The Hawaiian Archipelago - Six Months Among The Palm Groves, Coral Reefs, And Volcanoes Of The Sandwich Islands By Isabella L. Bird
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I Mentioned In One Of My First Letters That East Maui, That Part Of
The Island Which Lies East Of The Isthmus Of Perpetual Dust-Storms,
Consists Of A Mountain Dome 10,000 Feet In Height, With A Monstrous
Base.
Its slopes are very regular, varying from eight to ten
degrees.
Its lava-beds differ from those of Kauai and Oahu in being
lighter in colour, less cellular, and more impervious to water. The
windward side of the mountain is gashed and slashed by streams,
which in their violence have excavated large pot-holes, which serve
as reservoirs, and it is covered to a height of over 2000 feet by a
luxuriant growth of timber. On the leeward side, several black and
very fresh-looking streams of lava run into the sea, and the whole
coast for some height above the shore shows most vigorous volcanic
action. Elsewhere the rock is red and broken, and lateral cones
abound near the base.
The ascent from Makawao, though it is over rather a desolate tract
of land, has in its lower stages such a dismal growth of pining koa
and spurious sandal-wood, and in its upper ones so much ohelo scrub,
with grass and common aspleniums quite up to the top, that as one
sits lazily on one's sure-footed horse, the fact that one is
ascending a huge volcano is not forced upon one by any overmastering
sterility and nakedness. Somehow, one expects to pass through some
ulterior stage of blackness up to the summit. It is no such thing;
and the great surprise of Haleakala to me was, that when according
to calculation there should have been a summit, an abyss of vast
dimensions opened below. The mountain top has been in fact blown
off, and one is totally powerless to imagine what the forces must
have been which rent it asunder.
The crater was clear of fog and clouds, and lighted in every part by
the risen sun. The whole, with its contents, can be seen at a
single glance, though its girdling precipices are nineteen miles in
extent. Its huge, irregular floor is 2000 feet below; New York
might be hidden away within it, with abundant room to spare; and
more than one of the numerous subsidiary cones which uplift
themselves solitary or in clusters through the area, attain the
height of Arthur's Seat at Edinburgh. On the north and east are the
Koolau and Kaupo Gaps, as deep as the crater, through which oceans
of lava found their way to the sea. It looks as if the volcanic
forces, content with rending the mountain top in twain, had then
passed into an endless repose.
The crater appears to be composed of a hard grey clinkstone, much
fissured; but lower down the mountain, the rock is softer, and has a
bluish tinge. The internal cones are of very regular shape, and
most of them look as if their fires had only just gone out, with
their sides fiercely red, and their central cavities lined with
layers of black ash. They are all composed of cinders of light
specific gravity, and much of the ash is tinged with the hydrated
oxide of iron. Very few of the usual volcanic products are present.
{335} Small quantities of sulphur, in a very impure form, exist
here and there, but there are no sulphur or steam-cracks, or hot
springs on any part of the mountain. With its cold ashes and dead
force, it is a most tremendous spectacle of the power of fire.
Some previous travellers had generously left some faggots on the
summit, and we made a large fire for warmth, and I rolled my blanket
round me, and sat with my feet among the hot embers, but all to no
purpose. The wind was strong and keen, and the fierce splendour of
the tropic sun conveyed no heat. Mr. A. went away investigating,
the native rolled himself in his poncho and fell asleep by the fire,
and I divided the time between glimpses into the awful desolation of
the crater, snatched between the icy gusts of wind, and the
enjoyment of the wonderful cloud scenery which to everybody is a
great charm of the view from Haleakala. The day was perfect; for
first we had an inimitable view of the crater and all that could be
seen from the mountain-top, and then an equally inimitable view of
Cloudland. There was the gaunt, hideous, desolate abyss, with its
fiery cones, its rivers and surges of black lava and grey ash,
crossing and mingling all over the area, mixed with splotches of
colour and coils of satin rock, its walls dark and frowning,
everywhere riven and splintered, and clouds perpetually drifting in
through the great gaps, and filling up the whole crater with white
swirling masses, which in a few minutes melted away in the sunshine,
leaving it all as sharply definite as before. Before noon clouds
surrounded the whole mountain, not in the vague flocculent,
meaningless masses one usually sees, but in Arctic oceans, where
lofty icebergs, floes and pack, lay piled on each other, glistening
with the frost of a Polar winter; then alps on alps, and peaks of
well remembered ranges gleaming above glaciers, and the semblance of
forests in deep ravines loaded with new fallen snow. Snow-drifts,
avalanches, oceans held in bondage of eternal ice, and all this
massed together, shifting, breaking, glistering, filling up the
broad channel which divides Maui from Hawaii, and far away above the
lonely masses, rose, in turquoise blue, like distant islands, the
lofty Hawaiian domes of Mauna Kea and Mauna Loa, with snow on Mauna
Kea yet more dazzling than the clouds. There never was a stranger
contrast than between the hideous desolation of the crater below,
and those blue and jewelled summits rising above the shifting
clouds.
After some time the scene shifted, and through glacial rifts
appeared as in a dream the Eeka mountains which enfold the Iao
valley, broad fields of cane 8000 feet below, the flushed palm-
fringed coast, and the deep blue sea sleeping in perpetual calm.
But according to the well-known fraud which isolated altitudes
perpetrate upon the eye, it appeared as if we were looking up at our
landscape, not down; and no effort of the eye or imagination would
put things at their proper levels.
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