PLATE II.

[Illustration: _Fig. 12._--KIMBERLEY MINE, 1874.]

[Illustration: _Fig. 13._--KIMBERLEY MINE, 1902. (From Photographs by

C. Evans.)]

In a very few years, however, the open pit mining was rendered

impossible by the mud rushes, by the falls of the masses of barren

rock known as "reef," which were left standing in the mine, and by

landslips from the sides, so that in 1883, when the pit had reached a

depth of about 400 ft., mining in the Kimberley crater had become

almost impossible. By 1889, in the whole group of mines, Kimberley,

Dutoitspan, De Beers and Bultfontein, open pit working was practically

abandoned. Meanwhile mining below the bottom of the pits by means of

shafts and underground tunnels had been commenced; but the full

development of modern methods dates from the year 1889 when Cecil

Rhodes and Alfred Beit, who had already secured control of the De

Beers mine, acquired also the control of the Kimberley mine, and

shortly afterwards consolidated the entire group in the hands of the

De Beers Company. (See KIMBERLEY.)

The scene of native mining was now transferred from the open pit to

underground tunnels; the vast network of wire ropes (Plate II. fig.

12) with their ascending and descending buckets disappeared, and with

it the cosmopolitan crowd of busy miners working like ants at the

bottom of the pit. In place of all this, the visitor to Kimberley

encounters at the edge of the town only a huge crater, silent and

apparently deserted, with no visible sign of the great mining

operations which are conducted nearly half a mile below the surface.

The aspect of the Kimberley pit in 1906 is shown in fig. 13 of Plate

II., which may be compared with the section of fig. 8.

In fig. 13, Plate II., the sequence of the basalt, shale and melaphyre

is clearly visible on the sides of the pit; and fig. 8 shows how the

crater or "pipe" of blue ground has penetrated these rocks and also

the underlying quartzite. The workings at De Beers had extended into

the still more deeply seated granite in 1906. Figure 9, Plate I.,

shows the top of the De Beers' crater with basalt overlying the shale.

Figure 8 also explains the modern system of mining introduced by

Gardner Williams. A vertical shaft is sunk in the vicinity of the

mine, and from this horizontal tunnels are driven into the pipe at

different levels separated by intervals of 40 ft. Through the blue

ground itself on each level a series of parallel tunnels about 120 ft.

apart are driven to the opposite side of the pipe, and at right angles

to these, and 36 ft. apart, another series of tunnels. When the

tunnels reach the side of the mine they are opened upwards and

sideways so as to form a large chamber, and the overlying mass of blue

ground and debris is allowed to settle down and fill up the gallery.

On each level this process is carried somewhat farther back than on

the level below (fig. 8); material is thus continually withdrawn from

one side of the mine and extracted by means of the rock shaft on the

opposite side, while the superincumbent debris is continually sinking,

and is allowed to fall deeper on the side farthest from the shaft as

the blue ground is withdrawn from beneath it. In 1905 the main shaft

had been sunk to a depth of 2600 ft. at the Kimberley mine.

For the extraction and treatment of the blue ground the De Beers

Company in its great winding and washing plant employs labour-saving

machinery on a gigantic scale. The ground is transferred in trucks to

the shaft where it is automatically tipped into skips holding 96 cubic

ft. (six truck loads); these are rapidly hoisted to the surface, where

their contents are automatically dumped into side-tipping trucks, and

these in turn are drawn away in a continual procession by an endless

wire rope along the tram lines leading to the vast "distributing

floors." These are open tracts upon which the blue ground is spread

out and left exposed to sun and rain until it crumbles and

disintegrates, the process being hastened by harrowing with steam

ploughs; this may require a period of three or six months, or even a

year. The stock of blue ground on the floors at one time in 1905 was

nearly 4,500,000 loads. The disintegrated ground is then brought back

in the trucks and fed through perforated cylinders into the washing

pans; the hard blue which has resisted disintegration on the floors,

and the lumps which are too big to pass the cylindrical sieves, are

crushed before going to the pans. These are shallow cylindrical

troughs containing muddy water in which the diamonds and other heavy

minerals (concentrates) are swept to the rim by revolving toothed

arms, while the lighter stuff escapes near the centre of the pan. The

concentrates are then passed over sloping tables (pulsator) and shaken

to and fro under a stream of water which effects a second

concentration of the heaviest material.

Until recently the final separation of the diamond from the

concentrates was made by hand picking, but even this has now been

replaced by machinery, owing to the remarkable discovery that a

greased surface will hold a diamond while allowing the other heavy

minerals to pass over it. The concentrates are washed down a sloping

table of corrugated iron which is smeared with grease, and it is found

that practically all the diamonds adhere to the table, and the other

minerals are washed away. At the large and important Premier mine in

the Transvaal the Elmore process, used in British Columbia and in

Wales for the separation of metallic ores, has been also introduced.

In the Elmore process oil is employed to float off the materials which

adhere to it, while the other materials remain in the water, the oil

being separated from the water by centrifugal action. The other

minerals found in the concentrates are pebbles and fragments of

pyrope, zircon, cyanite, chrome-diopside, enstatite, a green pyroxene,

mica, ilmenite, magnetite, chromite, hornblende, olivine, barytes,

calcite and pyrites.

In all the S. African mines the diamonds are not only crystals of

various weights from fractions of a carat to 150 carats, but also

occur as microscopic crystals disseminated through the blue ground. In

spite of this, however, the average yield in the profitable mines is

only from 0.2 carat to 0.6 carat per load of 1600 lb., or on an

average about 1-1/2 grs. per ton. The annual output of diamonds from

the De Beers mines was valued in 1906 at nearly L5,000,000; the value

per carat ranging from about 35s. to 70s.

[Illustration: SECTION OF KIMBERLEY MINE LOOKING EAST

Encyclopaedia Britannica, 11th Edition, "Diameter" to "Dinarchus" Volume 8, Slice 4 · 第 7 / 86 题