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190<br />

EAST ASIA.<br />

Shansi, Kansu, half of Shensi, the northern division of Honan, and extensive tracts<br />

in Shantung. This formation, comprising a France, reaches in some places even to the<br />

region larger than the whole of<br />

banks of the Yang-tze, and stretches<br />

westwards to the Tibetan plateaux.<br />

In these is<br />

regions everything yellow hills,<br />

fields, highways, houses, the very torrents and streams charged with alluvia.<br />

Even the is<br />

vegetation<br />

often covered with a yellow veil, while every puff<br />

of wind<br />

raises clouds of fine dust. From these lands the Emperor himself takes the title of<br />

Hoang-ti, or " Yellow Lord," equivalent to " Master of the World." According<br />

EofG.<br />

pig. 87. YELLOW LANDS OP NOBTH CHINA.<br />

Scale 1 : 18,000,000.<br />

Alluvium. Yellow Lands. Red Alluvinm. Palteozoie. Metamorphic. Volcanic. Carboniferous<br />

-^^^ _^_ 300 Miles.<br />

to Richthofcn, the hoang-tu, regarded by him as a formation analogous to the loess<br />

of the Rhine and Danube basins, is nothing more than so much dust accumulated<br />

during the course of ages by the northern Avinds. In any<br />

1C'<br />

case it cannot be of<br />

glacial origin, for, instead of being simply heaped up like the moraine deposits, it is<br />

pierced by vertical holes ramifying in various directions, and caused by the stems<br />

and roots of plants gradually covered by the dust. Nor is the hoang-tu deposited<br />

in layers like the alluvia of running waters, while it is destitute of marine fossils-<br />

attesting a possible submersion of the land under the ocean.

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