“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.
“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.”
Chapter II.
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.
“The Government Emigration Officers in the United Kingdom, are:—London: Lieut. Lean, R.N., Office, 70, Lower Thames-Street. Liverpool: Lieut. Hodder, R.N., Stanley Buildings. Plymouth: Lieut. Carew, R.N. Glasgow and Greenock: Capt. Patey, R.N. Dublin: Lieut. Henry, R.N. Cork: Lieut. Friend, R.N. Belfast: Lieut. Stark, R.N. Limerick: Mr Lynch, R.N. Sligo, Donegal, Ballina etc: Lieut. Shuttleworth, R.N.; Lieut. Moriarty, R.N. Londonderry: Lieut. Ramsay, R.N. Waterford and New Res. Comm. Ellis, R.N.
“These officers act under the immediate directions of the Colonial Land and Emigration Commissioners, and the following is a summary of their duties:
“They procure and give gratuitously information as to the sailing of ships, and means of accommodation for emigrants, and whenever applied to for that purpose, they see that any agreements between shipowners, agents or masters, and intending emigrants are duly performed. They also see that the provisions of the Passengers’ Act are strictly complied with, viz., that passenger-vessels are sea-worthy, that they have on board a sufficient supply of provisions, water, medicines, etc, and that they sail with proper punctuality.
“They attend personally at their offices on every week-day and afford gratuitously all the assistance in their power to protect intending emigrants against fraud and imposition, and to obtain redress where oppression or injury has been practised on them.
“The Government Immigration Agents at the Cape of Good Hope, are—Cape Town: R. Southey, Esq. Port Elizabeth: D.P. Francis, Esq.
“The duties of these officers are to afford gratuitously to emigrants every assistance in their power by way of advice and information as to the districts where employment can be obtained most readily, and upon the most advantageous terms, and also as to the best modes of reaching such districts.
“The rate of passage in private ships to the Cape of Good Hope and Natal is:
“At the Cape of Good Hope, persons of the following classes, if of good character and ability in their callings, are stated to be in demand; viz. agricultural labourers, shepherds, female domestic and farm servants, and a few country mechanics, such as blacksmiths, wheelwrights, carpenters, and masons.”
Of the rates of wages the Commissioners give the following Tables from the latest official returns in their possession:
As very many persons who would be most useful in the Colonies have no means of their own for proceeding thither, various provisions have been made to assist them. Thus the Emigration Commissioners “grant passages to those Colonies (only) which provide the necessary funds for the purpose. These funds, which in the Australian Colonies are derived from sales or rents of crown lands, are intended not