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| Titel: | |
| Auteur: | |
| Verschenen in: |
Annals of science |
| Paginering: | Jaargang 39 (1982) nr. 6 pagina's 565-583 |
| Jaar: |
1982-11 |
| Inhoud: |
James Geikie's Great Ice Age (1874) first presented to the geological public the Pleistocene. modern interpretation of alternating mild and cold periods during the Though it was supported by geological evidence, Geikie's view of the Ice Age was based on a theoretical framework supplied by the climatic physics of James Croll. Mid-nineteenth-century British geologists had encountered great difficulty in making sense out of the varied and complicated glacial deposits, or 'drift', and had formulated the 'iceberg' theory to account for the apparent chaos of the drift, an explanation which discouraged its stratigraphic study. The reaffirmation of faith in continental glaciation by several Scottish geologists in the 1850s brought with it a belief in an eventful Pleistocene, but it remained difficult to discover the events of Ice Age history from study of the glacial deposits. In 1864 Croll presented a detailed climatic history of the Ice Age deduced from astronomy and physical geography. By 1871 James Geikie was using Croll's scheme of Ice Age history as the basis for his impressive synthesis of Pleistocene data from throughout the world. |
| Uitgever: |
Taylor & Francis |
| Bronbestand: |
Elektronische Wetenschappelijke Tijdschriften |
Details van artikel 5 van 5 gevonden artikelen
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