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386<br />

EAST ASIA<br />

HYDROGRAPHIC SYSTEM CHIEF RIVERS.<br />

Owing to the narrowness of the land, which is nowhere 200 miles wide, and to<br />

the extremely mountainous character of its surface, no room is left for the develop-<br />

ment of large streams. The rivers, which are numerous enough, especially in<br />

Yeso and Hondo, in fact, resemble mountain torrents, with short and rapid courses,<br />

and, in their lower reaches, subject to sudden and disastrous inundations. They are<br />

consequently more damaging than beneficial even for irrigation purposes. To<br />

navigation they are not merely useless, but a positive hindrance, in consequence<br />

of the large quantities of sedimentary matter which they wash down, and by which<br />

several of the best harbours in the archipelago have already been choked up.<br />

Such has especially been the fate of Osaka and Nihi-gata harbours on the east and<br />

west sides of Nip-pon, which were formerly accessible to the largest vessels, but<br />

which can now be approached only by small craft. In Japan " a river-bed is a<br />

waste of sand, boulders and shingle, through the middle of which, among sand-<br />

banks and shallows, the river proper takes its devious course. In the freshets which<br />

occur to a greater or less extent every year, enormous volumes of water pour over<br />

these wastes, carrying sand and detritus down to the mouths, which are all ob-<br />

structed by bars. Of these rivers the Shinano, being the biggest, is the most refractory,<br />

and has piled up a bar at its entrance through which there is only a<br />

passage 7 feet deep, which is perpetually shallowing." *<br />

Subjoined is a table t of all the Japanese rivers, which have a total course of more<br />

than 50 miles :<br />

Name.

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