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
Notwithstanding these lessons, some of the Turkoman tribes still went on
marauding expeditions, robbing, killing, and enslaving their neighbors.
So, in 1878, another strong force of the Cossacks was sent against the
pillaging tribes, who were made to release all slaves and abolish
slavery. Little by little all Turkistan became Russian territory.
Bokhara and Khiva alone keep their old forms of government, but they are
practically Russian states and pay Russia annually a stipulated tribute.
It is thought that once upon a time Siberia had a much larger population
than it has now and the peoples who lived there dwelt farther north. The
first colonists lived in the stone age and were contemporaneous with the
mammoth, whose remains are found scattered all over the northern part of
Siberia and the adjacent islands.
In the interior these remains are found imbedded in thick strata of pure
blue ice, which is covered by the river gravels of streams that do not
now exist. So thick are these layers of ice that they may be likened to
the rocks found in lower latitudes. Several of these animals have been
found imbedded in the ice in an almost perfect state of preservation,
and quantities of their tusks are obtained annually along the northern
rivers where the spring freshets have worn away the banks of the
streams.
Whenever the ivory-tusk hunter sees the end of a tusk sticking out of
the river bank, he is soon able to remove it from its resting place with
pick and shovel. Great quantities of this fossil ivory are also obtained
from the islands to the north of the mainland.
As in arctic America, the ground of northern Siberia is frozen solid to
the depth of many feet, and even during the hottest summer it thaws down
only a few inches. The climate is continental in character, being marked
by fierce winds and great extremes both in temperature and moisture. In
midsummer the temperature may reach one hundred and ten degrees, while
in midwinter it has been known to reach ninety degrees below zero.
Roughly speaking, Siberia may be divided into three longitudinal belts:
first, the tundra, which borders the Arctic Ocean and extends several
hundred miles south of it; second, the forest belt, several hundred
miles wide, which extends across the continent; third, the southern
part, consisting of desert steppes, swamps, grassy plains, and a few
broken forests.
The tundra is a vast lowland plain which in winter is a desolate, frozen
waste, and in summer a vast swamp of lichens and arctic moss. Here
nature is embalmed in eternal frost, and life is a terror-inspiring
struggle with cold and hunger.
Public-domain text, read in full here on John Shaqi.
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