Observations on the geology, zoology and botany of Hudson's Strait and Bay, made in 1885 — John Shaqi
Observations on the geology, zoology and botany of Hudson's Strait and Bay, made in 1885Bell, Robert
History
Observations on the geology, zoology and botany of Hudson's Strait and Bay, made in 1885
Bell, Robert
Natural history -- Hudson Bay Region
A specimen of similar pyrites, obtained from a place on this coast
which the Eskimo call Iñari, in 1879, had a small quantity of light
bluish-grey magnesian limestone adhering to it. These specimens, which
all resemble the pyrites from Tilt Cove in Newfoundland and Capelton in
the Eastern Townships, except in the absence of copper, are evidently
from good-sized veins. The mineral is in common use among the Eskimo
for striking fire. The discovery of traces of gold and silver in the
specimen last assayed by Mr. Hoffmann is interesting. Specks of gold
are mentioned by Tennant in a specimen of quartz from Repulse Bay.
[Sidenote: Huronian series on the N. W. side of Hudson’s Bay.]
The majority of the lithological specimens brought from the coast in
the whole interval between Eskimo Point and Repulse Bay, correspond
with the rocks of the Huronian series. Laurentian types are absent from
the collections. So far as we know, therefore, the probabilities are
that Huronian rocks prevail all along the north-west coast of Hudson’s
Bay, from Eskimo Point to Chesterfield Inlet, and again at Repulse Bay;
possibly also, in the interval between the last mentioned localities.
[Sidenote: Quartzite of Marble Island.]
[Sidenote: Quartzite on mainland.]
[Sidenote: Quartzite in the interior.]
Marble Island, as far as examined, consists mainly of light-colored,
fine grained quartzite, associated with glossy mica-schists. Among the
specimens obtained from the mainland, is one of similar quartzite of a
delicate pink or flesh-color, from a point on the south side of Nevil
Bay. On Marble Island the average strike is south-westward or in this
direction, so that the two localities may occupy the same geological
horizon. White quartzite is reported as occurring further south-west in
the interior, especially in the region to the north-east of Hatchet or
Wollaston Lake, and in my report for 1882, page 28 C C, it was stated
that boulders of this rock are abundant at the Long or Methy Portage,
still further south-west.
APPENDIX I.
LIST
BY PROFESSOR MACOUN
OF
PLANTS COLLECTED IN NEWFOUNDLAND IN 1885,
BY
DR. ROBERT BELL.
I, Brigus. II, Petty Harbour. III, St. John’s. IV, Topsail.
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