West African studies. Mary Henrietta Kingsley
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Jengu Devil Dance of King William’s Slaves, Sette Camma, Nov. 9, 1888.
The sides of this submarine valley seem almost vertical cliffs, and herein lies its danger for the sailing ship. The master thereof, in the smoke or fog season (December-February), may not exactly know to a mile or so where he is, and being unable to make out Piccaninny Bassam, which is only a small native village on the sand ridge between the surf and the lagoon, he lets go his anchor on the edge of the cliffs of this Bottomless pit. Then the set of the tide and the onshore breeze cause it to drag a little, and over it goes down into the abyss, and ashore he is bound to go. In old days he and his ship’s crew formed a welcome change in the limited dietary of the exultant native. Mr. Barbot, who knew them well, feelingly remarks, “it is from the bloody tempers of these brutes that the Portuguese gave them the name of Malagens for they eat human flesh,” and he cites how “recently they have massacred a great number of Portuguese, Dutch and English, who came for provisions and water, not thinking of any treachery, and not many years since, (that is to say, in 1677) an English ship lost three of its men; a Hollander fourteen; and, in 1678, a Portuguese, nine, of whom nothing was ever heard since.”
From Cape Palmas until you are past the mouth of the Taka River (St. Andrew) the coast is low. Then comes the Cape of the Little Strand (Caboda Prazuba), now called, I think, Price’s Point. To the east of this you will see ranges of dwarf red cliffs rising above the beach and gradually increasing in height until they attain their greatest in the face of Mount Bedford, where the cliff is 280 feet high. The Portuguese called these Barreira Vermelhas; the French, Kalazis Rouges; and the Dutch, Roode Kliftin, all meaning Red Cliffs. The sand at their feet is strewn with boulders, and the whole country round here looks fascinating and interesting. I regret never having had an opportunity of seeing whether those cliffs had fossils on them, for they seem to me so like those beloved red cliffs of mine in Kacongo which have. The investigation, however, of such makes of Africa is messy. Those Kacongo cliffs were of a sort of red clay that took on a greasy slipperiness when they were wet, which they frequently were on account of the little springs of water that came through their faces. When pottering about them, after having had my suspicions lulled by twenty or thirty yards of crumbly dryness, I would ever and anon come across a water spring, and down I used to go—and lose nothing by it, going home in the evening time in what the local natives would have regarded as deep mourning for a large family—red clay being their sign thereof. The fossils I found in them were horizontally deposed layers of clam shells with regular intervals, or bands, of red clay, four or five feet across; between the layers some of the shell layers were 40 or more feet above the present beach level. Identical deposits of shell I also found far inland in Ka Congo, but that has nothing to do with the Ivory Coast.
Inland, near Drewin, on the Ivory Coast, you can see from the sea curious shaped low hills; the definite range of these near Drewin is called the Highland of Drewin; after this place they occur frequently close to the shore, usually isolated but now and again two or three together, like those called by sailors the Sisters. I am much interested in these peculiar-shaped hills that you see on the Ivory and Gold Coast, and again, far away down South, rising out of the Ouronuogou swamp, and have endeavoured to find out if any theories have been suggested as to their formation, but in vain. They look like great bubbles, and run from 300 to 2,000 feet.
The red cliffs end at Mount Bedford and the estuary of the Fresco River, and after passing this the coast is low until you reach what is now called the district of Lahu, a native sounding name, but really a corruption from its old French name La-Hoe or Hou.
You would not think, when looking at this bit of coast from the sea, that the strip of substantial brown sand beach is but a sort of viaduct, behind which lies a chain of stagnant lagoons. In the wet season, these stretches of dead water cut off the sand beach from the forest for as much as 40 miles and more.
Beyond Mount La-Hou on this sand strip there are many native villages—each village a crowded clump of huts, surrounded by a grove of coco palm trees, each tree belonging definitely to some native family or individual, and having its owner’s particular mark on it, and each grove of palm trees slanting uniformly at a stiff angle, which gives you no cause to ask which is the prevailing wind here, for they tell you bright and clear, as they lean N.E., that the S.W. wind brought them up to do so.
Groves of coco palms are no favourites of mine. I don’t like them. The trees are nice enough to look on, and nice enough to use in the divers ways you can use a coco-nut palm; but the noise of the breeze in their crowns keeps up a perpetual rattle with their hard leaves that sounds like heavy rain day and night, so that you feel you ought to live under an umbrella, and your mind gets worried about it when you are not looking after it with your common sense.
Then the natives are such a nuisance with coco-nuts. For a truly terrific kniff give me even in West Africa a sand beach with coco-nut palms and natives. You never get coco-nut palms without natives, because they won’t grow out of sight of human habitation. I am told also that one coco will not grow alone; it must have another coco as well as human neighbours, so these things, of course, end in a grove. It’s like keeping cats with no one to drown the kittens.
Well, the way the smell comes about in this affair is thus. The natives bury the coco-nuts in the sand, so as to get the fibre off them. They have buried nuts in that sand for ages before you arrive, and the nuts have rotted, and crabs have come to see what was going on, a thing crabs will do, and they have settled down here and died in their generations, and rotted too. The sandflies and all manner of creeping things have found that sort of district suits them, and have joined in, and the natives, who are great hands at fishing, have flung all the fish offal there, and there is usually a lagoon behind this sort of thing which contributes its particular aroma, and so between them the smell is a good one, even for West Africa.
The ancient geographers called this coast Ajanginal Æthiope, and the Dutch and French used to reckon it from Growe, where the Melaguetta Coast ends. Just east of Cape Palmas, to the Rio do Sweiro da Costa, where they counted the Gold Coast to begin, the Portuguese divided the coast thus. The Ivory, or, as the Dutchmen called it, the Tand Kust, from Gowe to Rio St. Andrew; the Malaguetta from St. Andrew to the Rio Lagos;[5] and the Quaqua from the Rio Lagos to Rio de Sweiro da Costa, which is just to the east of what is now called Assini.
It is undoubtedly one of the most interesting and nowadays least known bits of the coast of the Bight of Benin; but, taken altogether, with my small knowledge of it, I do not feel justified in recommending the Ivory Coast as either a sphere for emigration or a pleasure resort. Nevertheless, it is a very rich district naturally, and one of the most amusing features of West African trade you can see on a steamboat is to watch the shipping of timber therefrom.
This region of the Bight of Benin is one of enormous timber wealth, and the development of this of late years has been great, adding the name of Timber Ports to the many other names this particular bit of West Africa bears, the Timber Ports being the main ports of the French Ivory Coast, and the English port of Axim on the Gold Coast.
The best way to watch the working of this industry is to stay on board the steamer; if by chance you go on shore when this shipping of mahogany is going on you may be expected to help, or get out of the way, which is hot work, or difficult. The last time I was in Africa we on the——shipped 170 enormous bulks of timber. These logs run on an average 20 to 30 feet long and 3 to 4 feet in diameter. They are towed from the beach to the vessel behind the surf boats, seven and eight at a time, tied