built defensive wall. Even earlier activity is demonstrated by the presence of large pieces of 'megalithic' anthropomorphic stelai built into these walls, which, so far, have no parallels in the Aegean area.
There is then a gap in the archaeological record until the end of the Bronze Age c 1100 BC, when the first burials took place at the large cemetery of Kastri in the interior of the island.[3][4] Here built tombs covered with small mound of earth were typical until the end of the Iron Age. In the earliest tombs were a small number of locally imitated Mycenaean pottery vessels, but the majority of the hand-made pottery with incised decoration reflects connections eastwards with Thrace and beyond.
The island was colonized at an early date by Phoenicians, attracted probably by its gold mines; they founded a temple to the god Melqart, whom the Greeks identified as "Tyrian Heracles", and whose cult was merged with Heracles in the course of the island's Hellenization.[5] The temple still existed in the time of Herodotus.[6] An eponymous Thasos, son of Phoenix (or of Agenor, as Pausanias reported) was said to have been the leader of the Phoenicians, and to have given his name to the island.
Around 650 BC, or a little earlier, Greeks from Paros founded a colony on Thasos.[7] A generation or so later, the poet Archilochus, a descendant of these colonists, wrote of casting away his shield during a minor war against an indigenous Thracian tribe, the Saians.[8] Thasian power, and sources of its wealth, extended to the mainland, where the Thasians owned gold mines even more valuable than those of the island; their combined annual revenues amounted to between 200 and 300 talents. Herodotus says that the best mines on the island were those opened by the Phoenicians on the east side of the island, facing Samothrace.. Archilochus described Thasos as "an ass's backbone crowned with wild wood." The island's capital, Thasos, had two harbors. Besides its gold mines, the wine, nuts and marble of Thasos were well known in antiquity. Thasian wine was quite famous. Thasian coins had the head of the wine god Dionysos on one side and bunches of grape of the other.[9]
Thasos was important during the Ionian Revolt against Persia. After the capture of Miletus (494 BC) Histiaeus, the Ionian leader, laid siege. The attack failed, but, warned by the danger, the Thasians employed their revenues to build war ships [10] and strengthen their fortifications. This excited the suspicions of the Persians, and Darius compelled them to surrender their ships and pull down their walls. After the defeat of Xerxes the Thasians joined the Delian confederacy; but afterwards, on account of a difference about the mines and marts on the mainland, they revolted.
The Athenians defeated them by sea, and, after a siege that lasted more than two years, took the capital, Thasos, probably in 463 BC, and compelled the Thasians to destroy their walls, surrender their ships, pay an indemnity and an annual contribution (in 449 BC this was 21 talents, from 445 BC about 30 talents), and resign their possessions on the mainland. In 411 BC, at the time of the oligarchical revolution at Athens, Thasos again revolted from Athens and received a Lacedaemonian governor; but in 407 BC the partisans of Lacedaemon were expelled, and the Athenians under Thrasybulus were admitted.
After the Battle of Aegospotami (405 BC), Thasos again fell into the hands of the Lacedaemonians under Lysander who formed a decarchy there; but the Athenians must have recovered it, for it formed one of the subjects of dispute between them and Philip II of Macedonia. In the embroilment between Philip V of Macedonia and the Romans, Thasos submitted to Philip, but received its freedom at the hands of the Romans after the Battle of Cynoscephalae (197 BC), and it was still a "free" state in the time of Pliny.
It is related, that Byzantine Greek Saint Joannicius the Great (752–846) in one of his miracles freed the island of Thasos from a multitude of snakes.
Thasos was part of the Eastern Roman Empire, later known as Byzantine Empire. It was captured by the Turks in 1462. Under the Turks the island was known as Ottoman Turkish: طاشوز Taşöz. A brief revolt against Ottoman rule in 1821, led by Hajiyorgis Metaxas, failed. The island was given by the Sultan Mahmud II to Muhammad Ali of Egypt as a personal fiefdom in the late 1820s, as a reward for Egyptian intervention in the War of Greek Independence (which failed to prevent the creation of the modern Greek state). Egyptian rule was relatively benign (by some accounts Muhammad Ali had either been born or spent his infancy on Thasos) and the island became prosperous, until 1908, when the New Turk regime asserted Turkish control. It had the status of a sanjak in the vilayet of Salonici until the Balkan Wars. On October 20, 1912 during the First Balkan War, a Greek naval detachment claimed Thasos as part of Greece, which it has remained since.
During the Axis occupation (1941–1944) Thasos, along with the rest of Eastern Macedonia and Thrace, was under Bulgarian control. The Bulgarians planned to annex the territory under their control and closed down schools as a first step towards forced Bulgarization. Under Bulgarian rule the island was called Тасос. Mountainous terrain facilitated small-scale resistance activity. The Greek Civil War affected the island in the form of skirmishes and Communist guerilla attacks until 1950, almost a year after the main hostilities were over on the mainland.
Thasos, the capital, is now informally known as Limenas, or "the port". It is served by ferry routes to and from Kavala and Keramoti. The latter is a port close to Kavala International Airport, and has the shortest possible crossing to the island.
Thasos is a separate regional unit of the East Macedonia and Thrace region, and the only municipality of the regional unit.[11] As a part of the 2011 Kallikratis government reform, the regional unit Thasos was created out of part of the former Kavala Prefecture. The municipality, unchanged at the Kallikratis reform, includes a few uninhabited islets besides the main island Thasos. The province of Thasos (Greek: Επαρχία Θάσου) was one of the provinces of the Kavala Prefecture. It had the same territory as the present municipality.[12] It was abolished in 2006.
Thasos island is located in the northern Aegean sea approximately 7 km from the northern mainland and 20 km south-east of Kavala, and is of generally rounded shape, without deep bays or significant peninsulas. The terrain is mountainous but not particularly rugged, rising gradually from coast to centre. The highest peak is Ypsario (Ipsario), at 1,205 m (3428 ft), somewhat east of centre. Pine forest covers much of the island's eastern slopes.
Historically, the island's population was chiefly engaged in agriculture and stockbreeding, and established villages inland, some of them connected via stairways (known as skalas) to harbors at the shore. The local population gradually migrated towards these shoreline settlements as tourism began to develop as an important source of income. Thus, there are several "paired villages" such as Marion–Skala Maries, with the former inland and the latter on the coast.
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This section may be too technical for most readers to understand. (January 2013) |
The Island is formed mainly by gneisses, schists and marbles of the Rhodope Massif. Marble sequences corresponding to the Falacron Marbles intercalated by schists and gneisses, are up to 500m thick and are separated from the underlying gneisses by a transition zone about 300 m thick termed the T-zone consisting of alternances of dolomitic and calcitic marbles intercalated by schists and gneisses.
The rocks have undergone several periods of regional metamorphism, to at least upper amphibolite facies, and there was a subsequent phase of retrograde metamorphism. At least three periods of regional deformation have been identified, the most important being large scale isoclinal folding with axes aligned north-west. The T-zone is deformed and is interpreted by some authors as a regional thrust of pre-major folding age. There are two major high angle fault systems aligned north-west and north-east respectively. A large low-angle thrust cuts the gneiss, schist and marble sequence at the south-west corner of the island, probably indicating an overthrusting of the Serbomacedonian Massif onto the Rodope Massif.
The Late Miocene oil-producing Nestos-Prinos basin is located between Thassos island and the mainland. The floor of the basin is around 1,500 m deep off the Thassos coast (South Kavala ridge; Proedrou, 1988) and up to 4.000–5.000 m in the axial sector between Thassos and the mainland. The basin is filled with Late Miocene-Pliocene sediments, including ubiquitously repeated evaporite layers of rock salt and anhydrite-dolomite that alternate with sandstones, conglomerates, black shales, and uraniferous coal measures (Proedrou, 1979, 1988; Taupitz, 1985). Stratigraphically equivalent rocks on the mainland are clastic sediments with coal beds, marine to brackish fluvial units and travertines.
The earliest mining on the island has been dated to around 13,000 BC, when paleolithic miners dug a shaft at the site of the modern-era Tzines iron mine for the extraction of limonitic ochre.[13] Mining for base and precious metals started around the 7th century BC with the Phoenicians, followed in the 4th century by the Greeks, then the Romans. These later mines were both open-cast and underground., mostly to exploit the island's numerous karst hosted calamine deposits for their lead and silver. Gold, copper and iron were also found; the Byzantines quarried marble on the island.
In the early 20th century, mining companies exploited the island's Zinc-lead rich calamine ores, with a yield of around 2 million tonnes, and a processing plant at Limenaria produced zinc oxide. Iron ore was mined on a significant scale from 1954 to 1964, with a yield of around 3 million tonnes. Since 1964, surveys have established the existence of a deep-level zinc-lead deposit, but the only mining activity on the island has been marble quarrying.
By far the most important economic activity is tourism. The main agricultural products on the island are honey, olives (famously Throuba olives) and olive oil, as well as wine, sheep, goat herding and fishing. Other industries are lumber and mining which includes lead, zinc and marble, especially in the Panagia area where one of the mountains near the Thracian Sea has a large marble quarry. The marble quarries in the south (in the area of Aliki), now abandoned, were mined during ancient times.
Towns and villages with over 100 inhabitants are:
| Year | Town | Municipality |
|---|---|---|
| 1981 | 2,312 | – |
| 1991 | 2,600 | – |
| 2001 | 3,140 | 13,765 |
| 2011 | 3,240 | 13,770 |
This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press.
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