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 higher hills retain snow until the last of August, but none is to be
seen in the vicinity of Fort Chimo after that date. By the middle of
September snow again covers the tops of the distant high hills.
Fogs rarely occur so far inland as Fort Chimo. Those occurring are in
July and August. At times they are very dense; and, as they form during
the earliest hours of the day, they are usually dissipated by 4 to 7
a. m. While the ice is setting in the river, and driven back and forth
by the tides, huge volumes of steam arise from the inky water and are
spread over the land by the light winds prevailing at that season. This
moisture deposited on the bushes and trees forms a most beautiful sight.
AURORAS.
Auroras may be seen on most of the clear nights of the year. The month
of June is, on account of its light nights, the only month in which an
aurora is not observable.
VEGETATION.
The northern limit of trees on the Labrador coast is in latitude 57°.
Here the conifers are stunted and straggling. Beyond the coast range
they attain a slightly higher altitude and thence continue to a point
about thirty miles north of the mouth of George’s river. On the western
side of the mouth of this river the trees are pushed back 15 to 20 miles
from the sea. At the mouth of Whale river, the trees attain a height of
30 to 50 feet on the eastern (right) bank and within 2 miles of the
shore. On the left bank the trees do not approach to within 10 to 15
miles of the coast. At the mouth of False river they form a triangular
extension and attain considerable size, due in great measure to the
peculiar formation of a huge amphitheater whose north wall serves as an
admirable protection against the cold winds from the bay. On the western
side of False river the tree line extends in a southwesterly direction
across the Koksoak and to the banks of the Leaf river nearly at its
source from the large lake. From the south side of this lake the trees
are very much scattered and attain inconsiderable size, scarcely fitted
for other uses than fuel.
A line from this lake southwest to the eastern shore of Hudson bay forms
the northern limit of trees for the northwest portion of the region. The
people (Eskimo only) who dwell north of this line are dependent upon the
stunted willows and alders, growing in the deeper ravines and valleys
having a southern exposure. Large pieces of wood are much sought for by
the Eskimo of the northwest portion, for use in constructing their
kaiaks, umiaks and paddles, as well as spear shafts and smaller
requirements for which the distorted stems of willow and alder will not
suffice.
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