The North-West Passage by land: Being the narrative of an expedition from the Atlantic to the Pacific, undertaken with the view of exploring a route across the continent to British Columbia through British territory, by one of the northern passes in the Rocky MountainsMilton, William Fitzwilliam, Viscount
History
The North-West Passage by land: Being the narrative of an expedition from the Atlantic to the Pacific, undertaken with the view of exploring a route across the continent to British Columbia through British territory, by one of the northern passes in the Rocky Mountains
Milton, William Fitzwilliam, Viscount
British Columbia -- Description and travel; Northwest, Canadian -- Description and travel
characteristic of the district. Similar terraces were noticed by Dr.
Hector on the Athabasca, Kootanie, and Columbia Rivers, and they have
been also observed on some rivers in California and Mexico; but in none
of these instances do they appear comparable in extent and regularity
with those of the Thompson and Fraser. It is worthy of remark that in
nearly every instance where these terraces have been found, in various
countries, they occur in _three_ successive tiers, as in these of
British Columbia; which would seem to mark as many separate epochs when
important geological disturbances took place.
[Illustration: THE TERRACES ON THE FRASER RIVER.
(_See page 338._)
]
Gold is found in all these benches on the Fraser in the state of the
finest “flour gold,” but not in sufficient quantities to satisfy the
miner when the richer diggings of Cariboo outrun all competition. There
seems to be some unexplained connection between these terraces and
the celebrated “bunch-grass,” for where the terraces commence on the
north, the bunch-grass is also first found, and both end together above
Yale. The rolling country between the two rivers is indeed clothed with
this grass, but it does not extend beyond the northern limit of the
terraces. In the valley of the Columbia, to the south-west, it grows
with great luxuriance, and here again the curious terraces are found.
The probable explanation of this circumstance is that the peculiar kind
of soil formed by the disintegration of the limestone, or soft volcanic
rocks, found in this district, is necessary to the growth of this
peculiar grass.
Soon after we again reached the Thompson, we came to a place where a
portion of the road was not yet made, and led our horses over high
rocky bluffs, which at first sight appeared completely to bar all
passage. The trail was a mere ledge of rock of a few inches in width,
and conquered the precipitous ascent by a succession of windings and
zig-zags. The path was so narrow that it was quite impossible for
horses to pass one another, and as the river rushes hundreds of feet
immediately below, and even a slip would be certainly fatal, it is
necessary to ascertain that the road is clear before venturing over the
dangerous precipices.
Public-domain text, read in full here on John Shaqi.
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