The Great Frozen Sea: A Personal Narrative of the Voyage of the "Alert" — John Shaqi
The Great Frozen Sea: A Personal Narrative of the Voyage of the "Alert"Markham, Albert Hastings, Sir
History
The Great Frozen Sea: A Personal Narrative of the Voyage of the "Alert"
Markham, Albert Hastings, Sir
Alert (Sloop : 1856-1895); Arctic regions; Nares, George S. (George Strong), 1831-1915
"On those great waters now I am,
Of which I have been told,
That whosoever hither came
Should wonders there behold.
"Trim thou the sails, and let good speed
Accompany our haste;
Sound thou the channels at our need,
And anchor for us cast.
"A fit and favourable wind
To further us provide,
And let it wait on us behind,
Or lackey by our side."
GEORGE WITHER.
The morning following our arrival in Alexandra Harbour saw us again
battling with the ice in Hayes Sound, having been deluded into leaving
our comfortable snug quarters by the report that the pack had drifted to
the eastward, leaving a navigable channel extending to the north. The
report was fallacious, but we succeeded in threading our way to the N.W.
for about twenty miles, when both ships were helplessly beset, with but
little hope of extrication without a shift of wind.
Many broad glaciers were in view, winding their long white snaky
lengths between the hills, some of which could be traced into the
interior for ten or twelve miles, or until lost in illimitable space.
In twenty-four hours, the ice slackening enabled us to bore a way
through, eventually emerging into a broad stream of water. How sudden
and wonderful are the changes in these regions! From being closely
beset, a couple of hours saw us in an apparently open sea with _no ice_
in sight, and bowling along before a fresh southerly gale at the rate of
seven knots. Social barometer very high! In the morning not a spoonful
of water to be seen in any direction, in the evening not a vestige of
ice!
Passing close to the western shore we were able to confirm our views
regarding the Henry and Bache Islands of Hayes. They are undoubtedly
connected, and therefore not islands; but whether they were also
connected with the mainland we were not able to determine. In all
probability the supposed islands are a peninsula, apparently of
sandstone formation overlying trap, different to the granitic formation
of the southern shore of the strait. The land appeared quite bare of
vegetation, and bore a strong resemblance to the Silurian limestone
formation of the land about Prince Regent Inlet, showing stratifications
dipping to the northward at an angle of about 6°.
It does not do to indulge too freely in vain hopes in these regions. A
period of eight hours was sufficient to cause our hopeful anticipations
of a grand run to the northward to be "considerably eased down;" for in
that time we were again stopped by the ice, and compelled to make fast
to a floe, until the pack opened sufficiently to allow us to proceed.
During the run we passed some very heavy floes--heavier than anything
we had hitherto met, and quite sufficient in themselves to crush any
unfortunate ship that should happen to get nipped between two of them.
Public-domain text, read in full here on John Shaqi.
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