And now to conclude this unpleasant account with the good words of old Barbot: 'Axim, in my opinion, is the most tempting of any on the coast of Guinea, taking one thing with another. You have there a perpetual greenness, which affords a comfortable shade against the scorching heat of the sun, under the lofty palm and other trees, planted about the village, with a sweet harmony of many birds of several sorts perching on them. The walk on the low flat strand along the seaside is no less pleasant at certain hours of the day; and from the platform of the fort is a most delightful prospect of the ocean and the many rocks and small islands about it.'
CHAPTER XVI. — GOLD ABOUT AXIM, ESPECIALLY AT THE APATIM OR BUJIÁ CONCESSION.
Any one who has eyes to see can assure himself that Axim is the threshold of the Gold-region. It abounds in diorite, a rock usually associated with the best paying lodes. After heavy showers the naked eye can note spangles of the precious metal in the street-roads. You can pan it out of the wall-swish. The little stream-beds, bone-dry throughout the hot season, roll down, during the rains, a quantity of dark arenaceous matter, like that of Taranaki, New Zealand, and the 'black sand' of Australia, which collects near the sea in stripes and patches. The people believe that without it gold never occurs; and, if they collect the common yellow sand, it is to extract from it the darker material. If the stuff does not answer the magnet, it is probably schorl (tourmaline), hornblende, or dark quartz. Strangers have often mistaken this emery-like rock for tin, which occurs abundantly in the northern region. It is simply titaniferous iron, iserine, pleonaste, ilmenite [Footnote: Or peroxide of iron, with 8 to 23 per cent, of blue oxide of titanium.] and degraded itabirite, the iron and quartz formation so called in the Brazil; and it is the same mineral which I found so general throughout the gold and silver fields of neglected Midian. It is found striating white sandstone about Tákwá and other places in the interior. The surface-stone is decomposed by the oxide of iron, and thus the precious dust with its ingrained gold is dissolved and separated from it. At a greater depth the itabirite will be found solid; and the occurrence of these oldest crystalline formations in large layers is a hopeful sign. When Colonel Bolton was interested in the Gold Coast diggings I advised him to send for a few tons of this metal, and to test it as 'pay-dirt.' A barrelful was forwarded from the coast to the Akankon Company: it was probably thrown away without experiment.
At Axim, as at Cape Coast Castle and other parts of the shore, women may be seen gold-gathering even on the sea-sands. They rarely wash more than 40 lbs., or a maximum of 50 lbs., per diem; and they strike work if they do not make daily half a dollar (2s. 3d.) to two dollars. They have nests of wooden platters for pans, the oldest and rudest of all mechanical appliances. The largest, two feet in diameter, are used for rough work in the usual way with a peculiar turn of the wrist. The smallest are stained black inside, to show the colour of gold; and the finer washings are carried home to be worked at leisure during the night. This is peculiarly women's work, and some are well known to be better panners than others; they refuse to use salt-water, because, they say, it will not draw out the gold.
The whole land is impregnated with the precious metal. I find it richer in sedimentary gold than California was in 1859. Immediately behind the main square of Axim a bank of red clay leads eastward to a shallow depression, the old valley of the Besáon, a swamp during the rains backed by rising and forested ground to the east. On the inland versant a narrow native shaft has been sunk for gold by Mr. Sam, now native agent under Mr. Crocker. We pounded and panned the rock, which yielded about twopence per 2 lbs., or one ounce to the ton. Observing its strike, we concluded that it must extend through Mr. Irvine's property. Throughout the Gold Coast auriferous reefs ran north-south, with easting rather than westing; the deviation varies from 5º west to 15º-22º east; and I have heard of, but not seen, a strike of north-east (45º) to south-west. This confirms the 'meridional hypothesis' of Professor Sedgwick, who stated, 'As some of the great physical agencies of the earth are meridional, these agencies may probably, in a way we do not comprehend, have influenced the deposit of metals on certain lines of bearing.' We may also observe that all the great mineral chains of the old and new world are meridional rather than longitudinal, striking from north-east to south-west. The geologist's theory, combined with the knowledge that the noble metal is 'chiefly found among palæozoic rocks of a quartzose type,' is practically valuable on the Gold Coast. Every mound or hillock of red clay contains one or more quartz-reefs, generally outcropping, but sometimes buried in the subsoils. They can always be struck by a cross-cut trending east-west. The dip is exceedingly irregular: some lodes are almost vertical, and others quasi-horizontal.
We now take the main road leading to the Ancobra. After crossing the fetid Besáon by its ricketty bridge of planks, we find on the right hand, facing Messieurs Swanzy's, a fine bit of rising ground, which I shall call, after its proprietor, 'Mount Irvine.' Over the southern slope runs a cleared highway, which presently becomes a 'bush-path;' it is named the 'Dudley Road,' after an energetic District-commissioner. This is the first Tákwá line, whose length is described to be about fifty miles, or four days' slow journey for laden porters. Mr. Gillett, who had covered twenty-six (sixteen?) miles of it, describes the path as unbroken by swamps or streams. Further north, according to the many native guides whom I questioned, travellers pass two rivulets, and finally they are ferried over the Abonsá, or Tákwá River. The second road follows closely the left bank of the Ancobra: it is used by the Hausá soldiers, but only in the heart of the Dries, and it must be impassable during the Rains. Dr. J. Africanus B. Horton, who contributes to a characteristic paper, [Footnote: The African Times, January 2, 1882. The paper is full of inaccuracies; it begins by placing Tomento (Tumento) ninety-five miles (for thirty) along the river-course from the mouth, and he makes steam-launches 'take from two to four days (say one) to go up to it.'] has never heard of the former when he says 'from Axim to Taquah (Tákwá) there is no direct route,' and he justly deprecates the latter. But he cries up the Bushua or Dixcove-Tákwá line, upon which he has large concessions. I shall return to this subject in a future chapter.
On the north side of Mount Irvine is a second nullah, the Eswá, which flows, like the Besáon, through the dense growth of bush covering the eastern uplands. A few minutes' walk along the right bank leads to a broadening of the bed, a swamp during the Rains and a field of cereals in the Dries. Thence we plunge into the jungle, and after a couple of hundred yards come upon signs of mining. In the Eswá bed, where the gulch is choked by two mounds or hillocks, appear the usual 'women's washings,' shallow pits like the Brazilian catas, whence the pay-dirt has been extracted. On the right bank, subtending the bed, their husbands have sunk the usual chimney-hole to scratch quartz from the bounding-wall of the reef. These rude beginnings of shafts reach a depth of 82 feet, and perhaps more. All are round, like the circular hut of the African savage; similarly in Australia the first pits were circular or oval. They are descended in sweep-fashion by means of foot-holes, and they are just large enough for a man to sit in and use his diminutive tool. The quartz is sent up to grass by a basket, and carried to the hut. After a preliminary roasting, the old custom of Egypt, it is broken into little bits and made over to the women, who grind it down upon the cankey-stone which serves to make the daily bread. In some parts of Africa this is men's work, and it is always done at night, with much jollity and carousing.
I named this place the 'Axim Reef.' It had been taken by Dr. J. Ogilby Ross, formerly district medical officer, Axim, and now preparing to explore the regions behind the Ancobra sources. He allowed, however, his prospecting term to elapse, and thus it has been secured by Mr. Grant for Mr. J. Irvine. It taught us three valuable lessons.