A history of the Zulu Rebellion, 1906, and of Dinuzulu's arrest, trial, and expatriationStuart, James
History
A history of the Zulu Rebellion, 1906, and of Dinuzulu's arrest, trial, and expatriation
Stuart, James
Dinuzulu, approximately 1868-1913; Zulu Rebellion, 1906; Zululand (South Africa) -- History
Notwithstanding the sharp ascent so characteristic of Nkandhla ridges
and spurs, comparatively few stones or boulders are to be found. The
ground is covered with damp, decaying substances, such as leaves and
branches; here and there, especially along the beds of streams, are
to be seen moss-covered, slippery rocks, ferns and monkey-ropes, all
tending to give an impression of the immense antiquity and majesty of
the forest. Beautiful glades, varying in size and shape, are suddenly
come upon in parts, with all the freshness and evenness of some lowland
meadow. A look-out must be kept for snakes, such as rocky cobras,
_mambas_ and puff-adders. Leopards are also to be found. Of birds,
lories, red-necked partridges and eagles will frequently be seen. And
superstitious people will be interested to know that ghosts have, for
generations, haunted and are said still to haunt the dense, precipitous
forest Eziwojeni, immediately below Sigananda's kraal "Enhlweni."
Above and at the rear of the Mome waterfall (which has a drop of fifty
feet) is a natural stronghold, the one used by Cetshwayo in 1883.
Owing, however, to a feeling of insecurity, especially on account
of the presence of artillery, the rebels did not use it in 1906,
they preferred to take refuge in the Mome gorge and the adjoining
forest-covered valleys. A favourite, though unhealthy hiding-place, is
in the vicinity of Manzipambana (a tributary of the Nkunzana), which
never issues into open daylight. The peculiar vagaries of its course,
which, in parts, seems to proceed one way and then in exactly opposite
direction, are ascribed to perverse and occult powers emanating from
the still and sombre forest depths.
The Mome gorge, to be often referred to later, takes its name from a
stream that flows through it. It is about one and a half miles long,
with great mountain walls on either side. At the head of the valley is
the waterfall already referred to. Near the fall, the ground rises on
either side to an altitude of over 3,000 feet, but at the mouth of the
valley drops away with remarkable suddenness. Within a radius of 200 to
300 yards of the fall, the earth is covered with a dense forest which,
extending outwards on either side, connects with the various other
forests referred to above, especially on the east. A couple of isolated
forests are to be seen within the valley, particularly the Dobo or
'pear-shaped' one on the west near the mouth. So steep are the sides of
the gorge, like the letter V, that the sun in the morning and afternoon
is shut out to such an extent that the day appears to be considerably
shorter than it is.
Public-domain text, read in full here on John Shaqi.
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