File:Folded gneiss, old path to Reinigeadal, Harris - geograph.org.uk - 108339.jpg

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Folded_gneiss,_old_path_to_Reinigeadal,_Harris_-_geograph.org.uk_-_108339.jpg(640 × 427 pixels, file size: 289 KB, MIME type: image/jpeg)

Summary

Folded gneiss, old path to Reinigeadal, Harris. Folded gneiss, old path to Reinigeadal, North Harris. This rock is located by the side of the footpath, which was the only way to the isolated community until a road was built, approaching it from the north. Gneiss is the predominant rock type in Harris, and was formed around two billion years ago. The folds resulted from a sequence of mountain building events in the Precambrian.

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Date/TimeThumbnailDimensionsUserComment
current21:13, 12 January 2017Thumbnail for version as of 21:13, 12 January 2017640 × 427 (289 KB)127.0.0.1 (talk)Folded gneiss, old path to Reinigeadal, Harris. Folded gneiss, old path to Reinigeadal, North Harris. This rock is located by the side of the footpath, which was the only way to the isolated community until a road was built, approaching it from the north. Gneiss is the predominant rock type in Harris, and was formed around two billion years ago. The folds resulted from a sequence of mountain building events in the Precambrian.
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