The Hudsons Bay And Pacific Territories a Lecture
The Hudsons Bay And Pacific Territories a Lecture
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In our eReader you can find the full English version of the book. Read The Hudsons Bay And Pacific Territories a Lecture Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Hudsons Bay And Pacific Territories a Lecture
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Generally all the lines of temperature for the winter, curve far northward as they approach the Pacific, though they fall southward at the meridian of the west end of Lake Superior. The winter climate of the whole country west of the 100th meridian is remark- able, and inexplicably mild to one who has not studied the relation of continental climates to those of the adjacent seas. By the explanation this position affords, however, much of the case is made plain. The winds of the temperate lati- ...tudes are steadily from the west, and they bathe the western coasts in milder air, derived from the adjacent sea. In this manner, Ireland, England, the west of Norway and Germany, are far milder than the interior of Eussia in the same latitudes. At Moscow it is very cold in winter, while on the British coasts snow scarcely falls. It is pre- cisely so on the American continent. Quebec and Canada and the mountainous portion of New England represent the cold side, while "Washington Territory, British Columbia, and Vancouver's Island represent the west of Europe.
What to read after The Hudsons Bay And Pacific Territories a Lecture?
You can find similar books in the "Read Also" column, or choose other free books by Morris Alexander to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Generally all the lines of temperature for the winter, curve far northward as they approach the Pacific, though they fall southward at the meridian of the west end of Lake Superior. The winter climate of the whole country west of the 100th meridian is remark- able, and inexplicably mild to one who has not studied the relation of continental climates to those of the adjacent seas. By the explanation this position affords, however, much of the case is made plain. The winds of the temperate lati- ...tudes are steadily from the west, and they bathe the western coasts in milder air, derived from the adjacent sea. In this manner, Ireland, England, the west of Norway and Germany, are far milder than the interior of Eussia in the same latitudes. At Moscow it is very cold in winter, while on the British coasts snow scarcely falls. It is pre- cisely so on the American continent. Quebec and Canada and the mountainous portion of New England represent the cold side, while "Washington Territory, British Columbia, and Vancouver's Island represent the west of Europe.
What to read after The Hudsons Bay And Pacific Territories a Lecture?
You can find similar books in the "Read Also" column, or choose other free books by Morris Alexander to read onlineMoreLess
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