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West African studies. Mary Henrietta Kingsley
Читать онлайн.Название West African studies
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isbn 4064066119256
Автор произведения Mary Henrietta Kingsley
Жанр Книги о Путешествиях
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The aforesaid are everyday noises in West Africa, and you soon get used to them or die of them; but there are myriads of others that you hear when in the bush. The grunting sigh of relief of the hippos, the strange groaning, whining bark of the crocodiles, the thin cry of the bats, the cough of the leopards, and that unearthly yell that sometimes comes out of the forest in the depths of dark nights. Yes, my naturalist friends, it’s all very well to say it is only a love-lorn, innocent little marmoset-kind of thing that makes it. I know, poor dear, Softly, Softly, and he wouldn’t do it. Anyhow, you just wait until you hear it in a shaky little native hut, or when you are spending the night, having been fool enough to lose yourself, with your back against a tree quite alone and that yell comes at you with its agony of anguish and appeal out of that dense black world of forest which the moon, be she never so strong, cannot enlighten, and which looks all the darker for the contrast of the glistening silver mist that shows here and there in the clearings, or over lagoon, or river, wavering twining, rising and falling; so full of strange motion and beauty, yet, somehow, as sinister in its way as the rest of your surroundings, and so deadly silent. I think if you hear that yell cutting through this sort of thing like a knife and sinking despairingly into the surrounding silence, you will agree with me that it seems to favour Duppy, and that, perchance, the strange red patch of ground you passed at the foot of the cotton tree before night came down on you, was where the yell came from, for it is red and damp and your native friends have told you it is so because of the blood whipped off a sasa-bonsum and his victims as he goes down through it to his under-world home.
Seen from the sea, the Ivory Coast is a relief to the eye after the dead level of the Grain Coast, but the attention of the mariner to rocks has no practical surcease; and there is that submarine horror for sailing ships, the Bottomless pit. They used to have great tragedies with it in olden times, and you can still, if you like, for that matter; but the French having a station 15 miles to the east of it at Grand Bassam would nowadays prevent your experiencing the action of this phenomenon thoroughly, and getting not only wrecked but killed by the natives ashore, though they are a lively lot still.
Now although this is not a manual of devotion, I must say a few words on the Bottomless pit. All along the West Coast of Africa there is a great shelving bank, submarine, formed by the deposit of the great mud-laden rivers and the earth-wash of the heavy rains. The slope of what the scientific term the great West African bank is, on the whole, very regular, except opposite Piccaninny Bassam, where it is cut right through by a great chasm, presumably the result of volcanic action. This chasm commences about 15 miles from land and is shaped like a V, with the narrow end shorewards. Nine miles out it is three miles wider and 2,400 feet deep, at three miles out the sides are opposite each other and there is little more than a mile between them, and the depth is 1,536 feet; at one mile from the beach the chasm is only a quarter of a mile wide and the depth 600 feet—close up beside the beach the depth is 120 feet. The floor of this chasm is covered with grey mud, and some five miles out the surveying vessels got fragments of coral rock.
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[To face page 69.
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