The wide gulf near Cape Michael, which the winter had closed, had
reopened gradually, and now ran a mile inland, as far as the dried-up
bed of the little river. It was probable that it was soon to extend to
the bed itself, which was of course of little thickness, having been
hollowed out by the stream. Should it do so, the whole district between
Cape Michael and Port Barnett, bounded on the west by the river bed,
would disappear—that is to say, the colonists would lose a good many
square miles of their domain. On this account Hobson warned every one
not to wander far, as a rough sea would be enough to bring about the
dreaded catastrophe.
Soundings were, however, taken, in several places with a view to
ascertaining where the ice was thickest, and it was found that, near
Cape Bathurst, not only was the layer of earth and sand of greater
extent—which was of little importance—but the crust of ice was
thicker than anywhere else. This was a most fortunate circumstance,
and the holes made in sounding were kept open, so that the amount of
diminution in the base of the island could be estimated every day. This
diminution was slow but sure, and, making allowance for the unfortunate
fact that the island was drifting into warmer waters, it was decided
that it was impossible for it to last another three weeks.
The next week, from the 19th to the 25th May, the weather was very bad.
A fearful storm broke over the island, accompanied by flash after
flash of lightning and peals of thunder. The sea rose high, lashed by
a powerful north-west wind, and its waves broke over the doomed island,
making it tremble ominously. The little colony were on the watch, ready
on an emergency to embark in the raft, the scaffolding of which was
nearly finished, and some provisions and fresh water were taken on
board.
Rain heavy enough to penetrate to the ice-crust fell in large quantities
during this storm, and melted it in many places. On the slopes of some
of the hills the earth was washed away, leaving the white foundations
bare. These ravines were hastily filled up with soil to protect the ice
from the action of the warm air and rain, and but for this precaution
the soil would have been everywhere perforated.
Great havoc was caused amongst the woods by this storm; the earth and
sand were washed away from the roots of the trees, which fell in large
numbers. In a single night the aspect of the country between the lake
and the former Port Barnett was completely changed. A few groups of
birch trees and thickets of firs alone remained—a fact significant of
approaching decomposition, which no human skill could prevent! Every one
knew and felt that the ephemeral inland was gradually succumbing—every
one, except perhaps Thomas Black, who was still gloomily indifferent to
all that was going on.
Public-domain text, read in full here on John Shaqi.
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