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SOCIETY ISLANDS (French Archipel de la Societe) . an See also: archipelago of the Pacific Ocean, in the eastern See also: part of Polynesia, between 16° and 18° S., 148° and 1550 W., with a See also: total See also: land See also: area of 637 sq. m., belonging to See also: France
.
(For map, see PACIFIC OCEAN.) The See also: principal See also: island is See also: Tahiti (q.v.)
.
Part of the archipelago was discovered by Pedro See also: Fernandez Quiros in 1607
.
In 1767 See also: Samuel See also: Wallis re-discovered it, and named it See also: King
See also: George's Island
.
In 1768 See also: Louis de Bougainville visited Tahiti, claimed it as French, and named it La Nouvelle Cythere
.
On the 12th of
See also: April 1769 the See also: British expedition to observe the transit of See also: Venus, under the See also: naval command of See also: James
See also: Cook, arrived at Tahiti
.
On this first voyage (he subsequently re-visited the islands twice) he named the Leeward See also: group of islands Society in honour of the Royal Society, at the instigation of which the expedition had been sent; Tahiti and the adjacent islands he called Georgian, buL the first name was subsequently adopted for the whole group
.
In 1772 and 1774 the islands were visited by a See also: Spanish See also: government expedition, and some attempt was made at colonization
.
In 1788 See also: Lieutenant See also: Bligh of the " Bounty " spent some See also: time at Tahiti, to which island the See also: historical See also: interest now passes
.
The archipelago is divided into two groups—the Leeward (Iles sous le Vent) and the Windward Islands (Iles du Vent)—by a clear channel of 6o m. in breadth
.
The Leeward Islands are Tubai or Motuiti, a small uninhabited lagoon island, the most See also: northern of the group; Marua or Maupiti—" See also: Double See also: Mountain," the most western; Bola-Bola or See also: Bora-Bora; Huaheine; Raiatea or Ulietea (Spanish.Princessa), the largest island of this cluster, and Tahaa, which approach each other very closely, and are encircled by one See also: reef
.
To the west lie the small See also: groups of See also: coral islets—Mopiha (See also: Lord See also: Howe), Ura (Scilly) and Bellingshausen (discovered by See also: Otto von Kotzebue, 1824)
.
To the Windward Islands belong Tapamanu or Majaiti (Wallis's See also: Sir See also: Charles Saunders's Island and Spanish Pelada); Moorea or Eimeo (Wallis's Duke of
See also: York Island and Spanish See also: San Domin_go); Tahiti—Cook's Otaheite (probably Quiros's Sagittaria; Wallis's King George's Island, Bougainville's Nouvelle Cythere and Spanish See also: Isla d'Amat) ; Tefuaroa—" The Distant See also: Sea " (
?
Quiros's Fugitiva; Bougainville's Umaitia and Spanish Tres Hermanos) ; and Maitea (
?
Quiros's La Dezana, Wallis's See also: Osnaburg Island, Bougainville's Boudoir and See also: Pie de la Boudeuse and Spanish Cristoval), the most eastern and See also: southern of the archipelago
.
Tetuaroa and Tubai, besides the three western Leeward Isles, are coral atolls
.
The length of the Tetuaroa reef ring is about six See also: miles; it bears twelve palm-covered islets, of which several are inhabited, and has one narrow boat-passage leading into the lagoon
.
With the exception just named, the islands, which agree very closely in See also: geological structure, are mountainous, and See also: present, perhaps, the most wonderful example of volcanic rocks to be found on the globe
.
They are formed of See also: trachyte, dolerite and See also: basalt
.
There are raised coral beds high up the mountains, and See also: lava occurs in a variety of forms, even in solid flows; but all active volcanic agency has so long ceased that the craters have been almost entirely obliterated by denudation
.
Hot springs are unknown, and earthquakes are slight and rare
.
Nevertheless, under some of these flows remains of See also: plants and See also: insects of See also: species now living in the islands have been found—a proof that the formation as well as the denudation of the country is, geologically speaking, See also: recent
.
In See also: profile the islands are rugged and elevated (7349 ft. in Tahiti, Moorea 4045 ft., Raiatea 3389, Bola-Bola 2165)
.
A mountain, usually with very steep peaks, forms the centre, if not the whole island ; on all sides steep ridges descend to the sea, or, as is oftener the See also: case, to a considerable See also: belt of flat land
.
These mountains, excepting some stony crags and cliffs, are clothed with dense See also: forest, the See also: soil being exceptionally fertile
.
All voyagers agree that for varied beauty of See also: form and colour the Society Islands are unsurpassed in the Pacific
.
Innumerable rills gather in lovely streams, and, after heavy rains, torrents precipitate themselves in See also: grand cascades from the mountain cliffs--a feature so striking as to have attracted the See also: attention of all voyagers, from Wallis downwards
.
Round most of the islands there is a luxuriant coral growth; but, as the reefs lie at no See also: great distance, and follow the See also: line of the See also: coast, the inter-island channels are comparatively safe
.
Maitea, which rises from the sea as an exceedingly abrupt See also: cone, and Tapamanu, appear to be the only islands without almost completely encircling barrier-reefs
.
The coasts are fairly indented, and, protected by these reefs, which often support a chain of See also: green islets, afford many See also: good harbours and safe anchorages
.
In this respect the Society Islands have the See also: advantage of many Polynesian islands
.
The populations of the chief islands are: Tahiti 10,300, Moorea 1600, Raiatea and Tahaa 2300, Huaheine 1300, Bola-Bola 800; and that of the whole archipelago is about 18,500
.
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