Climatic Changes Their Nature And Causes
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C. -300 A. D. 300 A. D. - Brooks bases his chronology largely on De Geer's measurements of the annual layers of clay in lake i C. E. P. Brooks : The Evolution of Climate in Northwest Europe. Quart. Jour. Koyal Meteorol. Soc. , Vol. 47, 1921, pp. 173-194.
216 CLIMATIC CHANGES bottoms but makes much use of other evidence. Accord- ing to Brooks the last glacial epoch lasted roughly from 30, 000 to 18, 000 B. C. , but this includes a slight ameliora- tion of climate followed by a readvance of the i...ce, known as the Buhl stage. During the time of maximum glacia- tion the British Isles stood twenty or thirty feet higher than now and Scandinavia was "considerably" more elevated. The author believes that this caused a fall of 1C. In the temperature of the British Isles and of 2C. In Scandinavia. By an ingenious though not wholly con- vincing method of calculation he concludes that this lowering of temperature, aided by an increase in the area of the lands, sufficed to start an ice sheet in Scandinavia.
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To quickly assess the difficulty of the text, read a short excerpt:
C. -300 A. D. 300 A. D. - Brooks bases his chronology largely on De Geer's measurements of the annual layers of clay in lake i C. E. P. Brooks : The Evolution of Climate in Northwest Europe. Quart. Jour. Koyal Meteorol. Soc. , Vol. 47, 1921, pp. 173-194.
216 CLIMATIC CHANGES bottoms but makes much use of other evidence. Accord- ing to Brooks the last glacial epoch lasted roughly from 30, 000 to 18, 000 B. C. , but this includes a slight ameliora- tion of climate followed by a readvance of the i...ce, known as the Buhl stage. During the time of maximum glacia- tion the British Isles stood twenty or thirty feet higher than now and Scandinavia was "considerably" more elevated. The author believes that this caused a fall of 1C. In the temperature of the British Isles and of 2C. In Scandinavia. By an ingenious though not wholly con- vincing method of calculation he concludes that this lowering of temperature, aided by an increase in the area of the lands, sufficed to start an ice sheet in Scandinavia.
What to read after Climatic Changes Their Nature And Causes?
You can find similar books in the "Read Also" column, or choose other free books by Huntington Ellsworth to read onlineMoreLess
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