Narrative of travels and discoveries in Northern and Central Africa, in the years 1822, 1823, and 1824Denham, Dixon
History
Narrative of travels and discoveries in Northern and Central Africa, in the years 1822, 1823, and 1824
Denham, Dixon
Africa, Central -- Description and travel; Africa, North -- Description and travel; Natural history -- Africa, North
The elevation gradually increases in advancing towards the equator;
and the soil, on approaching Delow, where the northernmost point
of the Mandara chain commences, is covered with a glittering
micaceous sand, principally decomposed granite, which forms a
productive earth. The hills extend in apparently interminable ridges
east-south-east, south-west, and west; while to the south several
masses or systems of hills, if I may so express myself, spread
themselves out in almost every picturesque form and direction that
can be imagined. Those nearest the eye apparently do not exceed
2500 feet in height; but the towering peaks which appear in the
distance are several thousand feet higher. They are composed of
enormous blocks of granite, both detached and reclining on each
other, presenting the most rugged faces and sides. The interstices
and fissures appeared to be filled with a yellow quartzose earth, in
which were growing mosses and lichens: trees of considerable size also
grow from between them. On almost all the hills that I approached,
clusters of huts were seen in several places towards the centre,
and sometimes quite at the summit; generally on the flats of the
ridges. At the base of these mountains, and also at a considerable
elevation on their sides, are incumbent masses of what appeared
to be the decomposed fragments of primitive rocks recompounded,
and united anew by a species of natural cement. At some distance
from the base of those which I ascended from the valley of Mora,
were collections of quartzose rocks, of great variety and colour;
fragments of hornblende, and several large abutments of porphyroidal
rocks. About one hundred yards above the spring which I have before
mentioned, in a space between two projecting masses of rock, were
numerous shells, some petrified and finely preserved, while others
were perforated by insects, worm-eaten, and destroyed: they were
confusedly mixed with fragments of granite, quartz, sand and clay;
and in some cases adhered to pieces of the composition rocks: the
greater part were of the oyster kind. Various specimens of these,
with pieces of every variety of the structure of the hills, I had
collected, but they were all lost in the general confusion of the
battle; and on the return of the army I was unable to do more than
procure a few specimens of the northernmost part of the mountains;
and the half of these were lost by my negro.
Public-domain text, read in full here on John Shaqi.
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