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Caledonian orogeny |
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Caledonian orogeny [¦kal·ə¦dōn·ē·ən ȯ′räj·ə·nē] (geology) Deformation of the crust of the earth by a series of diastrophic movements beginning perhaps in Early Ordovician and continuing through Silurian, extending from Great Britain through Scandinavia. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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