Wealth of the World's Waste Places and OceaniaGilson, Jewett C. (Jewett Castello)
Science
Wealth of the World's Waste Places and Oceania
Gilson, Jewett C. (Jewett Castello)
Oceania -- Economic conditions; Waste lands
Unlike the ocean waves, in which only the form moves forward, while the
water composing it moves up and down only, the sand dune and the
material of which it is composed are both moving in the direction of
the wind. A breeze even of five or six miles an hour will keep the
lighter surface dust moving freely, while a twelve-mile wind will not
only sweep along much larger particles but it also carries more of them.
And just as the surface, or "skin," friction forms waves at the surface
of water, it also piles the desert sand in wave-like dunes.
The loose bits of rock waste are carried along, up the windward slope of
the dune until they roll over its crest, where, no longer impelled by
the wind, they come to rest. Thus, the crest, built forward by new
material constantly added, is advancing. Valleys are filled; old stream
channels are obliterated; and the inequalities of the surface are
levelled off until the whole landscape is one of shifting, drifting
sand.
Notwithstanding all these drawbacks, the Sahara and the arid lands
southward to the Sudan are by no means destitute of life and wealth. It
is an almost universal custom to speak of the barren condition of the
desert. The contrary is the truth; there is no soil elsewhere so fertile
and productive. It is vastly superior even to the soil of the lands
reclaimed from the bottom of the North Sea.
Water is the magic wand that makes the sands of the Sahara bring forth
crops that are marvellous both in quantity and quality. No fruit grown
elsewhere in the world can compare with that grown on desert lands, and
the French engineers are planning the means whereby water may be
obtained. Surface water that is available to irrigate the wastes of the
Sahara does not exist. The level of the Nile is so far below the surface
on both sides of its own flood-plain that its waters cannot be used for
the reclamation of any part of the Libyan Desert, and the same is
practically true of the Niger, which barely more than touches the
borders of the Sahara. The few wadys, or "dry washes," are destitute of
water except when a cloud-burst may fill them; but this happens at
intervals of years only.
The engineer takes into his confidence a caravan driver--perhaps an
Arab, possibly a Berber, but quite as likely a slave. And the long
experience has taught the caravan man where to find the precious water.
The engineer then brings his science into play and drives an artesian
well. The well thus driven may be a "gusher," but for most of them pumps
are required to raise the water to the surface. The best well, however,
furnishes water enough to irrigate but a very small area. Indeed, all
the lands of the Sahara together irrigated by artesian wells would make
an area scarcely larger than the State of Delaware, and all the water
thus obtained would not supply New York City!
Public-domain text, read in full here on John Shaqi.
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