Page:Travels in West Africa, Congo Français, Corisco and Cameroons (IA travelsinwestafr00kingrich).pdf/128

 fourth funeral, two youngsters (junior clerks of the deceased) from drink brought on by fright, fell into the grave before the coffin, which got lowered on to them, and all three had to be hauled out again. "Barely necessary though, was it?" said another member of the party, "for those two had to have a grave of their own before next sundown." And the general consensus of opinion was that one of these periodic epidemics was "just about due now." Next to the scenery of "a River," commend me for cheerfulness to the local conversation of its mangrove-swamp region; and every truly important West African river has its mangrove-swamp belt, which extends inland as far as the tide waters make it brackish, and which has a depth and extent from the banks depending on the configuration of the country. Above this belt comes uniformly a region of high forest, having towards the river frontage clay cliffs, sometimes high, as in the case of the Old Calabar at Adiabo, more frequently dwarf cliffs, as in the Forcados up at Warree, and in the Ogowé,—for a stretch through Kama country. After the clay cliffs region you come to a region of rapids, caused by the river cutting its way through a mountain range; such ranges are the Pallaballa, causing the Livingstone rapids of the Congo; the Sierra del Cristal, those of the Ogowé, and many lesser rivers; the Rumby and Omon ranges, those of the Old Calabar and Cross Rivers.

Naturally in different parts these separate regions vary in size. The mangrove-swamp may be only a fringe at the mouth of the river, or it may cover hundreds of square miles. The clay cliffs may extend for only a mile or so along the bank, or they may, as on the Ogowé, extend for 130. And so it is also with the rapids: in some rivers, for instance the Cameroons, there are only a few miles of them, in others there are many miles; in the Ogowé there are as many as 500; and these rapids may be close to the river mouth, as in most of the Gold Coast rivers, save the Ancobra and the Volta; or they may be far in the interior, as in the Cross River, where they commence at about 200 miles; and on the Ogowé, where they commence at about 208 miles from the sea coast; this depends on the nearness or remoteness from the