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Greece: Travel Guide: Milos
Greece:
Cyclades
islands:
Milos
Milos is the southwesternmost island in the
Cyclades group, 120 km (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 mi), and its area is estimated at 151 km ²
(58.3 mi²). The greater portion is rugged and hilly, culminating in
Mount Profitis Elias 748 m (2454 ft) 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 to 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 miles) 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 (20 km)
north-west of Milos, is an uninhabited mass of trachyte, often
called Erimomilos (Desert Milos). Kimolos, or Argentiera, 1.6 km (1
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 south-east of Kimolos. It was the subject of dispute between the
Milians and Kimolians. It is now uninhabited.
Bentonite, perlite, pozzolana and small quantities
of kaolin are mined in Milos and sold all over the world. In the
past, baryte, sulfur, millstones and gypsum were also mined. 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, Cedar (Juniperus Cedaris) and arbutus trees grow
throughout the island, which, however, is too dry to have any
profusion of vegetation. The vine, the cotton plant and barley are
the main objects of cultivation.
The harbour town is Adamas; 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 Tripiti 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 Venus de Milo in the Louvre, the Asclepius in the
British Museum, and the Poseidon and an archaic Apollo in Athens.
Other villages include Triovasalos, Pera Triovasalos, Pollonia and
Zefyria (Kampos).
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