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Sleeman, William, 1788-1856

"II"

The abundance of the chloride of sodium in the soil,
from which the superabounding carbonates of soda are formed, seems to
indicate, unequivocally, that the bed from which they are brought to
the surface by capillary attraction must at some time have been
covered by salt water.
The soil of Scind, which was at one time covered by the sea, seems to
suffer still more generally from the same superabundance of the
carbonates of soda, formed from the _chlorides of sodium_, and
brought to the surface in the same manner. But in Scind the evil is
greater and more general from the smaller quantity of rain that
falls. Egypt would, no doubt, suffer still more from the same cause,
inasmuch as it has still less rain than Scind, but for the annual
overflowing of the Nile. The greater part of the deserts which now
disfigure the face of the globe in hot climates arise chiefly from
the same causes, and they may become covered by tillage and
population as man becomes wiser, more social, and more humane.
_January_ 9, 1850.--Halted at Nawabgunge. A vast deal of grain of all
sorts has for the last two years passed from Cawnpoor to Lucknow for
sale. The usual current of grain is from the northern and eastern
districts of Oude towards Cawnpoor; but for these two years it has
been from Cawnpoor to these districts. This is owing to two bad
seasons in Oude generally, and much oppression in the northern and
eastern districts, in particular, and the advantage which the
navigation of the Ganges affords to the towns on its banks on such
occasions.


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