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
HISTORICALLY, the Dominion of Canada was evolved from the separate
provinces; but it will be more convenient here to consider it as a whole
before giving some account of each of the nine provinces separately. In
this chapter, and generally throughout the book, when I speak of Canada,
I mean the Dominion of Canada, though the name was first applied to the
French province on the St. Lawrence, which was sometimes also called New
France. Afterwards, for three-quarters of a century, from 1791 to 1867,
the province now known as Quebec was called Lower Canada, or Canada
East; and that now known as Ontario, Upper Canada, or Canada West.
The immense area of Canada is one of its most striking features. Its
size is one of the reasons that it is a land of great opportunity; it is
also the root of many of the most difficult problems of its government
and development. In area it is over 3½ million square miles; that is to
say, it is a little larger than the United States, or than Europe would
be without France. It stretches from the Atlantic Ocean on the east to
the Pacific on the west, and from the United States boundary on the
south to the Arctic Ocean on the north. The distance from Halifax in
Nova Scotia to Vancouver in British Columbia is about 3,660 miles,
whilst that from Halifax to Liverpool is only about 2,820; and the
traveller, wishing to go from Victoria in Vancouver Island to Dawson in
the Yukon District, has to make a journey by land and water of over
1,500 miles.
It is just as well for the intending immigrant to try to realize that
Canada is a land of “magnificent distances”; otherwise, on his outward
journey, perhaps to some point in the far west, it may seem that the
distance he is putting between himself and his old home is interminable.
With modern conveniences of travel, however, the immigrant of to-day can
come from England and cross Canada to Vancouver in a shorter time than
it took the Loyalists to go from New York to Toronto.
The most southern point of Canada, a little islet in Lake Erie, is only
about the same distance from the equator as is Valladolid in Spain,
whilst Toronto is in nearly the same latitude as Florence, and the new
town of Prince Rupert, far up on the Pacific seaboard of the Dominion,
is not much farther north than Liverpool.
The vast extent of country and the variety in its physical features
cause considerable differences of climate; but generally the interior is
rather colder than the same latitudes in the west of Europe, and the
summer, though hot and dry, is shorter than in Europe. The climate in
the region near the Atlantic is colder than the countries on the
opposite side of that ocean, owing to a cold current which flows
southward along its shores from the Arctic regions; but the Pacific
Coast, which has the benefit of the warm Japanese current, has a climate
very much resembling that of the British Isles.
Public-domain text, read in full here on John Shaqi.
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