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47. Its soil, shape, and area


MAP

FIG. 23. AN EGYPTIAN SHADOOF, THE OLDEST OF 
WELL SWEEPS, IRRIGATING THE FIELDS

The man below stands in the water, holding his leather bucket
(A). The pole (B) of the sweep is above him, with large ball
of dried Nile mud on its lower end (C) as a lifting weight, or
counterpoise, seen just behind the supporting post (D). This 
man lifts the water into a mud basin (B). A second man (in the
middle) lifts it from this first basin (F) to a second basin (F) 
into which he is just emptying his bucket; while a third man 
(C) lifts the water from the middle basin (F) to the uppermost
basin (H) on the top of the bank, where it runs off to the left 
into trenches spreading over the fields. The low water makes
necessary three successive lifts (to F, to F, to H) without 
ceasing night and day for one hundred days
 

device (Fig. 23) exactly like the well sweep of our grandfathers in New England. The irrigation trenches are thus kept full of water until the grain ripens. This shows us that Egypt enjoys no rain.

The black soil we see from the train is un- excelled in fertility, and it is enriched each year by the overflow of the river, whose turbid waters rise above its banks every summer, spread far over the flats (Fig. 24), and stand there long enough to deposit a very thin layer of rich earthy sedi- ment. This sediment has built up the Nile Delta which we are now crossing. The Delta and the valley above, as far as the First Cataract, contain together over ten thousand square miles of cultivable soil, or somewhat more than the state of Vermont. 

As our train approaches the southern [NEXT]

 

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