New Lands Within the Arctic Circle Narrative of the Discoveries of the Austrian
New Lands Within the Arctic Circle Narrative of the Discoveries of the Austrian
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In our eReader you can find the full English version of the book. Read New Lands Within the Arctic Circle Narrative of the Discoveries of the Austrian 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 New Lands Within the Arctic Circle Narrative of the Discoveries of the Austrian
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THE Arctic Sea, in some of its features, forcibly impresses us with its resemblance to the glaciers of the Alps. In both cases, the ice presses from a region, colder and less favoured by climate, towards one warmer and more favoured. In the Alpine glaciers, the movement is from above downwards ; in the Frozen Ocean, the movement is from a higher to a lower geographical latitude. In both cases, the tongues and spurs of the masses of ice formed by the configuration of the land or by currents of t...he sea, terminate, whenever they reach an isothermal curve of altitude or latitude, the mean temperature of which suffices to dissolve them or prevent their formation. Moraines also have their equivalent in the Arctic Sea ; for it is an established fact that icebergs and ice-fields, laden with the debris and rubbish of Arctic lands, deposit these burdens round the outer edge of the Frozen Ocean, and to this process, partially at least, CHAP, iv. ] THE INNER POLAR SEA. 43 the origin of the Newfoundland Banks is ascribed.
What to read after New Lands Within the Arctic Circle Narrative of the Discoveries of the Austrian?
You can find similar books in the "Read Also" column, or choose other free books by Julius Payer to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
THE Arctic Sea, in some of its features, forcibly impresses us with its resemblance to the glaciers of the Alps. In both cases, the ice presses from a region, colder and less favoured by climate, towards one warmer and more favoured. In the Alpine glaciers, the movement is from above downwards ; in the Frozen Ocean, the movement is from a higher to a lower geographical latitude. In both cases, the tongues and spurs of the masses of ice formed by the configuration of the land or by currents of t...he sea, terminate, whenever they reach an isothermal curve of altitude or latitude, the mean temperature of which suffices to dissolve them or prevent their formation. Moraines also have their equivalent in the Arctic Sea ; for it is an established fact that icebergs and ice-fields, laden with the debris and rubbish of Arctic lands, deposit these burdens round the outer edge of the Frozen Ocean, and to this process, partially at least, CHAP, iv. ] THE INNER POLAR SEA. 43 the origin of the Newfoundland Banks is ascribed.
What to read after New Lands Within the Arctic Circle Narrative of the Discoveries of the Austrian?
You can find similar books in the "Read Also" column, or choose other free books by Julius Payer to read onlineMoreLess
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