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
I determined not to wait for the waggon, but to push on to the next
stopping place and see what arrangements could be made for our further
advance. The baggage was to follow. I was much struck with the view as
we started. It was very fine, but its effect was marred by the cloudy
atmosphere which hid the more distant peaks. For twenty-two miles to
Padmore the whole route was equally striking. The valley is from three
to eight miles wide, extending generally in a western direction between
the foot hills of the mountains. It is marked by no sudden precipitous
ascents and is usually flat, carrying the prairie character with a
gentle ascent into the heart of the mountains. We are told that at one
time this valley, with the country around Morley and Calgary, was the
haunt of the buffalo. Mr. David Macdougall tells us that he has seen
the ground black with them, and that from an eminence not far from
Morley he has beheld them in herds on the plains, the number of which
would not be less than a million!
The prairie diminishes in extent as we advance. We pass through
park-like scenery. Groups of trees appear at intervals, and the
Bow River in its windings gleams pleasantly in the sun. The heavy
atmosphere is partially lifted and the outline of the mountains in
the distance comes to our view. What we see is probably the outlying
group; they are, nevertheless, bold bluffs, some of them defined
precipices to the summit, with long slopes in one direction, and in
some cases their fantastic forms look as if shaped in masonry.
The streams crossed to-day run in ravines of some depth, and the water
is clear and cold. We halt at Padmore, where the valley is contracted
to half a mile. Evidently we are about entering the portals of the
mountains. To the north, the slopes are bare; to the south, they are
wooded. The bare precipitous rock to the north is stratified and
strongly contorted. The geological features are most striking and the
exposure is on a grand scale. A great bluff rises nearly vertically
to the height of possibly fifteen hundred feet and is about two miles
in length. The lines of the strata are distinctly traceable, dipping
towards the west.
Four miles west of Padmore we are completely in the mountains. On every
side the sound of the hammer and drill was heard, and every turn of
the road revealed new views of the grandest mountain scenery. Peaks
towering behind and above each other came in sight, and the sun poured
down its warmest rays, deepening the shadows and bringing out fresh
beauties. As we advanced, the eye rests only on these mighty heights
when they are not concealed from view by the hazy atmosphere. The smoky
air, occasionally, it seemed to me, opened up, and in a way added to,
the landscape by developing the aerial perspective. As we advanced the
vapour disappeared, and before us stood out, clear and well defined in
the horizon, bold, massive mountain heights, crowned by sharp, turreted
peaks.
Public-domain text, read in full here on John Shaqi.
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