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Accordingly, the Asua, receiving the Atabbi river, which is the main drain of the western face of the Madi mountains, and the entire drainage of the Madi and Shooa countries, together with that of extensive countries to the east of Shooa, including the rivers Chombi and Udat, from Lira and Umiro, it becomes a tremendous torrent so long as the rains continue, and conveys a grand volume of water to the Nile; but the inclination of all these countries tending rapidly to the northwest, the bed of the Asua river partakes of the general incline, and so quickly empties after the cessation of the rains that it becomes nil as a river.
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