Ethnology of the Ungava District, Hudson Bay Territory: Eleventh Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1889-1890, Government Printing Office, Washington, 1894, pages 159-350Turner, Lucien M. (Lucien McShan)
History
Ethnology of the Ungava District, Hudson Bay Territory: Eleventh Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1889-1890, Government Printing Office, Washington, 1894, pages 159-350
Turner, Lucien M. (Lucien McShan)
Indians of North America -- Québec (Province) -- Ungava Peninsula -- Folklore; Indians of North America -- Québec (Province) -- Ungava Peninsula -- Social life and customs; Inuit -- Québec (Province) -- Ungava Peninsula -- Folklore; Inuit -- Québec (Province) -- Ungava Peninsula -- Social life and c
The large island known as Akpatok lies in such a position as to break
much of the current along the south side of the middle of the strait,
but to give additional force to the currents at either end. This island
is about 100 miles long and has an average width of 18 miles. It is the
largest island in the strait proper.
The coast line of the northwest portion of the mainland is imperfectly
known, as is the western coast forming the eastern shore of Hudson bay.
Navigation in any portion of Hudson strait is attended with much danger,
not alone from the tremendous energy of the tides but also from the
quantity of ice to be found at all times. During the months of August
and September the strait is comparatively free from large fields of ice,
but after that date the harbors, coves, and other anchorages are apt to
be frozen up in a single night.
CLIMATE.
The temperature is controlled by the direction of the wind. The warmest
winds are southeast, south, and southwest during the summer. The
northeast winds bring (if backing) fog, rain, or snow; the north wind is
usually cold and disposed to disperse the clouds. The northwest wind is
always very cold in winter and chilly in summer. Westerly winds are
moderate in winter and summer. The southerly winds are warm at all
seasons if blowing hard, but very cold if blowing lightly in winter.
I think the coldest light winds of the winter are from a point little
west of south. They are doubtless due to the cold from the elevated
region--the Height of Land.
The greatest amount of cloudiness occurs in the spring and fall; rather
less in July and August, and least during December, January, and
February. The average cloudiness for the entire year is not less than
eighty-two hundredths of the visible sky.
Sleet falls mostly from the middle of September to the beginning of
December. Snow then succeeds it and continues to be the only form of
precipitation until the middle of April, when sleet and snow fall until
the first rain sets in. The season of rain is very erratic. It may rain
by the first of May, but rarely does. Snow falls every month in the
year; the 2d of July and the 6th of August were the dates farthest apart
for this form of precipitation. The character of the rain is usually
moderate to hard for the summer showers; although several notable
exceptions of abundant dashes occur during late June and all of July.
The August and September rains are usually light to moderate, but often
persistent for several days. The snowfalls are light to heavy in
character, rarely, however, lasting more than twenty-four hours. The
sleet is usually precipitated in severe squalls. The lower grounds are
permanently covered with snow by the 1st of December, this covering
remaining until the 10th of June. At the latter date only the heavier
drifts and the snow of the ravines remain. It entirely disappears by the
last of July at all elevations no higher than that of Fort Chimo.
Public-domain text, read in full here on John Shaqi.
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