For a wonder the canoes came in time, and, despite their mat- sails, we could not complain of them. There were twelve paddlers two for the stem, and two for the stern of each craft, under a couple of interpreters, Jotakwassi and Nchama-Chamvu, who were habited in European frock-coats of broadcloth, and in native terminations mostly "buff." Our excellent host bade us a kindly adieu, with many auguries of success—during the last night the frogs had made a noise in the house. Briefly, we set out on September 6th.

In the forty-five miles between Boma, where we enter the true trough of the Congo, and the landing-place of Banza Nokki below the cataracts, there are half-a-dozen reaches, the shortest of three, the longest of fifteen miles. They are not straight, as upon the chart; the windings of the bed exclude direct vision, and the succession of points and bays suggest, like parts of the Rhine, a series of mountain-tarns. The banks show the high-water level in a low shelf, a ribbon of green, backed by high rolling hills, rounded and stony, with grass dry at this season; the formation is primitive, and the material of the lower bed has been held to "prove the probability that the mountains of Pernambuco, Rio de Janeiro, and other adjacent parts of South America, were primevally connected with the opposite chains, that traverse the plains of Congo and Loango." In parts the rocks fall bluff into the river, and here the current rushes past like a mill-race without a shadow of backwater. The heights are intersected by gullies and ravines, of which I counted sixty-nine on the right and fifty-four on the left bank; many of them are well wooded, and others are fronted by plains of the reeds and flags, which manufacture floating islands, cast loose, like those of the Niger, about the end of July by the "Malka" rains. About a dozen contained running water: Captain Tuckey did not see one that would turn a mill in August and September; but in November and December all these fiumaras will discharge torrents.

The breadth of the entroughed bed varies from 700 yards to two miles where it most dispreads itself. The current increases from the normal three to five knots in rare places; the surface loses the glassiness of the lower section, and at once shows the boiling and swirling which will be noticed near the cataracts. The shores are often foul, but the midway is mostly clear, and, where sunken rocks are, they are shown by whirlpools. The flow of the tide, or rather the damming up of the lower waters between Porto da Lenha and the mouth, causes a daily rise, which we found to measure about a foot; thus it assists in forming a treble current, the rapid down-flow in the Thalweg being subtended by a strong backwater on either side carrying a considerable portion in a retrograde direction, and showing a sensible reflux; this will continue as far as the rapids. In the Amazonas the tides are felt a hundred leagues from the mouth; and, whilst the stream moves seawards, the level of the water rises, proving an evident under-current. Mr. Bates has detected the influence of oceanic tides at a point on the Tapajos, 530 miles distant from its mouth, such is the amazing flatness of the country's profile: here we find the reverse.

The riverine trough acts as wind-conductor to a strong and even violent sea-breeze; on the lower section it begins as a ground- current—if the "bull" be allowed—a thin horizontal stratum near the water, it gradually curves and slides upwards as it meets the mountain flanks, forming an inverted arch, and extending some 2,000 to 3,000 feet above the summits. At this season it is a late riser, often appearing about 3 P.M., and sometimes its strength is not exhausted before midnight. The brown water, grass-sheeted at the sides, conceals the bright yellow sand of the bed; when placed in a tumbler it looks clear and colourless, and the taste is perfectly sweet—brackishness does not extend far above Porto da Lenha. Yet at Boma the residents prefer a spring near the factories, and attribute dysentery to the use of river-water. According to Mr. George Maxwell, the supply of the lower bed has the quality of rotting cables, and the same peculiarity was attributed to the Tanganyika.

Of late years no ship has ventured above Boma, and boats have ascended with some difficulty, owing to the "buffing stream." Yet there is no reason why the waters should not be navigated, as proposed in 1816, by small steamers of good power, and the strong sea-breeze would greatly facilitate the passage. In older and more enterprising days merchant-schooners were run high up the Zaire. The master of a vessel stated to Tuckey that he "had been several voyages up to the distance of 140 miles from the mouth" without finding any difficulty.

Our course passed by Banza Chisalla where, as we had paid double, there was a vain attempt to make us pay treble. Travelling up the south-eastern reach, we passed a triangular insulated rock off the southern bank, and then the "diabolitos" outlying Point Kilu, opposite Banza Vinda on the other side. A second reach winding to the north-east showed on the right Makula (Annan) River, and a little further Munga-Mungwa (Woodhouslee); between them is the terminus of the São Salvador road. On the northern bank where the hills now become rounded mountains, 1,500 feet above the stream, perches Chinimi the village of Manbuku Prata, who expects canoes here to await his orders; and who was sorely offended because I passed down without landing. The next feature of the chart, Matádi "Memcandi," is a rocky point, not an island. Turning a projection, Point Makula (Clough Corner), we entered No. 3, elbow bending southeast; on its concave northern side appeared the settlement Vinda la Nzádi. This is the Vinda le Zally of Tuckey; on the chart Veinde len Zally, and according to others Vinda de Nzadi, or village of the Zaire River. It is probably the "Benda" of the Introduction (p. xxxiv.); and as b and v sound alike in Fiote, Cabinda, Cabenda or Kabendah is evidently Ca-vinda—great village.

Our terminus that day was the usual resting-place of travellers, "Mfumba" behind Nkumungu (Point) Kaziwa, a mass of granitoid slabs, with a single tree for landmark. Opposite us was Sandi ya Nzondo, which others call Sanga ya Ngondo; in the chart this one- tree island is written "Catlo Zonda," it is the first of two similar formations. Oscar Rock, its western (down stream) neighbour, had shared the fate of "Soonga lem Paccula," (Zunga chya Makula?) a stone placed in the map north-east of the Makula or Annan debouchure; both were invisible, denoted only by swirls in the water. We had taken seven hours to cover what we easily ran down in two, and we slept comfortably with groan of rock and roar of stream for lullaby.

September 7.—Our course now lay uninterruptedly along the left bank, where the scenery became yet more Rhine-like, in natural basins, reaches on the chart: here and there rugged uprocks passably simulated ruined castles. The dwarf bays of yellow sand were girt by a goodly vegetation, the palm and the calabash only telling us that we were in Africa.

Our men pointed to the work of a Nguvu or hippopotamus, which they say sometimes attacks canoes; they believe with Tuckey that the river-horses cause irregularity of soundings by assembling and trampling deep holes in the bed; but the Ngadi is a proof that they do not, as M. du Chaillu supposes, exclusively affect streams with shoals and shallows. The jacaré (crocodile) is known especially to avoid the points where the current sweeps swiftly past, yet no one will hang his hand over the canoe into the water: we did not see any of these wretches, but at Boma Coxswain Deane observed one about sixteen feet long.

Curls of smoke arose from the mountain-walls of the trough, showing that the bush was being burned; and spired up from a grassy palm-dotted plain, between two rocky promontories on the left bank, the site of the Chacha or Wembo village: in a gap of the herbage stood half-finished canoes, and a man was bobbing with rod, line, and float. After an hour's paddling we halted for breakfast under "Alecto Rock," a sheer bluff of reddish schist, 150 feet high; here a white trident, inverted and placed ten feet above the water, showed signs of H.M. Ship "Alecto," (late) Captain Hunt, whose boat passed up in 1855. The people call it Chimbongolo. The river is now three quarters of a mile wide, and the charming cove shows the brightest of sands and the densest of vegetation waving in the cool land-wind.