The Unexploited West: A Compilation of all of the authentic information available at the present time as to the Natural Resources of the Unexploited Regions of Northern CanadaChambers, Ernest J.
History
The Unexploited West: A Compilation of all of the authentic information available at the present time as to the Natural Resources of the Unexploited Regions of Northern Canada
Chambers, Ernest J.
Canada -- Economic conditions; Northwest, Canadian -- Economic conditions
Before the Senate committee of 1888, Bishop Clut stated that in Peace
river and Liard river, certainly there was gold in large quantities. On
Peace river, twelve or thirteen years prior to 1888, miners made from
fifteen dollars to twenty dollars a day washing, but in the winter and
when the water was high they could not work, and they abandoned the
mines. “If the country were settled,” the bishop remarked, “those mines
might be worked to better advantage, because the miners could find other
occupation in the winter and when the water was high.”
According to Mr. von Hamerstein, at Black bay, on Lake Athabaska, there
is first-class galena—none better. It carries gold, silver and copper.
They assayed some of the product at Chipewyan, and found that it carried
roughly about six dollars or seven dollars worth of gold, and some
copper. There is a big seam near Black bay, and one can follow it up
right along until it comes to an island. That is a very fine country for
gold, and there have been several attempts to make something out of it,
but the time is not ripe.
INDICATIONS OF IRON.
Indications of the presence of iron have been found on Peace,
Clearwater, and Athabaska rivers. A specimen rock from near Pelican
rapids on Athabaska river contained 12.4% of metallic iron. J. B.
Tyrrell found indications of iron in Churchill river district, and also
north of Lake Athabaska.
According to Mr. R. G. McConnell’s 1888 report:—Clay ironstone in
nodules and thin beds, is of universal occurrence in the Cretaceous
shales of the Peace region, but is especially abundant in some of the
outcrops of the Fort St. John shales on Peace river, between Battle
river and Smoky river. The ironstone, here, owing to the rapid erosion
of the soft shales, has been silted out, and in many places forms thick
accumulations at the foot of the cliffs lining the valley, some of which
may prove to be of economic value. The Pelican sandstone on the
Athabaska is usually capped with a bed of hemitiferous sandstone varying
in thickness from a few inches to four or five feet. A specimen of the
rock was examined in the laboratory of the Geological Survey, and found
to contain 12·4 per cent. of metallic iron.
Mr. von Hamerstein, in his evidence before the Senate committee of 1907,
stated that there are indications of iron along Clearwater river. He
found some very nice pieces of iron, and he found limestone in the
centre of Athabaska.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account