At Annesley Bay the narrow coast plain is succeeded by foothills
separated by small valleys through which flow innumerable streams.
From these hills the ascent to the plateau which constitutes northern
Eritrea is very steep. This tableland, which has a general elevation
of about 6500 ft., is fairly fertile despite a desert region--Sheb--to
the S.E. of Keren. It is characterized by rich, well-watered valleys,
verdant plains and flat-topped hills with steep sides, running in
ranges or isolated. The highest hills in Eritrean territory rise to
about 10,000 ft. The plateau is known by various names, the region
directly west of Massawa being called Hamasen. To the west and north
the plateau sinks in terraces to the plains of the Sudan, and eastward
falls more abruptly to the Red Sea, the coast plain, known as the
Samhar, consisting of sandy country covered with mimosa and, along the
khors, with a somewhat richer vegetation.
The colony contains no navigable streams. For a short distance the
Setit (known in its upper course as the Takazze), a tributary of the
Atbara, forms the frontier, as does also in its upper course the Gash
or Mareb (see ABYSSINIA). The Mareb, often dry in summer, in the
floods is a large and impassable river. Both the Setit and Mareb have
a general westerly course across the Abyssinian plateau. The Baraka
(otherwise Barka) and Anseba rise in the Hamasen plateau near Asmara
within a short distance of each other. The Baraka flows west and then
north; the Anseba, which has a more easterly course, also flows
northward and joins the Baraka a little N. of 17 deg. N. A few miles
below the confluence the Baraka leaves Italian territory. It is (as is
the Anseba) an intermittent stream. After heavy rain it discharges
some of its water into the Red Sea north of Tokar. The whole of the
hill country north of Asmara belongs to the drainage area of the
Baraka or Anseba. Of the numerous streams which, north of the Danakil
country, run direct from the hills to the Red Sea, the Hadas may be
mentioned, as along the valley of that stream is one of the most
frequented routes to the tableland. The Hadas, in time of flood,
reaches the ocean near Adulis in Annesley Bay.
Public-domain text, read in full here on John Shaqi.
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