Canada and the British immigrantWeaver, Emily P. (Emily Poynton)
History
Canada and the British immigrant
Weaver, Emily P. (Emily Poynton)
Canada -- Description and travel; Canada -- Economic conditions
It comprises the greater part of “the second prairie steppe,” which has
an average elevation of about fifteen hundred feet above sea-level, but
Lake Athabasca, thrusting itself into its extreme north-west, is less
than seven hundred feet above the sea, and the highest summit of the
Cypress hills is over four thousand two hundred feet. Thus this “prairie
province” is by no means all a level plain. In fact, it possesses such
differences of surface that it has been said that it may be divided into
“four well-defined zones.” In the south (with the exception of some
hilly districts) and extending to Saskatoon is the rolling prairie. Next
comes a belt of mingled prairie and woodlands, dotted with small lakes,
and often described as park-like. Then, about Prince Albert, begins the
great northern forest of “spruce, tamarac, jack-pine, poplar and birch.”
This timbered belt crosses the province, and is between three and four
hundred miles wide. North of it is the fourth zone, only sparsely
wooded.
The province is situated in the very heart of the Dominion, but it is
watered by several great rivers, which have cut their way deep into the
plains. One of these, the Saskatchewan or “Rushing Water,” as the
Indians called it—has given its name to the province in which its two
branches, the North and the South Saskatchewan, unite to flow together
into Lake Winnipeg and thence to Hudson Bay. Farther north the mightiest
river is the Churchill, one thousand miles long, which by many a
tumultuous rapid hurries to the same inland sea.
For a long time Saskatchewan had a bad reputation so far as climate is
concerned, and if any British immigrant comes to settle in the country
without understanding that the winters are very much colder than those
he has been accustomed to, he will probably be much disappointed and may
feel himself ill-used, though the chances are that he ought to have made
more particular inquiries before he came. The disadvantages of the
climate are a low winter temperature (for ten years the _average_
temperature of the coldest months, January and February, shows from 27
to 29 degrees of frost); an occasional severe snowstorm or “blizzard,”
and some dry windy weather at other seasons of the year, when the
blowing of the dust is very trying.
The advantages, often held by residents in Saskatchewan of more than two
or three years’ standing to outweigh the disadvantages, are the clear
exhilarating atmosphere, the light snowfall, the bright sunshine at all
seasons, the cool, pleasant nights of summer, and the infrequence of
rain or thaws during winter. Usually the cold weather does not reach its
greatest severity till after Christmas, and winter may be said to end
late in March. The sowing of the crops occasionally begins in March, but
generally not until April.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account