The Story of the Hills: A Book About Mountains for General Readers.Hutchinson, H. N. (Henry Neville)
Science
The Story of the Hills: A Book About Mountains for General Readers.
Hutchinson, H. N. (Henry Neville)
Mountains
"The abyss, which really is at a height of four thousand feet,
on the flank of Mauna Loa, has the appearance of a pit on
a rolling plain. But such a pit! It is quite nine miles in
circumference, and at its lowest area--which not long ago fell
about three hundred feet, just as ice on a pond falls when
the water below is withdrawn--covers six square miles. The
depth of the crater varies from eight hundred to one thousand
feet, according as the molten sea below is at flood or ebb.
Signs of volcanic activity are present more or less throughout
its whole depth, and for some distance round its margin, in
the form of steam-cracks, jets of sulphurous vapour, blowing
cones, accumulating deposits of acicular crystals of sulphur,
etc., and the pit itself is constantly rent and shaken by
earthquakes. Grand eruptions occurred with circumstances
of indescribable terror and dignity; but Kilauea does not
limit its activity to these outbursts, but has exhibited its
marvellous phenomena through all known time in a lake or lakes
on the southern part of the crater three miles from this side.
"This lake--the _Hale-mau-mau_, or 'House of Everlasting Fire,'
of the Hawaiian mythology, the abode of the dreaded goddess
Pele--is approachable with safety, except during an eruption.
The spectacle, however, varies almost daily; and at times the
level of the lava in the pit within a pit is so low, and the
suffocating gases are evolved in such enormous quantities, that
travellers are unable to see anything. There had been no news
from it for a week; and as nothing was to be seen but a very
faint bluish vapour hanging round its margin, the prospect was
not encouraging.... After more than an hour of very difficult
climbing, we reached the lowest level of the crater, pretty
nearly a mile across, presenting from above the appearance
of a sea at rest; but on crossing it, we found it to be an
expanse of waves and convolutions of ashy-coloured lava, with
huge cracks filled up with black iridescent rolls of lava only
a few weeks old. Parts of it are very rough and ridgy, jammed
together like field-ice, or compacted by rolls of lava, which
may have swelled up from beneath; but the largest part of the
area presents the appearance of huge coiled hawsers, the ropy
formation of the lava rendering the illusion almost perfect.
These are riven by deep cracks, which emit hot sulphurous
vapours....
Public-domain text, read in full here on John Shaqi.
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