Stanley's Adventures in the Wilds of Africa: A Graphic Account of the Several Expeditions of Henry M. Stanley into the Heart of the Dark ContinentHeadley, Joel Tyler
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Stanley's Adventures in the Wilds of Africa: A Graphic Account of the Several Expeditions of Henry M. Stanley into the Heart of the Dark Continent
Headley, Joel Tyler
Africa, Central -- Description and travel; Stanley, Henry M. (Henry Morton), 1841-1904
At first sight, it seems strange that Stanley should have selected this
lake as the next scene of his explorations. He had previously, with
Livingstone, explored thoroughly the upper half of it, and passed part
way down the western side; Livingstone had been at the foot of it, and
to crown all, Stanley had heard, before leaving Zanzibar, that Cameron
had explored the entire southern portion, so that really there was
nothing for him to do but follow a path which had been already trodden.
To employ an expedition fitted out at so great a cost, and spend so much
valuable time in going over old ground, seems an utter waste of both
time and labor, especially when such vast unexplored fields spread all
around him. But there was a mystery about Tanganika, which Stanley
probably suspected Cameron had not solved, and which he meant to clear
up. Here was a lake over three hundred miles long, with perhaps a
hundred streams, great and small, running into it, and yet with no
outlet, unless Cameron had found it, which he thinks he did. To find
this was the chief object of the expedition Stanley and Livingstone made
together to the north end of the lake. They had heard that the Rusizi
River at that extremity was the outlet, but they found it instead a
tributary. In fact, they proved conclusively that there was no outlet at
the northern end. It therefore must be at the southern, and if so, it
was the commencement of a river that would become a mighty stream
before it reached the ocean. But no such stream was known to exist. The
Caspian Sea has large rivers flowing into it, but no outlet, yet it
never fills up. Evaporation, it is supposed, accounts for this. But the
Caspian is salt, while the Tanganika is fresh water, and such a large
body of fresh water as this was never known to exist without an outlet,
and if it could be that evaporation was so great as to equal all the
water that runs into it, it would not remain so fresh as it is.
Public-domain text, read in full here on John Shaqi.
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