CHAPTER XXIV

GERMAN EXPLORERS DETERMINE THE SOUTHERN LIMITS OF THE NILE BASIN

The acquisition by Germany of those interior regions of the Zanzibar

coast-line which now constitute German East Africa led to a

considerable development of exploration in the southernmost regions

of the Nile basin. Prior to 1890 there had been much discussion as to

what was the Nile’s furthest tributary,--what stream, in fact, was the

ultimate source of the Nile. Stanley’s journeys in search of Emin Pasha

had revealed the existence of the Semliki and of Lake Albert Edward,

and had thus extended considerably the length of the Albertine Nile

system. Later on Count Götzen had shown by his remarkable journeys

north from Tanganyika that Lake Kivu (the existence of which had been

already reported by Burton, Speke, and Stanley) was connected with

Tanganyika, and therefore with the Congo. This put a limit to the Nile

basin in that direction, and disposed for ever of the last vestige of

Livingstone’s wild dream, by which the main course of the Nile would

have risen far south of the equator in what we now know to be the basin

of the Congo, and have flowed through Lake Albert instead of through

the Victoria Nyanza. Speke had discovered the important Kagera River

(which he called the Kitangule), and Stanley had extended our knowledge

of this, the largest affluent of the Victoria Nyanza. Stanley had,

in fact, in 1875 christened it the Alexandra Nile, but he was very

much misled about its origin and course, and he made it issue from a

hypothetical lake, Akanyaru,[108] which has no existence, but which

was no doubt in part an exaggeration of swamps along the course of the

Kagera, and in part a confusion with the rumoured Lake Kivu.

The Kagera is now acknowledged to be the extreme head-waters of the

Nile. A distinctly observable current passes across the Victoria

Nyanza from the mouth of the Kagera to the Ripon Falls. In 1891–1893

Dr. Oscar Baumann, a German official, who had previously done some

good exploring work in West Africa, made extensive journeys through

southern Masailand and Unyamwezi to the sources of the Kagera River.

This stream (especially in its upper waters, where it is known as

Ruvuvu), was further explored in 1899–1900 by M. Lionel Dècle, a French

traveller, who had done a great deal to increase our knowledge of

Central Africa.[109] Dr. Kandt,[110] in 1898, and other Germans, have

also put on the map portions of the Kagera’s course, and our knowledge

of this stream has received contributions from Messrs. Racey, Mundy,

and R. W. Macallister, officials of the Uganda Protectorate. The Kagera

River has two principal sources, both of them almost within sight of

the waters of Tanganyika. The stream which is usually taken to be the

more important source rises in south latitude 3° in the country of

Ruziga, about fifteen miles due north of the north end of Tanganyika,

at an altitude of about 6,270 feet above sea-level. Some fifty miles

south-southeast of this point, however, there is another source, which

may be taken to be the southernmost extension of the Nile system. This

fountain, in south latitude 3° 45′, is on the eastern slope of the

Utembera or Kangozi Mountains, only ten miles east of Tanganyika. The

altitude is about 6,300 feet. This would seem to be the farthest source

of the Nile.

[Illustration: A NATIVE OF UNYAMWEZI, FROM NEAR SOUTH SHORES OF

VICTORIA NYANZA.]

Herr Baumann made another contribution of negative value to Nile

exploration. Stanley and some other travellers had believed that the

southernmost source of the Nile lay in the country of Unyamwezi, in

certain streams which flowed northward into the Victoria Nyanza, which

they entered under the name of the river Simiyu or Shimeyu. But in

these deductions they were wrong. Baumann showed that the river Simiyu

was an inconsiderable stream of short course, and that the waters much

further to the south which had been identified with this river really

flowed northeastwards into a largish salt lake, discovered by Baumann

and called Lake Eyasi. Eyasi has no outlet. It is situated in a rift

valley which joins the great Rift valley of Masailand. The journeys

of Baumann and of other Germans considerably curtailed the present

extent of the Nile basin in Unyamwezi. The waters of this somewhat arid

tableland, which apparently is almost below the surface of the Victoria

Nyanza, flow mainly to Tanganyika, to Lake Rukwa, and to Lake Eyasi and

other isolated pools of the rift valleys.

[Illustration:

_Photo by J. Thomson._]

SIR FREDERIC D. LUGARD.]

The Nile quest · 第 24 / 28 章