Hostname: page-component-586b7cd67f-dlnhk Total loading time: 0 Render date: 2024-11-29T14:59:50.044Z Has data issue: false hasContentIssue false
  • English
  • Français

The Probable Solution of the Climate Problem in Geology

Published online by Cambridge University Press:  01 May 2009

Wilhelm Ramsay
Wilhelm Ramsay
Affiliation:
Professor of Geology and Mineralogy at the University of Helsingfors, Finland.
Get access Rights & Permissions [Opens in a new window]

Extract

In the following pages I have endeavoured to give an interpretation, not only of the appearance of ice ages, but also of the greater changes of climate registered in the geological record. In view of the importance ascribed in this discussion to relief, I have named the theory the relief hypothesis.

Type
Original Articles
Information
Geological Magazine , Volume 61 , Issue 4 , April 1924 , pp. 152 - 163
Copyright
Copyright © Cambridge University Press 1924

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 152 note 1 Ramsay, Wilhelm, “Die Reliefhypothese zur Erklärung der Klimaechwankungen”: Petermanns Mitteilungen, 1911, p. 335.Google Scholar

page 154 note 1 Nansen, Fridtjof, “The Strandflat and Isostasy”: Videnskabsselskabeta Skrifler: I. Mat.-naturv. Klasse, 1921, No. 11, Kristiania, p. 305.Google Scholar

page 155 note 1 Ramsay, Wilhelm, “Orogenesis und Klima”: Öfversigt af Finska Vetenskaps-Societetens Förhandlingar, Helsingfors, lii, 1910, Afd. A, No. 11.Google Scholar

page 156 note 1 Bacqué, Edgar, Grundlagen und Methoden der Paleogeographie, Jena, 1916.Google Scholar

page 158 note 1 Tylor, Alfred, “Evidence and Cause of great changes of the Sea-level during the Glacial Period”: Geol. Mag., Vol. V, 1868, p. 576.Google Scholar

page 158 note 2 Loc. cit., pp. 229–38.

page 160 note 1 Paschinger, V., “Die Eiszeit ein meteorologischer Zyklus”: Zeitschrift für Gletscherkunde, xiii, Leipzig, 1923, pp. 29–65.Google Scholar

page 160 note 2 Upham, Warren, Probable Causes of Glaciation.Google Scholar In Wright, G. F., The Ice Age in North America, London, 1890, Appendix, pp. 573–95.Google Scholar “Pleistocene Climatic Changes”: Geol. Mag., 1894, pp. 340–9.Google Scholar

page 160 note 3 Jamieson, T. F., “On the History of last Geological Changes in Scotland”: Quart. Journ. Geol. Soc., xxi, London, 1865.Google Scholar “On the Causes of Depression and Re-elevation of Land during the Glacial Period”: Geol. Mag., 1882, pp. 400–7 and 457–66.Google Scholar “On some Changes of Level during the Glacial Period and their causes”: Geol. Mag., 1887, pp. 344–9.Google Scholar

page 160 note 4 Salisbury, R. D., Editorial Note: Journal of Geology, ii, Chicago, 1894, pp. 222–4.Google Scholar

page 161 note 1 De Geer, Gerard, “A Geochronology of the last 12,000 years”: Compte rendu du XI Congrès Geologique Internationale, Stockholm, 1910, pp. 241–53.Google Scholar “A Thermographical Record of the late-Quaternary Climate”: Die Veränderungen des Klimas seit dem Maximum der letzten Eiszeit (Congrès Géol. Intern., 1910), Stockholm, 1910, pp. 303–10.Google Scholar

page 161 note 2 Sauramo, Matti, “Studies on the Quaternary Varve Sediments in Southern Finland”: Bulletin de la Commission Géologique de Finlande, No. 60, Helsingfors, 1923.Google Scholar

page 162 note 1 Loc. oit., pp. 286–7.

page 163 note 1 Marr, , Geology of the Lake District, p. 37 and fig. 7.Google Scholar

page 163 note 2 A calcareous ash with fossils, “ The Style End Grassing Beds,” was discovered years ago by Professors Harkness and Nicholson in the eastern part of the Lake District. It was also recognized by them near Millom (Quart. Journ. Geol. Soc., vol. xxxiii, 1877, p. 461).Google Scholar