The physiography of the river Nile and is basin . )-sided ravine deeply cut intothe basalt plateau until only IG kilometres from its source it is flowingin a ravine 600 metres deep ; - at some 50 kilometres east of themountains of Debra Tabor it turns northwards being joined bynumerous small tributaries, and others like tlie Tserare and the Ghivawhich are large streams, carr3-ing a considerable volume in the In about lat. 18° 12 N., near where the road from Aduato Gondar crosses it, the Takazze turns westwards and following ageneral direction somewhat north of w-est finally, unde
The physiography of the river Nile and is basin . )-sided ravine deeply cut intothe basalt plateau until only IG kilometres from its source it is flowingin a ravine 600 metres deep ; - at some 50 kilometres east of themountains of Debra Tabor it turns northwards being joined bynumerous small tributaries, and others like tlie Tserare and the Ghivawhich are large streams, carr3-ing a considerable volume in the In about lat. 18° 12 N., near where the road from Aduato Gondar crosses it, the Takazze turns westwards and following ageneral direction somewhat north of w-est finally, under the name of 1 As the gauges are only read once a day it is not always possible to determine with accuracythe time taken by tlie flood wave. * Markham .lour. K. (ieojf. Sue. , p. 42. PLATE XXVIII SECTIONS OF RAHAD RIVER No- 1 400 Km. from NHa 3 1 03. No. 2 Khor Abu So<h«lp, 20 Km. fV^»m Nil« 13 12 02.
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