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
The walking is dreadful, we climb over and creep under fallen trees of
great size and the men soon show that they feel the weight of their
burdens. Their halts for rest are frequent. It is hot work for us all.
The dripping rain from the bush and branches saturate us from above.
Tall ferns sometimes reaching to the shoulder and devil’s clubs through
which we had to crush our way make us feel as if dragged through a
horse-pond and our perspiration is that of a Turkish bath. We meet
with obstacles of every description. The devil’s clubs may be numbered
by millions and they are perpetually wounding us with their spikes
against which we strike. We halt very frequently for rest. Our advance
is varied by ascending rocky slopes and slippery masses, and again
descending to a lower level. We wade through alder swamps and tread
down skunk cabbage and the prickly aralias, and so we continue until
half-past four, when the tired-out men are unable to go further. A halt
becomes necessary. We camp for the night on a high bank overlooking the
Ille-celle-waet. Three of us have dry underclothing, in water-proof
bags, but the poor men have no such luxury, so they make large fires
by which to dry themselves. Dave, our cook, fries the pork and makes
us tea in the usual way on such expeditions. We have all excellent
appetites and no fear of a bad digestion; and all quite ready to sleep,
literally and truly in spite of thunder, without criticizing the couch
on which we lie.
The Ille-celle-waet, on whose banks we have camped, has increased from
a tiny brook to a raging torrent, some fifty yards wide. The colour of
the water is much as that at London Bridge; a result possibly due to
the disintegration of the rock over which the stream rushes and to the
grinding action of the boulders rolling down the stream. A sediment is
thus formed which is visibly precipitated in any vessel where the water
remains quiet.
Public-domain text, read in full here on John Shaqi.
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