Milos

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For the Slavic male name, see Miloš. For the refugee ship, see Patria disaster.
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Milos
Μήλος
The Chora of Milos
The Chora of Milos
Location
Milos is located in Greece
Milos
Milos
Coordinates 36°41′N 24°25′E / 36.683°N 24.417°E / 36.683; 24.417Coordinates: 36°41′N 24°25′E / 36.683°N 24.417°E / 36.683; 24.417
Government
Country: Greece
Administrative region: South Aegean
Regional unit: Milos
Population statistics (as of 2011)[1]
Municipality
 - Population: 4,977
 - Area: 160.1 km2 (62 sq mi)
 - Density: 31 /km2 (81 /sq mi)
Community
 - Population: 819
Other
Time zone: EET/EEST (UTC+2/3)
Elevation (min-max): 0–748 m ­(0–2454 ft)
Postal code: 840 xx
Telephone: 22870
Auto: EM
Website
www.milos.gr

Milos or Melos (/ˈmɛlɒsˌ -sˌ ˈmlɒs, -ls/; Modern Greek: Μήλος [ˈmilos]; Ancient Greek: Μῆλος Melos) is a volcanic Greek island in the Aegean Sea, just north of the Sea of Crete. Milos is the southwesternmost island in the Cyclades group.

The island is famous for the statue of Aphrodite (the "Venus de Milo", now in the Louvre), and also for statues of the Greek god Asclepius (now in the British Museum[2]) and the Poseidon and an archaic Apollo in Athens. The Municipality of Milos also includes the uninhabited offshore islands of Antimilos and Akradies. The combined land area is 160.147 square kilometres (61.833 sq mi) and the 2001 census population was 4,977 inhabitants.

History[edit]

The ancient theatre.

Obsidian from Milos was a commodity as early as 15,000 years ago.[3] Milos natural glass used for razor sharp "stone tools" was transported well before farming began and later: "There is no early farming village in the Near East that doesn't get obsidian".[4] The material was transported for thousands of miles. However the mining of obsidian did not lead to the development of permanent habitation or manufacturing on the island. Instead, those in search of obsidian arrived by boat, beaching it in a suitable cove and cutting pieces of the volcanic glass from the quarries.[5]

The position of Milos, between mainland Greece and Crete, and its possession of obsidian, made it an important centre of early Aegean civilization. Milos lost its arms-making importance when bronze became the preferred material for the manufacture of weapons.[6]

The first settlement at Phylakopi (Greek Φυλακωπή) arose in the Bronze Age, flourishing as the extraction of obsidian was in the decline. The first settlers were tuna fishermen.[5] Lying on the north-east coast, excavations by the British School of Archeology revealed a town wall and a Minoan-inspired structure, dubbed the Pillar room, which contained fragments of vivid wall paintings. The famous fresco of the flying fish[7] was found in the ruins of the Pillar room and was executed with delicate coloring and graphic observation of nature in the graceful movement of a fish. The stylistic similarities to Minoan frescoes are suggested and it could perhaps have been the work of a Cretan artist.[8] Part of the site has been washed away by the sea.

The antiquities found at the site covered three major periods, from the Early Cycladic period to the Mycenaean period Mycenaean age of Greece. At the site much pottery was excavated, with several changing styles and influences over the sites long occupation. In the early occupation of the site, there are many similarities and imports from other Cycladic islands and the settlement was very small. During the Middle Bronze Age however the site expanded significantly and the expansion of Minoan Crete saw an influx of Minoan pottery into the Cyclades, particularly at Akrotiri on Thera, though much found its way to Phylakopi. The quantities found at the Cycladic sites have been taken to suggest a Minoan control over the region, though it could also be the consumptive nature of the islanders adopting in vogue fashions. There is more than just pottery at Phylakopi however, the eruption of the Thera volcano saw a reduction in Minoan presence in the Cyclades and it is at this time that Mycenaean involvment on the islands increases. At Phylakopi(and unprecedented in the rest of the Cyclades) was found a Megaron structure, which is typically associated with the Mycenaean palaces, such as those at Tiryns, Pylos and Mycenae. This has been taken to suggest that the Mycenaeans conquered the settlement and installed a seat of power for a governor. The evidence is not clear, though again it could be a legacy of the islanders adopting foreign elements into their culture. Particularly unexpected was the discovery in the 1970's of a shrine at the site, which contained many examples of Aegean figurines, including the famous "Lady of Phylakopi". The shrine is unprecedented in the Bronze Age Cyclades and has provided a valuable insight ito the beliefs and rituals of the inhabitants of Phylakopi. The site was eventually abandoned and was never reoccupied.

In historical times, the island was occupied by Dorians from Laconia. In the 6th century BC, it again produced a remarkable series of vases, of large size, with mythological subjects and orientalizing ornamentation, and also a series of terra-cotta reliefs (Melian Reliefs).

Conflict with Athens[edit]

See also: Melian dialogue
Coin from Melos, 2nd century BC, Obverse: Apple (μῆλον mēlon) Reverse: The Palladion (right), krater (left).
The archaeological museum.
Klima village.

The Greek historian Thucydides wrote in his History of the Peloponnesian War of how, in 416 BCE, Athens attacked Melos for refusing to submit tribute and refusing to join Athens' alliance against Sparta.

The invasion of Melos occurred during the second phase of the Peloponnesian War (431 to 404 BCE). The Melians claimed Spartan descent but had remained neutral throughout this conflict.[6] In 426 BCE, Athens had prosecuted a brief perfunctory operation on the island but had withdrawn quickly because they were at the time involved in open conflict with Sparta. In 425 BCE Athens claimed suzerainty over Melos and had demanded tribute.[9] The second attack on Melos occurred five years after Athens and Sparta had signed a peace agreement and some historians like Bosworth believe that Athens' campaign against Melos in 416 BCE was motivated by imperial expansion.[9]

In the summer of 416 BCE the Athenians landed an army of over 3,000 soldiers on the island, led by the generals Cleomedes and Tisias. They sent diplomats to negotiate a surrender, offering to spare the Melians if they joined the Athenian-dominated Delian League and paid tribute to Athens. The Melians rejected the ultimatum. The Athenians laid siege to the city and withdrew most of their troops from the island to fight elsewhere. For months the Melians withstood the siege, but with reinforcements from Athens and the help of traitors within Melos, the Athenians took the city that winter. In the aftermath, as was common in ancient history with resisted sieges, the Athenians executed all the adult men they caught, and sold the women and children into slavery. They then settled 500 of their own colonists on the island.[10]

The next year, the Athenian tragedian Euripides wrote Trojan Women, which explored the hardships of conquest on women, set in the legendary past of the Trojan War.

When Athens was defeated by Sparta at the end of the Peloponnesian War, the Melian survivors, who had been resettled by Sparta, were restored to their homes by the Spartan general Lysander.

Medieval Period[edit]

A church in Milos.
Adamas town

During the Frankish period the island formed part of the Duchy of Naxos, except for the few years (1341–1383) when it was a separate lordship under Marco Sanudo and his daughter.

In 1566 the Venetians handed over the island to the Ottoman Turks, who were to rule it until 1830.

Geography[edit]

Milos, Kimolos (north), Polyaigos (East), Antimilos (west).

Milos is the southwesternmost island in the Cyclades, 120 kilometres (75 miles) due east from the coast of Laconia. From east to west it measures about 23 km (14 mi), from north to south 13 km (8.1 mi), and its area is estimated at 151 square kilometres (58 sq mi). The greater portion is rugged and hilly, culminating in Mount Profitis Elias 748 metres (2,454 feet) in the west. Like the rest of the cluster, the island is of volcanic origin, with tuff, trachyte and obsidian among its ordinary rocks. The natural harbour is the hollow of the principal crater, which, with a depth diminishing from 70 to 30 fathoms (130–55 m), strikes in from the northwest so as to separate the island into two fairly equal portions (see photo), with an isthmus not more than 18 km (11 mi) broad. In one of the caves on the south coast, the heat from the volcano is still great, and on the eastern shore of the harbour, there are hot sulphurous springs.

Antimelos or Antimilos, 13 miles (21 km) north-west of Milos, is an uninhabited mass of trachyte, often called Erimomilos (Desert Milos). Kimolos, or Argentiera, 1.6 km (0.99 mi) to the north-east, was famous in antiquity for its figs and fuller's earth, and contained a considerable city, the remains of which cover the cliff of St. Andrew's. Polyaigos (also called Polinos, Polybos or Polivo — alternative spelling Polyaegos) lies 2 km (1 mi) south-east of Kimolos. It was the subject of dispute between the Milians and Kimolians. It is now uninhabited.

The harbour town is Adamantas; from this there is an ascent to the plateau above the harbour, on which are situated Plaka, the chief town, and Kastro, rising on a hill above it, and other villages. The ancient town of Milos was nearer to the entrance of the harbour than Adamas, and occupied the slope between the village of Trypiti and the landing-place at Klima. Here is a theatre of Roman date and some remains of town walls and other buildings, one with a fine mosaic excavated by the British school at Athens in 1896. Numerous fine works of art have been found on this site, notably the Aphrodite in Paris, the Asclepius in London, and the Poseidon and the archaic Apollo in Athens. Other villages include Triovasalos, Peran Triovasalos, Pollonia and Zefyria (Kampos).

Climate[edit]

Milos has a Mediterranean climate (Köppen climate classification Csa) with mild, rainy winters and warm to hot dry summers.[11]

Climate data for Milos
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 21.6
(70.9)
26.2
(79.2)
25.6
(78.1)
28.4
(83.1)
35.4
(95.7)
40.0
(104)
41.0
(105.8)
38.4
(101.1)
36.3
(97.3)
32.0
(89.6)
27.8
(82)
23.4
(74.1)
41.0
(105.8)
Average high °C (°F) 12.9
(55.2)
13.2
(55.8)
14.8
(58.6)
18.4
(65.1)
22.8
(73)
27.1
(80.8)
28.1
(82.6)
27.6
(81.7)
25.2
(77.4)
21.3
(70.3)
18.0
(64.4)
14.6
(58.3)
20.3
(68.5)
Daily mean °C (°F) 10.5
(50.9)
10.7
(51.3)
12.1
(53.8)
15.2
(59.4)
19.3
(66.7)
23.5
(74.3)
25.0
(77)
24.6
(76.3)
22.3
(72.1)
18.5
(65.3)
15.3
(59.5)
12.3
(54.1)
17.4
(63.3)
Average low °C (°F) 8.5
(47.3)
8.5
(47.3)
9.6
(49.3)
12.4
(54.3)
15.9
(60.6)
19.8
(67.6)
21.8
(71.2)
21.6
(70.9)
19.6
(67.3)
16.1
(61)
13.1
(55.6)
10.3
(50.5)
14.8
(58.6)
Record low °C (°F) −2.0
(28.4)
−2.0
(28.4)
0.0
(32)
5.4
(41.7)
8.0
(46.4)
10.0
(50)
14.0
(57.2)
14.2
(57.6)
11.6
(52.9)
8.0
(46.4)
2.8
(37)
0.0
(32)
−2.0
(28.4)
Precipitation mm (inches) 74.7
(2.941)
50.6
(1.992)
47.2
(1.858)
20.5
(0.807)
13.1
(0.516)
3.3
(0.13)
0.3
(0.012)
1.4
(0.055)
5.8
(0.228)
42.9
(1.689)
60.7
(2.39)
90.3
(3.555)
410.8
(16.173)
Avg. precipitation days (≥ 1.0 mm) 8.8 7.3 5.7 2.9 1.4 0.3 0.1 0.1 0.9 3.9 5.8 9.0 46.2
 % humidity 73.3 72.5 72.0 67.0 63.5 58.8 60.1 63.4 66.8 71.3 73.9 73.7 68.0
Source: NOAA[12]

Natural resources[edit]

View of a mine
The bay of Milos

Bentonite, perlite, pozzolana and small quantities of kaolin are actively collected via strip mine or open-pit mine techniques in Milos and sold all over the world. In the past, baryte, sulfur, millstones and gypsum were also mined; in fact, Pliny notes that Milos was the most abundant source of sulfur in the ancient world.[13] In ancient times the alum of Milos was reckoned next to that of Egypt (Pliny xxxv. 15 [52]). The Melian earth was employed as a pigment by ancient artists. Milos was a source of obsidian during the Neolithic ages for the Aegean and Mediterranean. Orange, olive, cypress, tamarisk, juniper (Juniperus oxycedrus) and arbutus trees grow throughout the island, which, however, is too dry to have any profusion of vegetation. Vines, cotton and barley are the main crops.

Beaches[edit]

A coast
The steep beach of Tsigrado

There are about 70 beaches on Milos Island. Hivadolimni Beach is the longest at about 1 kilometre (0.62 mi). The rest of the beaches are starting from (North): Sarakiniko Beach, Papafragas, Kapros, Pachena, Alogomantra, Konstantinos, Mitakas, Mantrakia, Firopotamos, Nerodafni, Lakida, Plathiena, Fourkovouni, Areti, Pollonia, Gourado and Filakopi. (South): Firiplaka, Paliochori, Provatas, Tsigrado, Agia Kyriaki, Psaravolada, Kleftiko, Gerontas, Gerakas, Agios Sostis, Mouchlioti, Katergo, Spathi, Firligos, Pialothiafes, Kalamos, Krotiraki, Psathi, Svoronou and Sakelari. (West): Agios Ioannis, Cave of Sikia, Agathia, Triades and Ammoudaraki. (East): Voudia, Thalassa, Paliorema, Tria Pagidia and Thiafes. (In the Bay Area): Hivadolimni, Lagada, Papikinou, Fatourena, Klima, Skinopi and Patrikia. The North and South and bay beaches are tourist attractions. The east beaches are very quiet, and those to the west are also quiet beaches.

Demographics[edit]

Historical population[edit]

Year Island population
1907 17,638
1991 4,380
2001 4,771
2011 4,977

Notable people[edit]

Sister island[edit]

Gallery[edit]

See also[edit]

References[edit]

  1. ^ Detailed census results 2011 (Greek)
  2. ^ British Museum Collection [1]
  3. ^ N. Laskaris, A. Sampson, F. Mavridis, I. Liritzis, (September 2011) "Late Pleistocene/Early Holocene seafaring in the Aegean: new obsidian hydration dates with the SIMS-SS method" Journal of Archaeological Science, Volume 38, Issue 9, pp.2475–2479
  4. ^ C. Renferew
  5. ^ a b David Abulafia (2011). The Great Sea: A Human History of the Mediterranean. Penguin Books. ISBN 978-0-14-196999-2. 
  6. ^ a b Chalk and Jonassohn, 65
  7. ^ Flying fish
  8. ^ CAH pg. 448
  9. ^ a b Dinah L. Shelton, www.enotes.com
  10. ^ Thucydides. History of the Peloponnesian War, Chapter 17.
  11. ^ Kottek, M.; J. Grieser; C. Beck; B. Rudolf; F. Rubel (2006). "World Map of the Köppen-Geiger climate classification updated". Meteorol. Z. 15 (3): 259–263. doi:10.1127/0941-2948/2006/0130. Retrieved January 29, 2013. 
  12. ^ "Milos Climate Normals 1961-1990". National Oceanic and Atmospheric Administration. Retrieved January 29, 2013. 
  13. ^ C.Michael Hogan. 2011. Sulfur. Encyclopedia of Earth, eds. A.Jorgensen and C.J.Cleveland, National Council for Science and the environment, Washington DC
  14. ^ Gould, John (1838). Biographical dictionary of painters, sculptors, engravers, and architects, from the earliest ages to the present time: interspersed with original anecdotes, Volume 2. Greenland. p. 577. OCLC 261336841. "VASSILACCHI, called L'ALI- ENSE (Antonio), a Greek historical painter, born at Milo, a Greek island in the Venetian territory, in 1556, and died in 1629" 

Sources[edit]

External links[edit]