England and Canada: A Summer Tour Between Old and New Westminster, with Historical NotesFleming, Sandford
History
England and Canada: A Summer Tour Between Old and New Westminster, with Historical Notes
Fleming, Sandford
Canada -- Description and travel
Our poor horses could only nibble the leaves of the devil’s club in
the attempt to satisfy hunger. There was nothing to be done but to
proceed, and as soon as possible reach good pasture at the summit. We
were now no longer by Beaver River. We had followed it for fifteen
miles, and had ascended a branch named Bear Creek. We heard that a
number of these creatures are to be met in this locality. The surveying
party had seen as many as fifty. We pass through a tall forest until
we reach a rugged mountain defile leading up to the summit, which we
are to cross. The mountain peaks rise high above us, and although it is
far advanced in the forenoon the sun has not yet appeared to us in the
defile, for it has not yet ascended to the lofty horizon. We crossed
many old avalanche slides. On the southern side of the mountains, as we
wind our way, great scaurs, banked with snow, are seen two hundred or
three hundred feet above the bottom of the narrow valley through which
Bear Creek flows. To the north we observe a glacier, possibly fifty
yards thick at its overhanging termination. It takes its origin at some
remote lofty source far beyond the reach of our view. Below the glacier
on the mountain side there are traces of a heavy avalanche, where trees
have been broken and crushed in all directions. Judging from the age
of the timber the movement must have taken place a considerable time
back, and was probably caused by the breaking off of a huge mass of the
glacier. What could have been more majestic than the fall of one of
those great glaciers, in its descent driving everything before it as
stubble in the field.
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