User:Geo Swan/Fundy Epieugeosyncline
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The Fundy Epieugeosyncline is geologic formation that connects Eastern New Brunswick to Western Newfoundland.[1]
References
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Bill Galine (2008-09-11). "St George's Bay Preliminary Resource Assessment" (PDF). Expedition Mining. p. 16,17,18. Archived (PDF) from the original on 2014-09-10. Retrieved 2014-09-09.
The greatest thickness of Mississippian sediments within eastern Canada lies in the Fundy Epieugeosyncline.