On the addition of Formosa to her dominions, Fuji ceased to be Japan's
highest mountain, and took the third place on the list. Mount Morrison
(14,270 ft.), which the Japanese renamed Niitaka-yama (New High
Mountain), stands first, and Mount Sylvia (12,480 ft.), to which they
give the name of Setzu-zan (Snowy Mountain), comes second. Mount
Morrison stands nearly under the Tropic of Cancer. It is not volcanic,
but consists of argillaceous schist and quartzite. An ascent made by Dr
Honda of the imperial university of Japan showed that, up to a height of
6000 ft., the mountain is clothed with primeval forests of palms,
banyans, cork trees, camphor trees, tree ferns, interlacing creepers and
dense thickets of rattan or stretches of grass higher than a man's
stature. The next interval of 1000 ft. has gigantic cryptomerias and
chamoecyparis; then follow pines; then, at a height of 9500 ft., a broad
plateau, and then alternate stretches of grass and forest up to the top,
which consists of several small peaks. There is no snow. Mount Morrison,
being surrounded by high ranges, is not a conspicuous object. Mount
Sylvia lies in 24 deg. 30' N. lat. There are many other mountains of
considerable elevation. In the north is Getsurobi-zan (4101 ft.); and on
either side of Setzu-zan, with which they form a range running due east
and west across the island, are Jusampunzan (4698 ft.) and Kali-zan
(7027 ft.). Twenty-two miles due south of Kali-zan stands Hakumosha-zan
(5282 ft.), and just 20 m. due south of Hakumosha-zan begins a chain of
three peaks, Suisha-zan (6200 ft.), Hoo-zan (4928), and Niitaka-yama.
These five mountains, Hari-zan, Hakumosha-zan, Suisha-zan, Hoo-zan and
Niitaka-yama, stand almost exactly under 121 deg. E. long., in the very
centre of the island. But the backbone of the island lies east of them,
extending S. from Setzu-zan through Gokan-zan, and Noko-zan and other
peaks and bending S.W. to Niitaka-yama. Yet farther south, and still
lying in line down the centre of the island, are Sankyakunan-zan (3752
ft.), Shurogi-zan (5729 ft.), Poren-zan (4957 ft.), and Kado-zan (9055
ft.), and, finally, in the south-east Arugan-zan (4985 ft.). These, it
will be observed, are all Japanese names, and the heights have been
determined by Japanese observers. In addition to these remarkable inland
mountains, Formosa's eastern shores show magnificent cliff scenery, the
bases of the hills on the seaside taking the form of almost
perpendicular walls as high as from 1500 to 2500 ft. Volcanic outbreaks
of steam and sulphur-springs are found. Owing to the precipitous
character of the east coast few rivers of any size find their way to the
sea in that direction. The west coast, on the contrary, has many
streams, but the only two of any considerable length are the Kotansui,
which rises on Shurogi-zan, and has its mouth at Toko after a course of
some 60 m. and the Seirakei, which rises on Hakumosha-zan, and enters
the sea at a point 57 m.
Public-domain text, read in full here on John Shaqi.
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