This Rapidity Also, Bringing Down Vast Quantities Of Soil, Has So
Raised The Bed That In Recent Times The Tide
Has not entered the river, as
it probably did in our traveller's time, when, as it would appear from his
Account, seagoing craft used to ascend to the ferry north of Hwai-ngan fu,
or thereabouts. Another indication of change is his statement that the
passage just mentioned was only one day's journey from the sea, whereas it
is now about 50 miles in a direct line. But the river has of late years
undergone changes much more material.
In the remotest times of which the Chinese have any record, the Hwang-Ho
discharged its waters into the Gulf of Chih-li, by two branches, the most
northerly of which appears to have followed the present course of the
Pei-ho below Tien-tsing. In the time of the Shang Dynasty (ending B.C.
1078) a branch more southerly than either of the above flowed towards
T'si-ning, and combined with the T'si River, which flowed by T'si-nan fu,
the same in fact that was till recently called the Ta-t'sing. In the time
of Confucius we first hear of a branch being thrown off south-east towards
the Hwai, flowing north of Hwai-ngan, in fact towards the embouchure which
our maps still display as that of the Hwang-Ho. But, about the 3rd and 4th
centuries of our era, the river discharged exclusively by the T'si; and up
to the Mongol age, or nearly so, the mass of the waters of this great river
continued to flow into the Gulf of Chih-li.
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