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
"These mountains are much higher than the others, and are quite
impassable, presenting a rugged outline and bold and precipitous
escarpments. From a distant view, from the nature of the outline (not
having been near them) I infer that they are granitic.
"The area of this district, from the ascertained and assumed boundaries
will be much greater than has hitherto been supposed. It cannot, I
imagine, be less than 13,500 instead of 10,000 square miles. At the
same time it must be remembered, that if I find by my future
observations, (which I think will very probably be the case) the same
amount of error, and in the same direction in the southern portion of
the district, of which at present I know nothing, as I have found in the
northern, the area will be increased by a great quantity, and may not
fall far short of 16,000 square miles, as a small deviation in the
assigned direction of the Great Draakberg will easily make that
quantity.
"The district is everywhere covered with vegetation, either in the form
of luxuriant grass, which grows to a great height, or thorns and low
bushes. Timber trees only grow in kloofs on sides of hills, excepting a
belt which runs along the sea-coast.
"Water abounds in every part, and flowing streams cross the path at
intervals of only a few miles. In the winter some of these become dry,
but then water may always be obtained at moderate distances.
"The soil is in all cases well adapted for cultivation, and on the
alluvial lands near rivers particularly so, producing much larger crops
than are ever grown in the Colony of the Cape of Good Hope.
"The rocks which occur in the district, as far as I have yet seen, are
granite, basalt, and members of the trap family, slate, sandstone, and
shale.
"Coal containing but little bituminous matter occurs in in beds in the
sandstone. In a kloof near the drift of the Bushman's River, there is a
bed nine inches thick. This is the nearest locality I am aware of to
Pietermaritzburg; it is distant about sixty-three miles. It is more
abundant to the north-west, and I observed it in a small river near
Biggar's Berg, in about latitude 28 degrees 7 minutes South, and
longitude 29 degrees 25 minutes East, in a bed six feet thick, and of
good quality; it is here cut through by a vein of trap."
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Note 1. In the Blue Book for 1847, the latest published account, the
numbers stand, 71,113 white, and 75,977 coloured; but this leaves more
than 21,000 of the total unaccounted for.
PART ONE, CHAPTER TWO.
INFORMATION FOR EMIGRANTS.
As it is my wish to put nothing but trustworthy information into the
hands of those who may be meditating so very important a step as
removing themselves and all that they value far from their native land,
I have carefully abstracted the following statements from the last
_Colonisation Circular_, issued (March, 1850) by Her Majesty's Colonial
Land and Emigration Commissioners.
Public-domain text, read in full here on John Shaqi.
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