Through the Dark Continent, Vol. 2 (of 2) : $b or, The sources of the Nile around the Great Lakes of Equatorial Africa and down the Livingstone River to the Atlantic Ocean — John Shaqi
Through the Dark Continent, Vol. 2 (of 2) : $b or, The sources of the Nile around the Great Lakes of Equatorial Africa and down the Livingstone River to the Atlantic OceanStanley, Henry M. (Henry Morton)
History
Through the Dark Continent, Vol. 2 (of 2) : $b or, The sources of the Nile around the Great Lakes of Equatorial Africa and down the Livingstone River to the Atlantic Ocean
Stanley, Henry M. (Henry Morton)
Africa, Central -- Description and travel; Stanley, Henry M. (Henry Morton), 1841-1904 -- Travel -- Africa, Central
There appears to be no diminution in the altitude of the mountain ranges
which lie along the entire east coast of the Tanganika, or on the
western side, as we have had the west mountains plainly in view since
leaving Mpimbwé. Now and then we saw small streams issue into the lake,
but met no river of any importance, until we came to the Zinga, or Mui-
Zinga, as the Wajiji call it, which separates Fipa from Urungu.
_June 30._—On the 30th we were coasting along the base of the mountain
ranges of Urungu, and passing by Kalavera Point came to a bay before
which were two small grass-covered islets. On a point of the mainland,
nearly opposite these, stands Kakungu village. This point is formed of a
grey shaly rock supporting a white clay, out of which the Wajiji on
their return homeward paint the bows of their canoes. The scenery just
beyond is bold and imposing.
Kirungwé Point consists of perpendicular walls—from 50 to 200 feet high
above the lake—of a fine reddish sandstone with horizontal strata. Their
peculiar appearance may be imagined when the boat’s crew cried out:—
“Oh, mother, this is a fort! See, there are the windows, and here is one
of the gates.”
Kirungwé Point appears to be a lofty swelling ridge, cut straight
through to an unknown depth. There seems ground for believing that this
ridge was once a prolongation of the plateau of Marungu, as the rocks
are of the same material, and both sides of the lake show similar
results of a sudden subsidence without disturbance of the strata.
South of Kirungwé, or Castle Point, there lies what we may almost call
an island, which the guides said a few years ago was connected with the
mainland. It is almost entirely separated now. A village which once
nestled comfortably in the hollow between the rising ridges is now half
buried in water. The huts appeared ready to collapse, for the water had
already flooded them. This village was called Ma-Zombé.
In the evening, as we prepared to encamp, four canoes, of Ujiji, loaded
with women and children, to the number of sixty-four—slaves from the
Rufuvu river and from Muriro’s—passed by our camp.
The bay of Kawa, which we passed through next day, is very picturesque;
woods clothe the slopes and heights, and huts for the accommodation of
the Muzimus, or spirits, have been erected in several of the bends. Kawa
river empties into this bay.
_July 2, 3._—During the 2nd and 3rd of July we rowed close to the
uninhabited shore, and at noon of the 3rd arrived at the extreme south
end of the lake—which we ascertained to be 8° 47′ south latitude—in the
district of Ukituta. The little stream Kapata issues into the lake at
this end through a dense and dark grove, the dead trees standing in
front of the grove bearing witness to the destructive action of the
rising waters.
[Illustration: THE EXTREME SOUTHERN REACH OF LAKE TANGANIKA.]
Public-domain text, read in full here on John Shaqi.
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