The Albert N'Yanza, Great Basin of the Nile And Explorations of the Nile Sources by Sir Samuel W. Baker









 -  12 degrees 30 minutes;
descending its banks I crossed over a narrow strip of country to the
west, arriving at - Page 14
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12 Degrees 30 Minutes; Descending Its Banks I Crossed Over A Narrow Strip Of Country To The West, Arriving At

The river Dinder, and following these streams to their junction with the Blue Nile, I descended that grand river to

Khartoum, having been exactly twelve months from the day I had left Berber.

The whole of the above-mentioned rivers - i.e. the Atbara, Settite, Salaam, Angrab, Rahad, Dinder, and Blue Nile - are the great drains of Abyssinia, all having a uniform course from southeast to northwest, and meeting the main Nile in two mouths; by the Blue Nile at Khartoum, 15 degrees 30 minutes, and by the Atbara, in lat. 17 degrees 37 minutes. The Blue Nile during the dry season is so reduced that there is not sufficient water for the small vessels engaged in transporting produce from Sennaar to Khartoum; at that time the water is beautifully clear, and, reflecting the cloudless sky, its colour has given it the well-known name of Bahr el Azrak, or Blue River. No water is more delicious than that of the Blue Nile; in great contrast to that of the White river, which is never clear, and has a disagreeable taste of vegetation. This difference in the quality of the waters is a distinguishing characteristic of the two rivers: the one, the Blue Nile, is a rapid mountain stream, rising and falling with great rapidity; the other is of lake origin, flowing through vast marshes. The course of the Blue Nile is through fertile soil; thus there is a trifling loss by absorption, and during the heavy rains a vast amount of earthy matter of a red colour is contributed by its waters to the general fertilizing deposit of the Nile in Lower Egypt.

The Atbara, although so important a river in the rainy season of Abyssinia, is perfectly dry for several months during the year, and at the time I first saw it, June 13, 1861, it was a mere sheet of glaring sand; in fact a portion of the desert through which it flowed. For upwards of one hundred and fifty miles from its junction with the Nile, it is perfectly dry from the beginning of March to June. At intervals of a few miles there are pools or ponds of water left in the deep holes below the general average of the river's bed. In these pools, some of which may be a mile in length, are congregated all the inhabitants of the river, who as the stream disappears are forced to close quarters in these narrow asylums; thus, crocodiles, hippopotami, fish, and large turtle are crowded in extraordinary numbers, until the commencement of the rains in Abyssinia once more sets them at liberty by sending down a fresh volume to the river. The rainy season commences in Abyssinia in the middle of May, but the country being parched by the summer heat, the first rains are absorbed by the soil, and the torrents do not fill until the middle of June.

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