File:Serpentinite (Thetford Mines Ophiolite Complex, Ordovician; Thetford Mines area, Quebec, Canada) (14819946774).jpg

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Serpentinite (10.0 cm across) from Quebec’s Thetford Mines Ophiolite Complex, representing ancient oceanic lithospheric peridotite that was metamorphosed during the Taconic Orogeny (Ordovician).

Locality: Thetford Mines area, southeastern Mégantic County, southern Quebec, Chaudiere Appalachians, south of the St. Lawrence River, southeastern Canada.


Ophiolites are fragments of oceanic lithosphere (basaltic crust + uppermost mantle) that have been metamorphosed and plastered onto the edges of continental lithospheric plates by obduction (the opposite of subduction).
Date
Source Serpentinite (Thetford Mines Ophiolite Complex, Ordovician; Thetford Mines area, Quebec, Canada)
Author James St. John

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This file is licensed under the Creative Commons Attribution 2.0 Generic license.
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/14819946774 (archive). It was reviewed on 30 November 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

30 November 2019

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Date/TimeThumbnailDimensionsUserComment
current17:07, 30 November 2019Thumbnail for version as of 17:07, 30 November 20191,417 × 1,057 (1.15 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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