Somalia Rivers and Lakes

By | December 15, 2021

These climatic conditions, together with the calcareous or chalky karst nature of the prevailing rocks and the tabular form of the relief, determine the regime of the watercourses; it is for these reasons that all the watercourses of the northern part of the peninsula Рboth the marginal ones of the narrow slope of the Gulf of Aden, as well as those that turn to the Indian Ocean, some of which are very remarkable for the extension of their basin and the course length, like the Giahel, the Darror and the Nogal Рare essentially only temporary streams, generally active only a few days of the year, and sometimes lacking even morphological continuity in their current bed. The only perennial streams are those that draw from the highest and innermost massifs of the plateau and cross the southernmost and therefore less arid part of the peninsula: Uebi Scebeli and Giuba. The first, flows from the Malche Mountains in the Sidamo country at 2860 m., Describing a great arc of a circle; its narrow and deep valley, interrupted by picturesque waterfalls, collects the waters of the Arussi and Harar plateaus from the left by means of numerous tributaries: Halal, Hadido, Daro, Scianan, Dungata, Ramis, Errer, Dacato. The middle course, downstream from Imi, crosses an arid region, in which not only does any significant water supply cease, but evaporation and floods remove more and more water from the river, until it runs out before reaching the Juba, which it would be direct. Dungata, Ramis, Errer, Dacato. The middle course, downstream from Imi, crosses an arid region, in which not only does any significant water supply cease, but evaporation and floods remove more and more water from the river, until it runs out before reaching the Juba, which it would be direct. Dungata, Ramis, Errer, Dacato. The middle course, downstream from Imi, crosses an arid region, in which not only does any significant water supply cease, but evaporation and floods remove more and more water from the river, until it runs out before reaching the Juba, which it would be direct. For Somalia public policy, please check loverists.com.

The Giuba or Ganana originates from three main branches, the Ganale Doria, the Daua Parma and the Uebi Gestro, which with their tributaries form a dense and complex system of valleys deeply furrowing the plateau of the Sidama, the Giam Giam, the Borana and the Arussi. The middle course can be started in Dolo, where the Ueb from the left and the Daua from the right converge at a short distance from each other. In the middle and lower course the river, wide and rich in water, does not receive perennial or even temporary taxes, which are of any importance: it is nevertheless navigable and bordered by forests or crops. It flows into the Indian Ocean at Giumbo, just north of Chisimaio (see Juba). Downwards Juba heads from Somalia the Lacderr, which is the temporary emissary of the Lorian swamps, in Kenyaland, fed in turn by the Uaso Nyiro: the Lacderr spreads near the Juba in a swampy depression, the Descec Uama. In the Oltregiuba some marginal watercourses, such as the Bubasci and the Anole, flow into the ocean through estuaries.

Real lakes do not exist in Somalia; however, there are numerous small stretches of water of karst origin or due to the irregular flow of streams.

The main underground water resources are related to the sub-river course of the streams, or to a karst system that often supplies discrete water, or to the direct absorption by the surface sands, and then the water is often more or less loaded with salts.. Deep aquifers, often brackish, have been identified in the floodplains of Uebi Scebeli and Juba.

Somalia Rivers