Part 1 (2/2)

VIEW ON KOKSOAK RIVER.]

The extreme rise and fall of the tide at the mouth of the river is 62 feet 3 inches. The usual rise and fall is from 8 to 12 feet less, depending on the stage of the river. At Fort Chimo the tide rises as much as 31 feet. The backwater is held in check as far as the upper rapids in a common stage of water, and during a high rise in the month of June the water is ”backed” some 3 miles beyond the upper rapids.

The branches of the Koksoak river are few and unimportant. The larger tributary is the Larch river. It is a rapid and almost unnavigable stream of variable depth, mostly shallow, and 100 to nearly 400 yards wide.

At about 40 miles from its mouth the Larch forks, the lower or southwest fork draining the eastern sides of the same mountains whose western slopes are drained by the Little Whale river. This southwest fork of the Larch river is quite small and scarcely capable of being ascended, although it may, with great caution, be descended. This is the course followed by the Little Whale river Indians when they traverse the country to join the Naskopies of the Koksoak valley. The northwest branch of the Larch is still smaller and is reported to issue from the swampy tract of land in about lat.i.tude 58 30'.

The next large river is the Leaf. Its mouth is about 34 miles northwest of Fort Chimo, and it flows into a peculiarly shaped bay named Ta.s.s'iyak, or ”like a lake.” The length of the river proper is estimated to be but 40 miles, flowing from a very long and narrow lake, having its longer axis extending southwestward and draining the greater part of the swampy tract lying in lat.i.tude 58 30'. The southwestern portion of this tract is merely an area covered with innumerable small lakes so intimately connected by short water courses that it is difficult to determine whether water or land const.i.tutes the greater part of the area. The rivers to the west are of less importance and drain the rugged area forming the northwestern portion of the district, or that part lying under the western third of Hudson strait.

The princ.i.p.al portion of Hudson strait that came under my observation is Ungava bay. This bay is a pocket-shaped body of water lying south of the strait and toward its eastern end. Soundings in various portions of this bay indicate a depth of 28 to 70 fathoms for the central area. The bottom appears to be uniformly the was.h.i.+ngs from the freshwater streams.

The extreme tides of Hudson strait tend to produce the most violent currents in this bay. Opposite the entrance of Leaf river bay is a whirlpool of considerable size, which causes much trouble to navigation.

It is safe enough at high water but very dangerous at half-tide.

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 sh.o.r.e 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 quant.i.ty 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.

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 lat.i.tude 57.

Here the conifers are stunted and straggling. Beyond the coast range they attain a slightly higher alt.i.tude 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 sh.o.r.e. 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 sh.o.r.e 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.

South of the line given as the northern limit of trees the growth slowly attains greater size and extension of area. The timber north of the Height of Land is comparatively small, the spruce and larch rarely attaining a size greater than 12 to 15 inches at the ground and rapidly tapering up for 2 feet or so above the surface. Above the height of 2 feet the stems slowly taper and, in a few instances, produce symmetrical stems for more than 15 feet. The trees growing within 40 miles of Fort Chimo seldom exceed 10 inches in diameter, and of the larger trunks the logs are selected to form the material from which the walls of all the buildings at that place are constructed.

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