Abstract
The most important single fact about continental glaciation is that, throughout geological time, it has taken place when a major land mass was located close to a pole. North America has undergone perhaps three extensive glaciations: the Pleistocene, roughly the last 106 yr; the Precambrian, approximately 109 yr ago; and the Precambrian, approximately 2 × 109 yr ago. (The oldest of these is subject to some doubt; perhaps the evidence can be interpreted in another way, although a good alternative explanation is not known). At each of these times, North America was located close to a pole; at other times in its history, it was not. The so-called Permian glaciation of North America (about 3 × 108 yr ago) has been based on misinterpreted evidence; no glaciation is indicated, and the continent was actually (based on paleobotanical and paleomagnetic data) close to the equator.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Tanner, W. F., 1965a: Cause and development of an ice age. J. Geol., 73, 413–430.
Tanner, W. F., 1965b: Marine terraces: pre-Pleistocene? Southeastern Geol., 6, 219–222.
Author information
Authors and Affiliations
Editor information
Rights and permissions
Copyright information
© 1968 American Meteorological Society
About this chapter
Cite this chapter
Tanner, W.F. (1968). Cause and Development of an Ice Age. In: Mitchell, J.M. (eds) Causes of Climatic Change. Meteorological Monographs, vol 8. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-935704-38-6_11
Download citation
DOI: https://doi.org/10.1007/978-1-935704-38-6_11
Publisher Name: American Meteorological Society, Boston, MA
Online ISBN: 978-1-935704-38-6
eBook Packages: Springer Book Archive