FREE BOOKS

Author's List




PREV.   NEXT  
|<   97   98   99   100   101   102   103   104   105   106   107   108   109   110   111   112   113   114   115   116   117   118   119   120   121  
122   123   124   125   126   127   128   129   130   131   132   133   134   135   136   137   138   139   140   141   142   143   144   145   146   >>   >|  
the north in the Peace river valley. Though the climate of the plains is one of extremes and often of rather sudden changes, it is brisk and invigorating and of particular value for persons affected with lung troubles. The climate of the Cordilleran region presents even more variety than that of the other provinces because of the ranges of mountains which run parallel to the Pacific. Along the coast itself the climate is insular, with little frost in winter and mild heat in summer, and with a very heavy rainfall amounting to 100 in. on the south-west side of Vancouver Island and near Port Simpson. Within 100 m. inland beyond the Coast Range the precipitation and general climate are, like those of Ontario, comparatively mild and with moderate snowfall towards the south, but with keen winters farther north. The interior plateau may be described as arid, so that irrigation is required if crops are to be raised. The Selkirk Mountains have a heavy rainfall and a tremendous snowfall on their western flanks, but very much less precipitation on their eastern side. The Rocky Mountains have the same relationships but the whole precipitation is much less than in the Selkirks. The temperature depends largely, of course, on altitude, so that one may quickly pass from perpetual snow above 8000 ft. in the mountains to the mild, moist climate of Vancouver or Victoria, which is like that of Devonshire. In the far north of the territories of Yukon, Mackenzie and Ungava the climate has been little studied, as the region is uninhabited by white men except at a few fur-trading posts. North-west and north-east of Hudson Bay it becomes too severe for the growth of trees as seen on the "barren grounds," and there may be perpetual ice beneath the coating of moss which serves as a non-conducting covering for the "tundras." There is, however, so little precipitation that snow does not accumulate on the surface to form glaciers, the summer's sun having warmth enough to thaw what falls in the winter. Leaving out the maritime provinces, southern Ontario, southern Alberta and the Pacific coast region on the one hand, and the Arctic north, particularly near Hudson Bay, on the other, Canada has snowy and severe winters, a very short spring with a sudden rise of temperature, short warm summers, and a delightful autumn with its "Indian summer." There is much sunshine, and the atmosphere is bracing and exhilarating. _Flora_.--The general flora of the
PREV.   NEXT  
|<   97   98   99   100   101   102   103   104   105   106   107   108   109   110   111   112   113   114   115   116   117   118   119   120   121  
122   123   124   125   126   127   128   129   130   131   132   133   134   135   136   137   138   139   140   141   142   143   144   145   146   >>   >|  



Top keywords:
climate
 

precipitation

 

summer

 
region
 

Hudson

 

rainfall

 
southern
 

severe

 

Vancouver

 
temperature

winters

 

Mountains

 

perpetual

 
snowfall
 
general
 

Ontario

 

winter

 

Pacific

 
sudden
 

provinces


mountains

 

barren

 

growth

 

Though

 

grounds

 

conducting

 

covering

 

tundras

 

serves

 

beneath


coating

 

uninhabited

 
studied
 

Ungava

 

valley

 
extremes
 

trading

 

plains

 

accumulate

 

spring


summers

 

Arctic

 
Canada
 

delightful

 

autumn

 
exhilarating
 

bracing

 
atmosphere
 
Indian
 
sunshine