The Sea Road to the East, Gibraltar to Wei-hai-wei: Six Lectures Prepared for the Visual Instruction Committee of the Colonial OfficeSargent, A. J. (Arthur John)
History
The Sea Road to the East, Gibraltar to Wei-hai-wei: Six Lectures Prepared for the Visual Instruction Committee of the Colonial Office
Sargent, A. J. (Arthur John)
Travel -- Guidebooks
Let us try to realize where we are standing. If we travel 17
southward from Wagga or from Sheikh, we go downhill, but we find
that the dried-up beds of the streams are sloping away from the
sea. We have crossed the main water-parting of the country. The
mountain ridges which we have scaled are merely the steep broken
edges of a great highland block which falls gently southwards to
a broad plateau, without hills or streams, a monotony of stones,
red earth, dust and dense thorn scrub. In the dry season we may
travel for a week or ten days together and find not a drop of
water. On the caravan routes are a few wells, such as we 18
see here, but many of these dry up, and we have to dig for a few
mouthfuls of warm, dirty water in the liquid mud at the bottom.
This is the _Haud_; it belongs partly to Britain, partly to Italy
and partly to Abyssinia, though in such a country boundaries have
little or no meaning; they are merely imaginary lines drawn from
a few known points through the unexplored area.
On the mountain slopes and on the plains at the foot are the
courses of many rivers and streams. These are marked on the map,
but few are permanent. In the rains they are rushing torrents,
overflowing the channels which are too narrow to contain them and
spreading out into wide unhealthy marshes; in the dry season
they are mere channels or _tugs_, with a few stagnant pools in
the deepest parts. The rains are of the tropical kind, beginning
in April and going on, with one break, through the summer. The
winter months are almost rainless, and the smallest annual fall
is on the coast.
The peculiarities of the plateau and the seasonal rainfall have
been largely responsible for the shaping of the Somali. He is
essentially a nomad; all his property is moveable and consists of
flocks and herds and camels. It is true that there are remains of
stone buildings, and deep wells in the rock, especially further
inland; but these are not the work of the present-day Somali; his
house is as easily moved as his cattle. In the dry weather we 19
see the herds collected round the permanent wells and on the
banks of the few streams where some water and pasture are still
to be found. Notice the primitive native method of getting 20
at the water. A man is handing it up in a jar or skin, while
another pours it into a trough for the cattle. The summer rains
bring vegetation to the dry steppe, and forthwith the people with
their animals migrate to the cooler air and fresh pasture of the
plateau. Berbera and the coast towns empty themselves in this way
in the hot weather, so that there is a great change in the size
of the population at different seasons of the year. There is no
real agriculture until we reach the borders of Abyssinia and the
river valleys in the far south and west.
Public-domain text, read in full here on John Shaqi.
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