“Of course it is generally understood that the winter climate of the country round the bay is usually very severe. The lowest temperature I have experienced there, however, was 39° below zero on Nov. 29, 1906, with a strong wind blowing from the bay, which intensified the cold. It is exceedingly rare to have winds off the bay in the winter months. In winter the wind is generally from the west and northwest, while in summer it is generally from the east and northeast. I have always found the thermometer lower one hundred and fifty miles inland. It can never be called dark in the north, even in the depth of winter.”


[14] It will be observed that part of this evidence treats of other districts than the one immediately under consideration; but it cannot conveniently be eliminated here without awkwardly dislocating Mr. Tyrrell’s evidence.—(E. J. C.).

CHAPTER III.

THE KEEWATIN AREA.

(Newest Ontario and Northern Manitoba.)

Tree Growth and Timber Resources.

Considerable Areas of Good Timber.—The Range of the More Important Trees.—The Banskian Pine.—Forests of Trees in Many Places that Would Make Good Logs, and Much Pulp Wood.—Occasional Beautiful Forests of Aspen Poplar.—Magnificent Coniferous Forest Northwest of Lake Winnipeg.—Water Power on the Nelson.—Destruction Wrought by Forest Fires.—Ample Supply of Timber For Fuel.

There is considerable evidence showing that there are, in different sections of the territory immediately west and south of Hudson bay, considerable areas of useful timber.