FREE BOOKS

Author's List




PREV.   NEXT  
|<   573   574   575   576   577   578   579   580   581   582   583   584   585   586   587   588   589   590   591   592   593   594   595   596   597  
598   599   600   601   602   603   604   605   606   607   608   609   610   611   612   613   614   615   616   617   618   619   620   621   622   >>   >|  
ntly to the depression from the south, east and north, and into it drain a considerable number of streams, turning the greater part into a morass of reeds and papyrus. The term Bangweulu is sometimes applied to the whole depression, but is properly confined to the area of clear water. Only on its south-west and western sides are the banks of the lake clearly defined. The greatest extent of open water is about 60 m. N. to S. and 40 m. E. to W. Long narrow sandbanks almost separate Chifunawuli, the western pan of the lake, from the main body of water, while the water surface is further diminished by a number of islands. The largest of these islands, Kirui (Chiru), lies on the east side of the lake close to the swamp. Kisi (Chishi) is a small island occupying a central position just south of 11deg S., and Mbawali, 20 m. long by 3 broad, lies south of Kisi. South of Bangweulu the swamp extends to 12deg 10' S. Into this swamp on its east side flows the Chambezi, the most remote head stream of the Congo. Without entering the lake the Chambezi mingles its waters in the swamp with those of the Luapula. The Luapula, which leaves Bangweulu at its most southern point, is about a mile wide at the outflow, but soon narrows to 300 or so yds. West of the Luapulu and near its outflow lies Lake Kampolombo, 20 m. long and 8 broad at its southern end. A sandy track separates Bangweulu from Kampolombo, and a narrow forest-clad tongue of land called Kapata intervenes between the Luapula and Kampolombo. Various channels lead, however, from the river to the lake. The Luapula flows south through the swamp some 50 m. and then turns west and afterwards north (see CONGO). The flood waters of the Chambezi and other streams, which deposit large quantities of alluvium, are gradually solidifying the swamp, while the Luapula is believed to be, though very slowly, draining Bangweulu. The waters of the lake do not appear to be anywhere more than 15 ft. deep. Though heard of by the Portuguese traveller, Francisco de Lacerda, in 1798, Bangweulu was first reached in 1868 by David Livingstone, who died six years later among the swamps to the [v.03 p.0317] south. It was partially surveyed in 1883 by the French traveller, Victor Giraud, and first circumnavigated by Poulett Weatherley in 1896. See P. Weatherley in _Geog. Journ._ vol. xii. (1898) and vol. xiv. p. 561 (1899); L. A. Wallace in _Geog. Journ._ vol. xxix. (1907), with map by O. L. Beringer. Giraud'
PREV.   NEXT  
|<   573   574   575   576   577   578   579   580   581   582   583   584   585   586   587   588   589   590   591   592   593   594   595   596   597  
598   599   600   601   602   603   604   605   606   607   608   609   610   611   612   613   614   615   616   617   618   619   620   621   622   >>   >|  



Top keywords:

Bangweulu

 

Luapula

 

waters

 
Kampolombo
 

Chambezi

 

outflow

 

Giraud

 
islands
 
narrow
 

southern


traveller

 

number

 

streams

 

depression

 

Weatherley

 
western
 

slowly

 

believed

 

draining

 

solidifying


channels

 

Various

 

called

 

Kapata

 
intervenes
 

deposit

 

quantities

 
alluvium
 
gradually
 

circumnavigated


Victor
 

Poulett

 

French

 

partially

 

surveyed

 

Beringer

 
Wallace
 

Portuguese

 

Francisco

 
Lacerda

Though

 

reached

 

swamps

 
Livingstone
 

leaves

 

sandbanks

 

greatest

 

extent

 

separate

 
diminished