File:Cape-Breton-Diapir-Finlay-Point 038.jpg

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English: Gypsum and anhydrite cap atop the Finlay Point salt diapir near Mabou Mines, Nova Scotia. The diapir is sourced in the Windsor Group (Mississippian) and deforms the overlying coal-bearing strata of the Inverness Formation (Pennsylvanian).
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Author Michael C. Rygel
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If used outside of Wikipedia or Wikimedia Commons, please acknowledge the source of this photo (Michael C. Rygel via Wikimedia Commons) in a legible, clearly visible position near one of the corners of the image, in a figure caption, or in the acknowledgements section of the publication.
Camera location46° 08′ 07.99″ N, 61° 27′ 48.31″ W Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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current14:25, 6 January 2011Thumbnail for version as of 14:25, 6 January 20113,310 × 1,236 (2.3 MB)Rygel, M.C. (talk | contribs){{Information |Description={{en|1=Gypsum and anhydrite cap atop the Finlay Point salt diapir near Mabou Mines, Nova Scotia. The diapir is sourced in the Windsor Group (Mississippian) and de

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