TIERRA DEL FUEGO
, an See also:archipelago at the See also:southern extremity of See also:South See also:America, from which it is separated by See also:Magellan Strait, at the First Narrows and other points scarcely a mile wide
.
The See also:group lies between 52° 40' and 55° 59' S. and 63° 3o' and 74° 30' W. stretching nearly in a See also:line with the Patagonian See also:Andes for over 400 M
.
N.W. and S.E., between Capes See also:Pillar (Desolation See also:Island) and See also:Horn, and for about 270 M
.
W. and E. from Cape Pillar to See also:Catherine Point at the See also:north of the See also:main island of Tierra del Fuego
.
Southwards it tapers to 120 M. between Capes Horn and See also:San Diego, See also:east of which extends Staten Island, which terminates in Cape St See also:John
.
The boundary between See also:Argentina and See also:Chile has been settled in such a manner that Argentina holds that See also:part of the main island of Tierra del Fuego which is situated east of the See also:meridian of Cape Espiritu Santo, the frontier striking the north See also:shore of Beagle Channel about its centre; and Chile holds all the western part of the main island and the other numerous islands to the See also:west and to the south of Beagle Channel
.
The See also:Argentine See also:side is known as the Territory of Tierra del Fuego (including Staten Island), and the Chilean forms part of the Territory of See also:Magallanes
.
Although on See also:ordinary maps this region presents to the See also:eye a hopelessly confused aggregate of islands, channels and See also:fjord-like inlets, it is nevertheless clearly disposed in three main sections: (1) the main island; (2) the islands to the south, from which it is separated by Beagle Channel; (3) the islands to the west, marked off from those to the south by the Brecknock See also:Peninsula
.
Knowledge of these lands increased considerably during the later years of the 19th See also:century, and their reputation for dreariness has been favourably modified
.
The See also:climate in the eastern and southern regions is not so rigorous as was believed, there are no barren lands, the See also:soil is fertile and can support fruitful See also:industries, and the See also:aborigines are far from being so dangerous as they were once considered to be
.
The greater part of the main island of Tierra del Fuego is formed by the continuation of the See also:Tertiary beds of the Patagonian tableland cut by the transversal depression of Magellan Strait and by the See also:low See also:land extending from Useless See also:Bay on the west to San See also:Sebastian Bay on the east, of so See also:recent origin that there exist still some See also:salt lakes, this depression being represented in the old charts as an inter-oceanic passage for small boats
.
Although in 188o numerous prospectors discovered extensive deposits of alluvial See also:gold, its exploitation was not generally successful, and farms took the See also:place of mines
.
By the end of the 19th century reo square See also:miles had been occupied by See also:cattle and See also:sheep on the Argentine side, and about the same extent on the Chilean; and the cattle See also:industry proved very profitable
.
The undulating tableland has an See also:average height of 300 ft. above the See also:sea, and its climate, however See also:cold in See also:winter—in 1892 and 1893 the temperature reached 12.6° F.—allows of the cultivation of See also:barley, oats and occasionally potatoes, which, however, grow better along Beagle Channel
.
To the south the tableland is higher and more broken, being drained by the See also:Silva and Grande, among smaller See also:rivers, the Grande being navigable in some parts by small See also:craft
.
To the west and south-west the See also:general See also:character of the land changes; the ends of the Tertiary beds are raised in small hills and Mesozoic rocks appear, forming broken ridges of the Pre-See also:Cordillera, a name given on the See also:continent to the ridges which precede, to the east, the Andes
.
In this region appears the See also:Antarctic See also:forest in which pre-
dominates the Fagus antarctica and F. betuloides, Drymis Wmteri, Berberis lieifolia, Pernettia, Desfonteinia and Philesia buxifolia
.
See also:Lake Seller and Lake Fagnano receive the See also:waters of these mountains and hills
.
Lake Fagnano is only 18o ft. above the sea, and its See also:depth reaches 700 ft
.
To the south of the lake rises the south-eastern prolongation of the Cordillera of the Andes, with ridges of a See also:uniform height of 3500 ft., in which predominate crystalline See also:schists which do not seem to be very old
.
Some peaks of Tertiary See also:granite break the uniformity, such as Mt Sarmiento (7200 It.), Mt See also:Darwin, of which two peaks have been measured (6201 and 7054 ft.), and Mt Olivaia (4324 ft.)
.
Sarmiento, the culminating point of
the archipelago, was generally supposed to be volcanic, but it presents such extremely precipitous flanks that John See also:Ball considered it more probably " a portion cf the See also:original See also:rock See also:skeleton that formed the See also:axis of the Andean See also:chain during the See also:long ages that preceded the See also:great volcanic outbursts that have covered the framework of the western side of South America."' See also:Sir See also:- MARTIN (Martinus)
- MARTIN, BON LOUIS HENRI (1810-1883)
- MARTIN, CLAUD (1735-1800)
- MARTIN, FRANCOIS XAVIER (1762-1846)
- MARTIN, HOMER DODGE (1836-1897)
- MARTIN, JOHN (1789-1854)
- MARTIN, LUTHER (1748-1826)
- MARTIN, SIR THEODORE (1816-1909)
- MARTIN, SIR WILLIAM FANSHAWE (1801–1895)
- MARTIN, ST (c. 316-400)
- MARTIN, WILLIAM (1767-1810)
Martin See also:Conway, who ascended it, ascertained that it is,not a See also:volcano
.
This is altogether an alpine region with numerous See also:snow-clad summits and glaciers descending down to the sea
.
Deep valleys, which seem to be only the prolongation of fjords, penetrate into the chain in the southern slope where exist several harbours on which settlements have been founded
.
Yendegaia, Lapatia and Ushuaia Bays are among the larger
.
Ushuaia is the site of the See also:capital of the Argentine Territory, and has shown considerable development, having See also:regular communication by monthly steamers with Buenos Aires, while smaller steamers serve the different settlements along the See also:coast
.
Cattle farms prosper along Beagle Channel, the See also:timber industry is growing, See also:lignite seams have been discovered, and alluvial gold is washed principally at Slogget Bay
.
These regions, as they become more known, may even invite the See also:attention of tourists by their See also:sublime scenery
.
Staten Island to the east of Tierra del Fuego has been settled by the Argentine See also:government; there are a See also:prison and lighthouse at St John See also:Harbour, and a first-class permanent meteorological and magnetic station
.
The See also:division of the archipelago to the south of Beagle Channel includes the islands of See also:Hoste, Navarin, See also:Gordon, See also:Londonderry, See also:- STEWART, ALEXANDER TURNEY (1803-1876)
- STEWART, BALFOUR (1828-1887)
- STEWART, CHARLES (1778–1869)
- STEWART, DUGALD (1753-1828)
- STEWART, J
- STEWART, JOHN (1749—1822)
- STEWART, JULIUS L
- STEWART, SIR DONALD MARTIN (1824–19o0)
- STEWART, SIR HERBERT (1843—1885)
- STEWART, SIR WILLIAM (c. 1540—c. 1605)
- STEWART, STUART
- STEWART, WILLIAM (c. 1480-c. 1550)
Stewart, See also:Wollaston and numerous islets, disposed in triangular See also:form with the See also:base on Beagle Channel and the See also:apex at the rocky headland of Cape Horn
.
At its west end Beagle Channel takes the name of Darwin See also:Sound, which leads to the Pacific at the Londonderry and Stewart Islands
.
Partial exploration in this region was conducted by the See also:French See also:Mission du Cap Horn in 1882-1883, and the See also:geological See also:foundations are granite and basic volcanic rocks
.
The western group of islands, demarcated by Brecknock Peninsula, includes See also:Clarence Island and See also:Captain See also:Cook's Desolation Land, with See also:Dawson Island and numerous rocks and islets
.
Desolation Land was supposed by Cook to form a continuous See also:mass stretching from the western entrance of Magellan Strait to See also:Cockburn Channel, but it actually consists of several islands, separated from each other by very narrow channels flowing between the Pacific and the western See also:branch of Magellan Strait
.
The name Desolation is given to the See also:northern member of the group terminating at Cape Pillar; the southernmost and largest island nearer to Clarence Island, is See also:Santa Ines
.
In other cases small surveys among these fjords have shown that several of the larger islands are cut by channels which See also:separate them into smaller ones, while elsewhere the low valleys which unite the mountains and hills are the result of See also:post-Glacial deposits that have filled part of the former channels, these islands being the summits of an old continuous See also:half-submerged See also:mountain chain
.
At Dawson Island the Chilean government has established settlements, and a See also:Roman See also:Catholic mission has carried on See also:work among the Alakaluf See also:Indians
.
Climate.—At Ushuaia ten years' meteorological observations' have shown a mean See also:annual temperature of 42.84° F., with a winter mean of 34.7° and a summer mean of 50.18°
.
These figures show that tolerably mild winters (as a whole, apart from the extremes of cold already indicated) are followed by cool summers, both seasons being accompanied by overcast skies, See also:constant and sudden changes from See also:fair to foul See also:weather; while fogs, mists, rains, snows and high winds (prevailing throughout the See also:year) endanger the See also:navigation of the intricate inland channels
.
The precipitation during ten years at Ushuaia has been observed to average 24.8 in
.
But on the southern seaward islands, under the See also:influence of the prevalent See also:westerly or south-westerly winds, it is very much heavier, and reaches 59 in. at Staten Island
.
See also:Fauna.—In the main island of Tierra del Fuego, the low-lying plains with their See also:rich growth of tall herbage are frequented by the See also:rhea, See also:guanaco and other animals See also:common to the adjoining mainland
.
In the southern and western islands the fauna is restricted mainly to foxes, bats, rats, mice, the sea See also:otter, the See also:penguin and other aquatic birds, and various cetaceans in the surrounding waters
.
Inhabitants.—To the three See also:geographical divisions correspond three well-marked ethnical See also:groups—the Onas of the main island, the Yagans (Yahgans) of the south and the Alakalufs of the west
.
With the See also:settlement of the main island, which is now sometimes called Onisia, leaving the name of Tierra del Fuego to the archipelago, the Onas tribe has become fairly known
.
Their origin, like that of the other groups, is obscure
.
Undoubtedly among these Indians are many that recall some Patagonian types; it seems that they are not the same as the See also:Tehuelche type, but that they pertain to one of the races that in earlier times existed in See also:Patagonia
.
Their See also:language is closely allied to that called Old Tehuelche; it is a hard, slow-spoken speech, not at all resembling the soft, rapidly-spoken language of the Yagans, which has many points
' Notes of a Naturalist in South America (See also:London, 1887)
.
2 Dr Chavanne, See also:Die Temperatur . and Regenverhaltnisse Argentiniens (Buenos Aires, 1903).965
of similarity with that of the Alakalufs
.
The See also:isolation of the Onas is peculiarly marked, inasmuch as they are an insular See also:people who do not use boats
.
Their See also:life is nomadic, and they are hunters, living upon the flesh of the guanaco, and using only tussock-roots and See also:wild See also:celery for See also:vegetable See also:food
.
Their skill in and necessary devotion to the See also:chase influence their whole mode of life; " their moral See also:code is based upon a See also:standard of See also:physical culture and See also:health." 2 They live in small groups, every member of which is connected by See also:family ties; between these groups, as in the See also:case of the Yagans and Alakalufs, the See also:vendetta is common
.
They have no gods, though certain legends are preserved
.
They have maintained their stock untainted, and have withstood the influence of the See also:- WHITE
- WHITE, ANDREW DICKSON (1832– )
- WHITE, GILBERT (1720–1793)
- WHITE, HENRY KIRKE (1785-1806)
- WHITE, HUGH LAWSON (1773-1840)
- WHITE, JOSEPH BLANCO (1775-1841)
- WHITE, RICHARD GRANT (1822-1885)
- WHITE, ROBERT (1645-1704)
- WHITE, SIR GEORGE STUART (1835– )
- WHITE, SIR THOMAS (1492-1567)
- WHITE, SIR WILLIAM ARTHUR (1824--1891)
- WHITE, SIR WILLIAM HENRY (1845– )
- WHITE, THOMAS (1628-1698)
- WHITE, THOMAS (c. 1550-1624)
white See also:man to a remarkable degree (for example, they use no spirituous or fermented drink), though they have suffered a serious decrease in See also:numbers at his hands
.
The men average about 5 ft. io in. in height; the See also:women 5 ft
.
6 in
.
They are of a See also:light See also:copper See also:colour, with See also:black straight See also:hair, and remarkably See also:muscular
.
The Yagans live under conditions of extraordinary rigour
.
In See also:- ORDER
- ORDER (through Fr. ordre, for earlier ordene, from Lat. ordo, ordinis, rank, service, arrangement; the ultimate source is generally taken to be the root seen in Lat. oriri, rise, arise, begin; cf. " origin ")
- ORDER, HOLY
order to obtain food, they venture naked in small canoes into the treacherous seas; their life is a constant See also:battle with See also:starvation and a See also:rude climate, and their character has become rude and low in consequence
.
They have no higher social unit than the family
.
On the authority of See also:Charles Darwin they have been held by many to be cannibals, but they are not, although those suffering from incurable ailments are often put to See also:death
.
Although taller than the Negritoes of the eastern hemisphere (4 ft
.
Io in. to 5 ft
.
4 in.), the Yagans See also:present in some respects a more debased type characterized by low brows, prominent zygomatic See also:arches, large tumid lips, See also:flat See also:nose, loose wrinkled skin, black restless eyes very wide apart, coarse black unkempt hair, and See also:head and See also:chest disproportionately large compared with the extremely slender and outwardly curved legs
.
The missionaries, who have reduced the language to See also:writing (See also:Gospel of St See also:Luke, London, 1881), assert that it contains no fewer than 30,000 words, although the numerals stop at five, already a See also:compound form, and although the same word expresses both See also:hand and See also:finger; but it appears that a large number of the words included in this See also:total are compounds
.
Comparatively little is known about the Alakalufs
.
They have a reputation for treachery, and for assaults on shipwrecked crews
.
They are hunters both on land and on the See also:water, using the See also:bow and arrow like the Onas, and See also:building canoes often of large See also:size
.
The aborigines are decreasing rapidly in the whole archipelago, and although the Rev
.
See also:- THOMAS
- THOMAS (c. 1654-1720)
- THOMAS (d. 110o)
- THOMAS, ARTHUR GORING (1850-1892)
- THOMAS, CHARLES LOUIS AMBROISE (1811-1896)
- THOMAS, GEORGE (c. 1756-1802)
- THOMAS, GEORGE HENRY (1816-187o)
- THOMAS, ISAIAH (1749-1831)
- THOMAS, PIERRE (1634-1698)
- THOMAS, SIDNEY GILCHRIST (1850-1885)
- THOMAS, ST
- THOMAS, THEODORE (1835-1905)
- THOMAS, WILLIAM (d. 1554)
Thomas See also:Bridges, who, as missionary first and then as See also:farmer, resided See also:thirty years there, calculated the See also:population to be io,000 when he arrived, towards the See also:close of the 19th century it was estimated to be little more than See also:i000
.
Tierra del Fuego was discovered by Fernando de Magellan in 1520, when he sailed through the strait named after him, and called this region the " Land of See also:Fire," either from now See also:extinct volcanic flames, or from the fires kindled by the natives along parts of his course
.
In 1578 Sir See also:Francis See also:Drake first sighted the point which in 1616 was named Cape See also:Hoorn (anglicized Horn) by the Dutch navigators See also:Jacob Lemaire and Willem Cornelis Schouten (1615-'617)
.
In 1619 the See also:brothers See also:Garcia and Gongalo de Nodal first circumnavigated the archipelago, which was afterwards visited at intervals by Captain Sir John See also:Narborough (1670), M. de Gennes and the Sieur Froger (1696), See also:Commodore John See also:Byron (1764), See also:Samuel See also:Wallis and See also:- PHILIP
- PHILIP (Gr.'FiXtrsro , fond of horses, from dn)^eiv, to love, and limos, horse; Lat. Philip pus, whence e.g. M. H. Ger. Philippes, Dutch Filips, and, with dropping of the final s, It. Filippo, Fr. Philippe, Ger. Philipp, Sp. Felipe)
- PHILIP, JOHN (1775-1851)
- PHILIP, KING (c. 1639-1676)
- PHILIP, LANOGRAVE OF HESSE (1504-1567)
Philip See also:Carteret (1767), See also:- JAMES
- JAMES (Gr. 'IlrKw,l3or, the Heb. Ya`akob or Jacob)
- JAMES (JAMES FRANCIS EDWARD STUART) (1688-1766)
- JAMES, 2ND EARL OF DOUGLAS AND MAR(c. 1358–1388)
- JAMES, DAVID (1839-1893)
- JAMES, EPISTLE OF
- JAMES, GEORGE PAYNE RAINSFOP
- JAMES, HENRY (1843— )
- JAMES, JOHN ANGELL (1785-1859)
- JAMES, THOMAS (c. 1573–1629)
- JAMES, WILLIAM (1842–1910)
- JAMES, WILLIAM (d. 1827)
James Cook (1768) and James Weddell (1822)
.
But no systematic exploration was attempted until the See also:British See also:Admiralty undertook a thorough survey of the whole group by Philip See also:Parker See also:- KING
- KING (O. Eng. cyning, abbreviated into cyng, cing; cf. O. H. G. chun- kuning, chun- kunig, M.H.G. kiinic, kiinec, kiinc, Mod. Ger. Konig, O. Norse konungr, kongr, Swed. konung, kung)
- KING [OF OCKHAM], PETER KING, 1ST BARON (1669-1734)
- KING, CHARLES WILLIAM (1818-1888)
- KING, CLARENCE (1842–1901)
- KING, EDWARD (1612–1637)
- KING, EDWARD (1829–1910)
- KING, HENRY (1591-1669)
- KING, RUFUS (1755–1827)
- KING, THOMAS (1730–1805)
- KING, WILLIAM (1650-1729)
- KING, WILLIAM (1663–1712)
King (1826–1828) and See also:Robert See also:Fitzroy 1831-1836)
.
The latter expedition (Voyage of the " Beagle") was accompanied by Charles Darwin, then a See also:young man
.
To these admirable surveys is due most of the present geographical terminology of the archipelago
.
Subsequently the work of exploration was continued by See also:Dumont d'Urville (1837), Charles Wilkes (1839), Parker Snow (1855), various later travellers, a selection of whose See also:works are quoted below, and British, See also:American and Roman Catholic missionaries
.
' W
.
S
.
See also:Barclay, " The Land of Magallanes, with some See also:account of the Onas and other Indians," Geographical See also:Journal, vol. See also:xxiii
.
(London, 1904)
.
Lista, " East Fuegia," in Petermanns Mitteilungen (May 1887); Mission stientifique du Cap Horn, 1882-1883 (See also:Paris, 1888); Thomas Bridges, " Notts on Tierra del Fuego," Revista del Museo de la See also:Plata (1892); See also:Otto Nordenskjold, " Ueber die Natur der Magellanslander," See also:- PETER
- PETER (Lat. Petrus from Gr. irfpos, a rock, Ital. Pietro, Piero, Pier, Fr. Pierre, Span. Pedro, Ger. Peter, Russ. Petr)
- PETER (PEDRO)
- PETER, EPISTLES OF
- PETER, ST
Peter
.
Mitt., 43, 1897; L'Expedition suedoise a la Terre de See also:Feu (1895-1897; Wiss
.
Erg. der schwed
.
Exped. nach den Magellonslandern, 1895-1897 (See also:Stockholm, 1898) ; Geological See also:Map of the Magellan Territories (Stockholm, 1899) ; F
.
Lahille, " Fines de verano en la Tierra del Fuego," Revista Museo de La Plata (1898), vol . viii.; Sir Martin Conway, See also:Aconcagua and Tierra del Fuego (London
.
1902) ; R
.
Dabbene, " Viaje a la Tierra del Fuego y a la See also:Isla de los Estados," Bolet
.
Inst
.
Geog
.
Argentine (1905), See also:xx1
.
; K
.
Skotts•• See also:berg, Vegetationsbilder aus Feuerland, &c., parts, and iv. in G
.
See also:Karsten and H
.
Schenck's Vegetationsbilder (See also:Jena, 1906); R
.
Crawshay, The Birds of Tierra del Fuego .(London, 1907)
.
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