The Mountain
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In our eReader you can find the full English version of the book. Read The Mountain 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 Mountain
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These northern and southern zones of constant precipi- tation extend to the arctic and antarctic circles. There are rainless districts in all these zones ; stretching around the earth in different latitudes, they are generally, however, within or near the tropics. Within these zones of precipi- tation there are, as suggested in the quotations from John- ston's Physical Atlas, various causes for irregular distribu- tion of the quantities of rain in different parts of the earth's surface.
On this... subject, Schouw, of the University of Copen- hagen, has the following remarks : "Another principal cause of the increased quantity of rain, lies in the inequalities of the earth's surface. Mountains increase the * Johnston's Map is VERT far from correct for the American continent.
RAIN. 453 amount of rain; it increases in proportion as we approach toward them, and the higher and steeper they are. The reason is obvious here also: the strata of air over the mountains are colder than those over plains, and a constant reaction takes place between these differ- ent strata.
What to read after The Mountain?
You can find similar books in the "Read Also" column, or choose other free books by Robert Montgomery Smith Jackson to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
These northern and southern zones of constant precipi- tation extend to the arctic and antarctic circles. There are rainless districts in all these zones ; stretching around the earth in different latitudes, they are generally, however, within or near the tropics. Within these zones of precipi- tation there are, as suggested in the quotations from John- ston's Physical Atlas, various causes for irregular distribu- tion of the quantities of rain in different parts of the earth's surface.
On this... subject, Schouw, of the University of Copen- hagen, has the following remarks : "Another principal cause of the increased quantity of rain, lies in the inequalities of the earth's surface. Mountains increase the * Johnston's Map is VERT far from correct for the American continent.
RAIN. 453 amount of rain; it increases in proportion as we approach toward them, and the higher and steeper they are. The reason is obvious here also: the strata of air over the mountains are colder than those over plains, and a constant reaction takes place between these differ- ent strata.
What to read after The Mountain?
You can find similar books in the "Read Also" column, or choose other free books by Robert Montgomery Smith Jackson to read onlineMoreLess
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