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THE ISLAND OP KIU-SIU. 879<br />

miles from the mountain. Mud and gases escaped from innumerable fissures, and<br />

during the rains the whole ground bubbled up like a liquid mass. A former<br />

eruption of the neighbouring Miyi-yama, attended by tremendous floodings, cost<br />

the lives of 50,000 persons.<br />

South of Kiu-siu a group of volcanoes has received the name of Kiri-sima, or<br />

"Fog Island," on account of the sulphurous vapours constantly emitted by them.<br />

Here all the rocks consist of tufas, trachytes, pumice, and other igneous matter,<br />

and the plateau supporting the twin peaks of Kiri-sima is an arid region, strewn<br />

s#<br />

Fig. 177- KAOO-STMA AND MI-TAKE VOLCANO.<br />

Scale t : 300,000.<br />

E.ofG 130 30V J3I?<br />

to 100 Feet. 180 to 320 Feet 320 Feet and upwards.<br />

. c. Miles.<br />

with ashes and reddish scoriso, relieved only by a few dwarf pines and other shrubs.<br />

These appear to be the culminating points of ICiu-siu, and they are certainly more<br />

elevated than Aso-yama and Komats-yama in the south-cast.<br />

The jH-iiiiisiiIa enclosing the picturesque bay of Kago-sima on the west is one of<br />

the most remarkable regions in Japan. The long tongue of land bending<br />

round (lie b;iv is dominated by the superb Mount Kaiinon, the Cape Ilorner of<br />

European maps, which is almost unrivalled for its beautiful form and symmetrical<br />

contour. .North of it formerly stood a still more elevated volcano, the pyramidal<br />

crest of which was destroyed during an eruption, all memory of which has

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