I have treated the subject of Axim with a minuteness that is almost 'porochial;' its future importance must be my excuse. The next chapter will show that we are truly in the Land of Gold, in an Old New California.
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.'
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.