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but little vegetation to give token of the earth’s
vitality.
One of the principal objects in coming so far '
was to see the various geysers in eruption ; but,
like many other travellers, our lonely vigil closed
without seeing the Great Geyser perform, for it is
necessary to wait its pleasure, and the chances of
an eruption are very slight. In 1770 it is
recorded that it spouted eleven times a day, and
in 1814 every six hours, but now, of all unpunctual
exhibitions, this is the most uncertain. Tourists
have been known to wait a week, and there are
legends of a wasted month. One quaint old
historian gives an account of these springs about
the year 1187. He says “ On an island in the
midst of the wild sea there is a smoking fountain
that turns everything its waters touch into stone.
It is not to bo trifled with, for it lies in ambush
to petrify all things. There are other fountains
that burst into the air and disappear in the earth.
There are springs that are of the most deadly
poison, whilst others taste like ale.” Another
writer in 1757 tells us :—“ There are two
fountains, one a cold one, which immediately
turned a cane into iron, weighing as heavy as that
metal; the other a boiling one, in which could be
seen a parcel of great animals as big as divers,
frisking about and playing together, but if anyone
approached, they immediately plunged down to
the bottom of the boiling fountain, 300 feet deep.”
Although we did not see these wonders, we saw
much to astonish us, and many hours were spent
in visiting the various springs, the smallest of
which would arrest a traveller’s attention in any
other country. The Great Geyser in the course of
ages has formed out of the silica it deposits a
mound about thirty feet high, which contains a
circular basin about 200 feet in circumference; in
the middle of this is a pipe with an opening some
16 feet in diameter, which has been probed to the
depth of 80 feet. The sides are smoothly polished
and so hard that it is not possible to strike off a
piece with a hammer. The basin was filled to the
brim with sea-green water, as pure as crystal, and
of a temperature of 186 degrees. The second largest
geyser is also surrounded by a deposit of light
flinty grit and laminae. As we first looked down
its tube fifty feet deep, we could see the water ten
or twelve feet from the surface—boiling hard,
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