File:EGS MOI Fig S 02.jpg
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Summary
| description | {{|1=Generalized reconstructions of the positions of the main continents from the late Neoproterozoic to late Silurian times (from Open University, 2003). The configuration of Laurentia, Baltica and Gondwana depicted here in S.2a remained stable throughout the Neoproterozoic from the formation of the supercontinent Rodinia to the rifting at c.600 Ma which led to the formation of the Iapetus Ocean. From: Fig. S.2. Strachan, Rob et al. Editors. 2010. A geological excursion guide to the Moine geology of the Northern Highlands of Scotland. Edinburgh: Geological Society of Edinburgh and Geological Society of Glasgow}} |
| source | Edinburgh Geological Society |
| author | Edinburgh Geological Society |
Licencing
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| This image is Copyright Edinburgh Geological Society. The images may be reproduced free of charge for any non-commercial use in any format or medium provided they are reproduced accurately and not used in a misleading or derogatory context. Where any images on this site are being republished or copied to others, the source of the material must be identified and the copyright status acknowledged. For all other uses of the images please contact the Edinburgh Geological Society. publications@edinburghgeolsoc.org |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 18:48, 21 December 2017 | | 1,801 × 1,999 (1.14 MB) | Scotfot (talk | contribs) | User created page with UploadWizard |
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