Frank Richardson Cana

Summary

Frank Richardson Cana 1911 Encyclopædia Britannica, Volume 6… (1911)

From the high lands of the south and east in which the head-streams of the Congo have their origin, the land falls in a succession of steps, generally marked by gorges or rapids in the upper courses of the streams. Besides the main stream most of the affluents of the river are navigable for considerable distances; in all there are over 6000 m. of navigable water in the Congo basin and 20,000 m. of overhanging wooded banks. On the Congo alone are over 4000 islands, many of considerable length—some fifty of them are over ten miles long.
Source: Wikisource

Frank Richardson Cana 1911 Encyclopædia Britannica, Volume 6… (1911)

Between the rapids named and 7° 40′ S. its valley is studded with a chain of small lakes and backwaters. The largest—Upemba—has channels communicating both with the Lualaba and the Lufira. In the rainy season the whole region becomes a marsh; various grasses, especially papyrus, form floating islands, and the conditions generally recall the sudd region of the Nile. In about 8° 20′ S. the Lualaba and Lufira unite in one of these marshy lakes—Kisale—through which there is a navigable channel. The river issuing from Lake Kisale is called Kamolondo; it has a width varying from 300 to 1000 ft.
Source: Wikisource

Frank Richardson Cana 1911 Encyclopædia Britannica, Volume 6… (1911)

From Bangweulu to Mweru the fall of the river in a total distance of 350 m. is about 700 ft. The river (known now as the Luvua) makes its exit at the N.W. corner of the lake, and bending westwards in a winding course, passes, with many rapids, across the zone of the Kebara and Mugila mountains, falling during this interval nearly 1000 ft. In about 6° 45′ S., 26° 50′ E. it joins the Kamolondo (otherwise Lualaba) , the western main branch of the Congo, which, as it flows in a broad level valley at a lower level than the eastern branch, is held by some to be the true head-stream.
Source: Wikisource

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