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The universal geography : earth and its inhabitants

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THE CHOBE BTTER. 2414,500 feet above sea- level. It flows at first towaras tlic south-east, <strong>and</strong> is soouswollen by the contributions of innumerable streamlets into the proportions of averitable river navigable for the greater part of <strong>its</strong> course, although obstructedhere <strong>and</strong> there by forests of tall reeds. In this region <strong>its</strong> basin is separated bya scarcely perceptible sill from that of the Zambese properly so called. ^Neverthelessit still maintains <strong>its</strong> independent course west of this low parting line, flowina southerly direction parallel with the main stream, <strong>and</strong> at lust emerging onthe great alluvial plain -which also receives the discharge of the Ku-Bango. <strong>The</strong>Fig. 69. Kass.u, Ku-Baxgo, axd Zajdjese.Scale 1 : 11,000,000.^-;^.-E:.:.:.':cFGKwa-Ndo even occasionally effects a junction with this river during exceptionalfloods, <strong>and</strong> then sweeps round to the cast, here exp<strong>and</strong>ing into the serpentineLake Chobe, which in many places takes the aspect of a river. When I^ivingstoncexplored it, the current had a mean depth of from 1-t to IG feet, but wouldnevertheless be inaccessible to a steamer of any size owing to <strong>its</strong> extremely sharpwindings.<strong>The</strong> junction of the Chobe with the Zambese is effected through an intricatelabyrinth of little channels <strong>and</strong> passages, in the midst of which st<strong>and</strong>s an isl<strong>and</strong>VOL. XIII. u

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