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MELDS (mod. Milo)

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Originally appearing in Volume V18, Page 99 of the 1911 Encyclopedia Britannica.
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MELDS (mod. Milo)  , an island of the
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Aegean Sea (
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Cyclades
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group), at the S.W. corner of the
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archipelago, 75 M. due E. from the coast of Laconia . From E. to W. it
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measures about 14 m., from N. to S . 8 m., and its
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area is estimated at 52 q. m . The greater portion is rugged and hilly, culminating in Mount Elias in the west (2538 ft.) . Like the rest of the cluster, the island is of volcanic origin, with tuff, trachyte and
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obsidian among its ordinary rocks . The natural harbour, which, with a
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depth diminishing from 70 to 30 fathoms, strikes in from the north- west so as to cut the island into two fairly equal portions, with an isthmus not more than i; m. broad, is the hollow of the prin- cipal
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crater . In one of the caves on the south coast the heat isstill
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great, and on the eastern
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shore of the harbour there are hot sulphurous springs .
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Sulphur is found in abundance on the top of Mount Kalamo and elsewhere . In ancient times the
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alum of Melos was reckoned next to that of
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Egypt (Pliny
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xxxv. i5 [52]), and millstones, salt (from a marsh at the east end of the harbour), and
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gypsum are still exported . The Melian earth (
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yii M,l?cas) was employed as a pigment by ancient artists . Orange, olive, cypress and arbutus trees grow throughout the island, which, however, is too dry to have any profusion of vegetation . The
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vine, the cotton plant and barley are the main
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objects of cultivation .

Pop . (1907), 4864 (

commune), 12,774 (province) . The harbour
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town is Adamanta; 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 Melos was nearer to the entrance of the harbour than Adamanta, and occupied the slope between the
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village of Trypete and the landing-place at Klima . Here is a theatre of
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Roman date and some remains of town walls and other buildings, one with a
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fine mosaic excavated by the
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British school at Athens in 1896 . Numerous fine
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works of
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art have been found on this site, notably the
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Aphrodite of Melos in the Louvre, the Asclepius in the British Museum, and the
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Poseidon and an archaic Apollo in Athens . The position of Melos, between
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Greece and Crete, and its possession of obsidian, made it an important centre of early Aegean
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civilization . At this time the chief settlement was at the place now called Phylakopi, on the north-east coast . Here the excavations of the British school cleared many houses, including a palace of " Mycenaean" type; there is also a town wall .
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Part of the site has been washed away by the sea . The antiquities found were of three main periods, all preceding the Mycenean age of Greece . Much pottery was found, including examples of a
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peculiar style, with decorative designs, mostly floral, and also considerable deposits of obsidian .

There are some traditions of a Phoenician occupation of Melos . In

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historical times the island was occupied by
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Dorians from Laconia . In the 6th century it again produced a remarkable series of vases, of large
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size, with mythological subjects and orientalizing ornamentation (see GREEK ART, fig . 9), and also a series of terra-cotta reliefs . Though Melos inhabitants sent a contingent to the Greek
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fleet at
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Salamis, it held aloof from the Attic
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league, and sought to remain neutral during the Peloponnesian War . But in 416 B.C. the Athenians, having attacked the island and compelled the Melians to surrender, slew all the men capable of bearing arms, made slaves of the
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women and children, and introduced 500 Athenian colonists . Lysander restored the island to its Dorian possessors, but it never recovered its former prosperity . There were many Jewish settlers in Melos in the beginning of the Christian era, and
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Christianity was early introduced . During the " Frankish " period the island formed part of the duchy of
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Naxos, except for the few years (1341–1383) when it was a
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separate lordship under Marco Sanudo and his daughter . Antimelos or Antimilo, 5i M. north-west of Milo, is an uninhabited mass of trachyte, often called Eremomilo or
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Desert Melos . Kimolos, or Argentiera, less than r m. to the north-east, was famous in antiquity for its
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figs and fuller's earth (KcµwAia yi), and contained a considerable city, the remains of which cover the cliff of St Andrews . Polinos, Polybos or Polivo` (anc .

Polyaegos) lies rather more than a mile south-east of Kimolos . It was the subject of dispute between the Melians and Kimolians . It has

long been almost uninhabited . See Leycester, " The Volcanic Group of Milo, Anti-Milo, &c.," in Jour . Roy . Geog .
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Soc . (1852) ; Tournefort, Voyage; Leake,
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Northern Greece, iii . ; Prokesch von Osten, Denkwurdigkeiten, &c.; Bursian, Geog. von Griechenland, ii.; Journ . Hell .
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Stud. xvi., xvii., xviii.; Excavations at Phylakopi ; Incr.
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gram xii. iii . 197 sqq .

; on coins found in 1909, see

Jameson in Rev . Num . 1909, 188 sqq . (E .

End of Article: MELDS (mod. Milo)
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