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See also:SUDAN (Arabic Bilad-es-Sudan, See also:country of the blacks) , that region of See also:Africa which stretches, See also:south of the See also:Sahara and See also:Egypt, from Cape Verde on the See also:Atlantic to See also:Massawa on the Red See also:Sea . It is bounded S . (I) by the maritime countries of the See also:west See also:coast of Africa, (2) by the See also:basin of the See also:Congo, and (3) by the See also:equatorial lakes, and E. by the Abyssinian and Galla high-lands . The name is often used in See also:Great See also:Britain in a restricted sense to designate only the eastern See also:part of this vast territory, but it is properly applied to the whole See also:area indicated, which corresponds roughly to that portion of See also:negro Africa See also:north of the See also:equator under See also:Mahommedan See also:influence . The terms Nigritia and Negroland, at one See also:time current, referred to the same region . The See also:Sudan has an ethnological rather than a See also:physical unity, and politically it is divided into a large number of states, all now under the See also:control of See also:European See also:powers . These countries being separately described, brief See also:notice only is required of the Sudan as a whole . Within the limits assigned it has a length of about 4000 m., extending southwards at some points See also:I000 m., with a See also:total area of over 2,000,000 sq. m., and a See also:population, approximately, of 40,000,000 . Between the arid and sandy See also:northern wastes and the well-watered and arable Sudanese lands there is a transitional See also:zone" of level grassy See also:steppes (partly covered with mimosas and acacias) with a mean breadth of about 6o m . The zone lies between 17° and 18° N., but towards the centre reaches as far south as 15° N . Excluding this transitional zone, the Sudan may be described as a moderately elevated region, with extensive open or See also:rolling plains, level plateaus, and abutting at its eastern and western ends on mountainous See also:country . Crystalline rocks, granites, gneisses and See also:schists, of the Central See also:African type, occupy the greater part of the country . Towards the south-See also:east, slates, quartzites and See also:iron-bearing schists occur, but their See also:age is not known . The Congo sandstones do not appear to extend as far north . The Nubian See also:sandstone See also:borders the Libyan See also:desert on the south and south-west, but it is doubtful if this sandstone is of Cretaceous or earlier date . The Sudan contains the basin of the See also:Senegal and parts of three other hydrographic systems, namely: the See also:Niger, draining southwards to the Atlantic; the central depression of See also:Lake See also:Chad; and the See also:Nile, flowing northwards to the Mediterranean . Lying within the tropics and with an See also:average See also:elevation of not more than 1500 to 2000 ft. above the sea, the See also:climate of the Sudan is hot and in the See also:river valleys very unhealthy . Few parts are suitable for the See also:residence of Europeans . Cut off from North Africa by the Saharan desert, the inhabitants, who belang in the See also:main to the negro See also:family proper, are thought to have received their earliest See also:civilization from the East . Arab influence and the Moslem See also:religion began to be See also:felt in the western Sudan as See also:early as the 9th See also:century and had taken deep See also:root by the end of the Ilth . The existence of native See also:Christian states in See also:Nubia hindered for some centuries the spread of See also:Islam in the eastern Sudan, and throughout the country some tribes have remained See also:pagan . It was not until the last See also:quarter of the 19th century that the European nations became the ruling force . The terms western, central and eastern Sudan are indicative of See also:geographical position merely . The various states are politically divisible into four See also:groups: (I) those west of the Niger; (2) those between the Niger and Lake Chad; (3) those between Lake Chad and the basin of the Nile; (4) those in the upper Nile valley . The first See also:group includes the native states of See also:Bondu, Futa Jallon, Masina, Mossi and all the tribes within the great See also:bend of the Niger . In the last quarter of the 19th century they See also:fell under the control of See also:France, the region being styled officially the See also:French Sudan . In 1900 this See also:title was abandoned . The greater part of what was the French Sudan is now known as the Upper Senegal and Niger See also:Colony (see SENEGAL, FRENCH WEST AFRICA, &C.) . The second group of Sudanese states Ernttrma'ttXA is almost entirely within the See also:British See also:protectorate of Northern See also:Nigeria . It includes the sultanate of See also:Sokoto and its dependent emirates of See also:Kano, See also:Bida, See also:Zaria, &c., and the See also:ancient sultanate of See also:Bornu, which, with See also:Adamawa, is partly within the See also:German colony of Cameroon (see NIGERIA and CAMEROON) . The third or central group of Sudanese states is formed of the sultanates of See also:Bagirmi (q.v.) with Kanem and See also:Wadai (q.v.) . Wadai was the last See also:state of the Sudan to come under European influence, its See also:conquest being effected in 1909 . This third group is included in French Congo (q.v.) . The See also:fourth group consists of the states conquered during the 19th century by the Egyptians and now under the See also:joint control of Great Britain and Egypt . These countries are known collectively as the Anglo-See also:Egyptian Sudan (see below) . For the regions west of Lake Chad the See also:standard See also:historical See also:work is the Travels of Dr Heinrich See also:Barth (5 vols., See also:London, 1857-1858) . Consult also P . C . See also:Meyer, Erforschungsgeschichte and Staatenbildungen See also:des Westsudan (See also:Gotha, 1897), an admirable See also:summary with bibliography and maps; Karl Kumm, The Sudan (London, 1907); See also:Lady A as° B 30° C 35° D s~g~j « y~ _ See also:rc ) _ Ed t All 10–E'gYPtlall 1 ai t t rKL atar{a ..n (Eb ) Jab 1St IT ,~tS sipAVHabb . SUDAN 0 AMb BbM1` lurr t ,+` c R ~~o 1 t b a m +cB_ snare' K na ' N +blfrp~, g f See also:Art D Igo D---2: ~"E—Y[Yif }-(q - IIo See also:English See also:Miles O Su' .00 seo J d . H t d p b / 'EN'S' AE 4 o ~e 4Ro~ yO Raihuays-r-• Dermot, routes —~ a tl av•;.y See also:tin ~:^ A See also:Cataract d Ca dots erectness O Uongola p ee S f m (El See also:Orel) 1 m E . :', f + 0 IF t • An r ieii naa 4 .J clloc r c 1, See also:Ea. tit ^.~ i, R a b), to.a. k~ r~~ W. a " •See also:Hit Nat ron 2'1 lM B° Z tm • 8 ~ QSd Yd ~ T ha T KA . 0 2 ' L I V SLQG B Ed D Ed Danrf EI Huai., Q ¢ .. a t~ D O N •- "l..,F~ F+:i1FrM.t1~a, • D e r Ada/ \ ., ti / al J " 9Q °1~ G a;~ e Y t 3, s m n dI"a n }F st P eu rR hCa See also:rod ti ~ ~Y y .. . '~ .. c t a sat r+ K8arta t C` II t$ -- 3 •i 7 itiP f 2 5 t' ;rk besh~" y_ 1.} ' C :- .e . .See also:ram p ,9.^ t acn .;Tali ee u •:B r r io C:n 1 L ai •See also:Leda a.-p, ' (ut .a.~ N lQ n f: +r,...,\ c , DaeitYt s wt +ro .'Z See also:ice ..-;, • !Path El Obef• CC °s° yls . "~ ta- K dq on" abaft q a .aM1 f• fil G t: + . W . b ZuC +See also:Dee •; x` a oy` . 3 )r sl f U R G~ ,' CJ f, , eb Q r.: - ` . ., Y NOOOaipfi M° galor; Rewires ° r r i dt Z e, 4;6. c t D qaF A N wa „a,*J {• 7 T > ao•tt . ~J "s iGas z P F i cs ; , a et~be ~a "' cc . --%, . J,°a r EO° • Wu .. See also:fry ;A•7d >~~ ~ . 4•~ o . ,. i 8,91•C+,/y1 ~'O <nsal) ',a F~•E t .... + a. m ° t ~(f 4 ;T, p el Ba rN-Arab tr L3 R Yt.Abta16 ° Yang* ,r ° tr ijll _ . a r ~S ,y1lt .r 4 See also:star 'y: D Wi 4' ...a ..h , eA r (See also:Weir t" w AFp - $ _ Bor e . s° See also:Mead N G A L, t~` Aa L . t o , as / d .tip ~` dAE "' alit a "T PQ 9eH ~' RE GaruL• ~r triode rJ E .e/ . . . M sk'Q 464 .. La e , AJK ma Oeh ke } G, ,a7 Oi .
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See also:Lugard, A Tropical Dependency (London, 1905) ; and the See also:bibliographies given under the various countries named
.
For See also:sources and See also:history see See also:TIMBUKTU
.
For the central Sudan the most important work is that of Gustav See also:Nachtigal, Sahara and Sudan (3 vols., See also:Berlin 1879-1889)
.
See also See also:Boyd See also: |
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