The Cape and the Kaffirs: A Diary of Five Years' Residence in Kaffirland — John Shaqi
The Cape and the Kaffirs: A Diary of Five Years' Residence in KaffirlandWard, Mrs.
History
The Cape and the Kaffirs: A Diary of Five Years' Residence in Kaffirland
Ward, Mrs.
South Africa -- History -- Frontier Wars, 1811-1878
"The Umzinyati rises at the base of the Draakberg, in latitude 27
degrees 46 minutes and longitude 20 degrees 25 minutes; from this its
course is about E.S.E., until it falls into the Utukela (incorrectly
called the Tukela.) From all the information I can obtain, (not having
yet visited this part of the district) this is below the confluence of
the Mooi River and the Utukela, and therefore not very far from the
mouth of the latter, which from the maps appears to be in latitude 29
degrees 16 minutes South and longitude 31 degrees 30 minutes East; thus
forming the north-eastern boundary of the district.
"The country below the rise of the Umzinyati, and for the distance of
about twenty miles, is for the most part flat and undulating, with
little or no wood, but covered with sweet grass, and from what I can
ascertain is considered a good tract for country sheep.
"The river, when I saw it (in February, 1847), was about sixty yards
wide, it being then full of water; below this, and during its whole
course, I understand it runs through a broken and thick bushy country.
"The Draakberg, instead of being considered as one continuous chain of
mountains, may be more correctly divided into two, of different
geological structure, and having different directions: the one forming
the north-western boundary I shall call the Great Draakberg; and the
other, forming the western boundary, the Small Draakberg.
"The north-western portion of the Draakberg is of the average altitude
of five thousand feet above the sea, and about fifteen hundred feet
above the general level of the country at its base.
"The outline is in general round and soft, presenting some remarkable
features, and occasionally high table-lands with precipitous sides.
These mountains are composed of beds of sandstone, cut through by veins
of trap, and diminish in height as they advance to the north-east, until
at some distance beyond the source of the Umzinyati they appear to
terminate in low hills. They are passable almost at any part by horses
and cattle; but there are only three passes in use by the Boers, one
near Bezuidenhout's Farm, in latitude 28 degrees 33 minutes South and
longitude 28 degrees 44 minutes East; and one at De Beer's, in latitude
28 degrees 20 minutes South and longitude 28 degrees 52 minutes East,
and another a little more to the south-west of Bezuidenhout's. The two
former are in constant use; the latter rarely.
"Timber abounds in the kloofs on the south-eastern side of the mountain.
On the north-west the country is much higher, being a plain of great
elevation.
"The Great Draakberg, or that portion of it which forms the western
boundary, has a direction N.N.W. and S.S.E. The junction of this with
the former, or Small Draakberg, is ten or twelve miles to the S.W. of
Bezuidenhout's Pass:--from this part the Utukela rises.
Public-domain text, read in full here on John Shaqi.
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