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SANTORIN (corruption of St Irene; anc...

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Originally appearing in Volume V24, Page 196 of the 1911 Encyclopedia Britannica.
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SANTORIN (corruption of St See also:Irene; anc. See also:THERA)  , a volcanic See also:island in the See also:Aegean See also:Sea, the southernmost of the See also:Sporades . In shape See also:Santorin forms a See also:crescent, and encloses a See also:bay on the See also:north, See also:east and See also:south, while on the western See also:side lies the smaller island of Therasia . The encircling See also:wall thus formed, which is elliptical in shape and 18 m. See also:round in its inner rim, is broken in two places—towards the north-See also:west by a strait a mile in breadth, where the See also:water is not less than 1100 ft. deep, and towards the south-west by an See also:aperture about 3 M. wide, where the water is shallow, and an island called Aspronisi or See also:White Island lies in the See also:middle . The cliffs rise perpendicularly from the bay, in some places to the height of l000 ft.; but towards the open sea, both in Santorin and Therasia, the ground slopes gradually away, and has been converted into broad level terraces, every-where covered with tufaceous See also:agglomerate, which, though See also:bare and ashen, produces the famous Santorin See also:wine . Towards the south-east rises the See also:limestone See also:peak of See also:Mount See also:Elias, the highest point of the island (1910 ft.); this existed before the See also:volcano was formed . In the middle of the See also:basin See also:lie three small islands, which are the centre of volcanic activity, and are called Palaea, Mikra and Nea Kaumene, or the Old, the Little and the New Burnt Island; the highest of these, Nea Kaumene, is 351 ft. above the sea . Owing to the See also:depth of the water there is no anchorage, and vessels have to be moored to the See also:shore, except at one point in the neighbourhood of the See also:modern See also:town, where there is a slight rim of shallow bottom . The cliffs of Santorin and Therasia are marked in See also:horizontal bands by See also:black See also:lava, white porous tufa, and other volcanic strata, some parts of which are coloured dark red . The modern town of See also:Thera (or Phera, as it is more commonly pronounced) is built at the edge of these, overlooking the middle of the bay at a height of 900 ft. above the water, and the See also:foundations of the houses and in some cases their sides also, are excavated in the tuf a, so that occasionally they are hardly traceable except by their chimneys . Owing to the See also:absence of See also:timber—for, except. the fig, See also:cactus and See also:palm, there are hardly any trees in the island—they are roofed with See also:barrel vaults of See also:stone and See also:cement . Both See also:wood and water have occasionally to be imported from the neighbouring islands, for there are no See also:wells, and the See also:rain water, collected in cisterns, does not always suffice .. The largest of the other villages is Apanomeria, near the See also:northern entrance, which is crowded together in a white See also:mass, while the rocks below it are the reddest in the island .

Santorin is closely connected with the See also:

earthquake movements to which the countries in the neighbourhood of the Aegean are subject . It is hardly accurate to speak of the basin which forms the See also:harbour as a See also:crater, for most geologists support the view that the whole of this space was once covered by a single volcanic See also:cone, the incline of which is represented by the outward slope of Santorin and Therasia, while the position of the crater was that now occupied by the Kaumene Islands; and that owing to a volcanic See also:explosion and the subsidence of the strata the basin was formed . The Kaumene Islands arose subsequently, and that of Palaea Kaumene is considered to have been prehistoric . The See also:principal eruptions that have taken See also:place within historic times are that of 196 B.c., when, as we learn from See also:Strabo (i . 3, § 16, p . 57), flames See also:rose from the water See also:half-way between Thera and Therasia for four days; that of A.D . 726, during the reign of the See also:Emperor See also:Leo the Isaurian (on both these occasions islands were thrown up, 'but it is supposed that they after-wards disappeared); that of 157o, when Mikra Kaumene arose; that of 165o, which destroyed many lives by noxious exhalations, and ended in the upheaval of an island in the sea to the north-east of Santorin, which afterwards subsided and became a See also:reef below sea-level; that of 1707, when Nea Kaumene arose; and that of 1866, when Nea Kaumene was extended towards the south and enlarged threefold . In the See also:southern parts both of Santorin and Therasia pre-historic dwellings have been found at some height above the sea, and there is no doubt that these date from a See also:period antecedent to the formation of the bay . This is proved by their position underneath the layer of tufa which covers the islands, and by these layers of tuf a being broken off precipitously, in the same way as the lava-rocks, a fact which can only be explained by the supposition that they all See also:fell in together . The foundations of the dwellings rested, not on the tufa, but on the lava below it; and here and there between the stones branches of See also:wild See also:olive were found, according to a mode of See also:building that still prevails in the island, in See also:order to resist the shocks of earthquakes . Very few implements of See also:metal were found . Some of the vases found were Cretan See also:ware which had been imported; and the See also:correspondence between these and various specimens of the native pottery proves that to some extent this See also:primitive See also:art was derived from See also:Crete .

In See also:

Greek See also:legend the island of Thera was connected with the See also:story of the See also:Argonauts, for it was represented as sprung from a clod of See also:earth which was presented to those heroes by See also:Triton (Apollon., Argonaut., hr., 1551 sq., 1731 sq.) . According to See also:Herodotus (iv . 147), a Phoenician See also:colony was established there by See also:Cadmus . Subsequently a colony from See also:Sparta, including some of the Minyae, was led thither by Theras, who gave the island his own name, in place of that of Calliste which it had See also:borne before . But the one event which gave importance to Thera in See also:ancient See also:history was the planting of its famous colony of See also:Cyrene on the north See also:coast of See also:Africa by See also:Battus in 631 B.C., in accordance with a command of the Delphic See also:oracle . The ancient See also:capital, which See also:bore the same name as the island, occupied a site on the eastern coast now called Mesavouno, between Mount Elias and the sea . Since 1895 this place has been excavated by See also:Baron See also:Hiller von Gartringen and other See also:German explorers . There are extensive ancient cemeteries . A steep ascent leads from a Heroum of See also:Artemidorus to the See also:Agora; in its neighbourhood were the See also:Stoa Basilice, a vast See also:hall with a See also:row of pillars; a See also:temple of See also:Dionysus and the See also:Ptolemies, which at a later period was dedicated to the Caesars; and the barrack of the See also:garrison of the Ptolemies and a gymnasium . The names which occur here remind us that Thera, as a member of the See also:League of the See also:Cyclades, was from B.C . 308 to 145 under the See also:protectorate of the Ptolemies . The See also:main See also:street has narrow lanes diverging from it to right and See also:left; one of these leads to the See also:sanctuary of the See also:Egyptian gods .

Near the street there is a small See also:

theatre, beneath the seats of which a vast cistern was constructed, arranged so that rain-water should drain into it from the whole of the auditorium . The way then descends south-eastwards first to the temple of See also:Ptolemy Euergetes III., and then to that of . See also:Apollo Carneius; finally, at the point where the rocks fall precipitously, there is a gymnasium of the See also:Ephebi . Numerous See also:rock-carvings and See also:inscriptions have been discovered,as well as statues and vases of various periods . Near the western See also:foot of Mount Elias is the temple of Thea Basileia, which, though very small, is perfect throughout even to the roof . It is now dedicated to St See also:Nicolas Marmorites . See also:Tournefort mentions that in his See also:time nine or ten chapels were dedicated to St See also:Irene, the See also:patron See also:saint of the place; the name Santorin was given to the island after the See also:fourth crusade, when the See also:Byzantine See also:empire was partitioned among the Latins, and the island formed a portion of the duchy of the See also:Archipelago . Santorin is prosperous, for, in addition to the wine See also:trade, there is a large export of pozzolana, which, when mixed with See also:lime, forms a hard cement . Santorin (officially Thera) is a See also:province in the See also:department of the Cyclades . It is divided into 9 communes (see CYCLADES), with a See also:total See also:population of 19,597 in 1907 . (H . F .

End of Article: SANTORIN (corruption of St Irene; anc. THERA)
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