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Cause and Development of an Ice Age

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Causes of Climatic Change

Part of the book series: Meteorological Monographs ((METEOR,volume 8))

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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.

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References

  • Tanner, W. F., 1965a: Cause and development of an ice age. J. Geol., 73, 413–430.

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  • Tanner, W. F., 1965b: Marine terraces: pre-Pleistocene? Southeastern Geol., 6, 219–222.

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J. Murray Mitchell Jr.

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© 1968 American Meteorological Society

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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

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  • 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

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