History of Science, a — Volume 3 by Henry Smith Williams;Edward Huntington Williams
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page 4 of 354 (01%)
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earth--His belief in volcanic cataclysms in raising and forming
the continents--His famous paper before the Royal Society of Edinburgh, 1781---His conclusions that all strata of the earth have their origin at the bottom of the sea---His deduction that heated and expanded matter caused the elevation of land above the sea-level--Indifference at first shown this remarkable paper--Neptunists versus Plutonists-- Scrope's classical work on volcanoes--Final acceptance of Hutton's explanation of the origin of granites--Lyell and uniformitarianism--Observations on the gradual elevation of the coast-lines of Sweden and Patagonia--Observations on the enormous amount of land erosion constantly taking place, --Agassiz and the glacial theory--Perraudin the chamois- hunter, and his explanation of perched bowlders--De Charpentier's acceptance of Perraudin's explanation--Agassiz's paper on his Alpine studies--His conclusion that the Alps were once covered with an ice-sheet--Final acceptance of the glacial theory--The geological ages--The work of Murchison and Sedgwick--Formation of the American continents--Past, present, and future. CHAPTER V. THE NEW SCIENCE OF METEOROLOGY Biot's investigations of meteors--The observations of Brandes and Benzenberg on the velocity of falling stars-- Professor Olmstead's observations on the meteoric shower of 1833- -Confirmation of Chladni's hypothesis of 1794--The aurora borealis--Franklin's suggestion that it is of electrical origin--Its close association with terrestrial magnetism--Evaporation, cloud-formation, and dew--Dalton's |
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