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
Having failed to enter Ashe’s Inlet on the inward voyage, we crossed
the straits to Stupart’s Bay, in Prince of Wales’ Sound. Our visit to
this station was too brief to allow me to make any fresh geological
explorations in the neighborhood. The geology and scenery of this
locality are described in my report of last year. The accompanying
engraving, from a photograph, represents a view of the country from
Eskimo Inlet, about two miles south of Stupart’s Bay, looking westward,
and it may be taken as a characteristic specimen of the scenery on
the south side of Hudson’s Straits. I found that Mr. Stupart and his
associates had collected numerous geological specimens for me. They
consisted of gneiss, soapstone, quartz, felspar, hornblende, mica-rock,
epidote and iron pyrites, all apparently derived from ordinary
Laurentian rocks, which prevail everywhere in this region.
While at Port de Boucherville, on the south end of Nottingham Island,
some further exploration was made in the vicinity, but nothing worthy
of remark, was observed.
[Sidenote: Niagara formation.]
Last year Mansfield Island was found to consist of flat-lying, grey
limestones. The fossils then collected, on its eastern side, although
badly preserved and not numerous, indicate the age of our Niagara
formation.
[Sidenote: Southampton Island.]
[Sidenote: Gneiss.]
Similar limestones prevail on Southampton Island (proper) from Cape
Southampton to within twenty-five or thirty miles of Cape Pembroke
at its north-eastern extremity, the latter interval being occupied,
according to Captain William Hawes, of the Hudson’s Bay Company, by
rugged, dark-looking rocks, like those of Hudson’s Strait, which are
Laurentian gneiss. The large island north of Southampton Island, of
which Seahorse Point forms the eastern extremity, and which Lieutenant
Gordon has called Bell’s Island, in the absence of any other name, is
mountainous and appears to consist of gneiss.
[Illustration: British American Bank Note Co. Montreal
VIEW WESTWARD IN PRINCE OF WALES SOUND, HUDSON’S STRAIT.
SHOWING OUTLINE OF MOUNTAINS IN THIS REGION. ESKIMO TENTS IN
FOREGROUND.]
[Sidenote: Track-survey of Outer Digges.]
[Sidenote: Glaciation.]
Public-domain text, read in full here on John Shaqi.
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