A biographical memoir of the late Dr. Walter Oudney, Captain Hugh Clapperton, both of the Royal Navy, and Major Alex. Gordon Laing, all of whom died amid their active and enterprising endeavours to explore the interior of AfricaNelson, Thomas
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A biographical memoir of the late Dr. Walter Oudney, Captain Hugh Clapperton, both of the Royal Navy, and Major Alex. Gordon Laing, all of whom died amid their active and enterprising endeavours to explore the interior of Africa
Nelson, Thomas
Africa -- Description and travel; Clapperton, Hugh, 1788-1827; Laing, Alexander Gordon, 1794-1826; Oudney, Walter, 1790-1824
I have anxiously searched for springs, but have found none fit for
an accurate result. The whole country is a spring, if I may use the
expression, for water comes bubbling up on digging a few feet; its
temperature then is affected by the earth, and the heat indicated
is of no use in ascertaining the mean temperature of the place, and
consequently its elevation. The abundance of water in a country in
which rain scarcely ever falls, and in which there is no dew, is a
curious and interesting circumstance to the philosophic inquirer. It
is not generated in the earth, and it cannot be supplied by the sea.
From whence then does it come? Is it from the tropical rains? Or is it
from rivers lost in the earth? The supply is constant, and the wells
yield as much at one time as another. The supposition that appears most
probable to me is, that the countries to the southward are much higher
than this, that during the rainy season water penetrates a considerable
way into the earth, till it meets with _strata_ resisting its farther
descent, and then that it flows along these like a river to far distant
countries. My explanation may be censured, but still on reflection, I
regard it as the most probable that I can think of. There is another
interesting feature in Fezzan, namely, the constant formation of salt
on the surface of the sand. In travelling along, the different stages
of the process are very distinctly observable. First, a thin crust is
formed like hoar frost, and this continues to increase in thickness. In
some places the layer of salt is a foot deep. At present I must defer
the explanation of this phenomenon till I shall have time to enter
upon the description of the geological structure of Fezzan—a thing I
hope I shall soon be enabled to do. In the mean time the courier is
waiting, and the camels are ready to convey us to Ghaat. My worthy
friend Clapperton and I are just on the point of setting out on a visit
to that country, that we may render our delay here as serviceable as
possible. The Tuarick country is, perhaps, interesting only on account
of its inhabitants, who are a brave, independent race. Clapperton and I
have been at Tucta, and we were both struck with the general uniformity
of the scenery and the structure. He desires to be kindly remembered to
you, and intends to write you soon. We expect to be able to set out for
Bornou in two or three months.”
Public-domain text, read in full here on John Shaqi.
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