The Antiquity of Man in Europe, Being the Munro Lectures, 1913
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In our eReader you can find the full English version of the book. Read The Antiquity of Man in Europe, Being the Munro Lectures, 1913 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 Antiquity of Man in Europe, Being the Munro Lectures, 1913
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Hence the motion is greater in summer than in winter, and during day than during night. Again, other things being equal, a glacier moves more rapidly on a steep than on a gentle slope ; while very thick ice-streams flow faster than glaciers of relatively insignificant dimensions.
The glaciers to which I have been referring are typically represented by those of the Alps- — the distinguishing character of which is that they have their source in deep mountain-recesses whence they make their way do...wn mountain valleys. But there are other types of ice-flow of great interest, especially from a geological point of view. These may be called ice-cap glaciers, of which excellent examples are seen in Norway. The configuration of that country differs essentially from that of the Alps. In the latter we have a complicated series of mountain- groups and crested ranges, everywhere overlooking the profound cirques and deep valleys in which glaciers are generated. Norway, on the other hand, is a lofty plateau, deeply trenched, it is true, by mountain valleys and fiords, but showing between these depressions extensive tracts with a relatively flat or undulating surface, which are often not dominated by peaks or ridges.
What to read after The Antiquity of Man in Europe, Being the Munro Lectures, 1913?
You can find similar books in the "Read Also" column, or choose other free books by Geikie, James, 1839-1915 to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Hence the motion is greater in summer than in winter, and during day than during night. Again, other things being equal, a glacier moves more rapidly on a steep than on a gentle slope ; while very thick ice-streams flow faster than glaciers of relatively insignificant dimensions.
The glaciers to which I have been referring are typically represented by those of the Alps- — the distinguishing character of which is that they have their source in deep mountain-recesses whence they make their way do...wn mountain valleys. But there are other types of ice-flow of great interest, especially from a geological point of view. These may be called ice-cap glaciers, of which excellent examples are seen in Norway. The configuration of that country differs essentially from that of the Alps. In the latter we have a complicated series of mountain- groups and crested ranges, everywhere overlooking the profound cirques and deep valleys in which glaciers are generated. Norway, on the other hand, is a lofty plateau, deeply trenched, it is true, by mountain valleys and fiords, but showing between these depressions extensive tracts with a relatively flat or undulating surface, which are often not dominated by peaks or ridges.
What to read after The Antiquity of Man in Europe, Being the Munro Lectures, 1913?
You can find similar books in the "Read Also" column, or choose other free books by Geikie, James, 1839-1915 to read onlineMoreLess
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