File:Anorthosite xenolith (anorthosite series, Duluth Complex, Mesoproterozoic, 1099 Ma; Keene Creek East Skyline Parkway roadcut, Duluth, Minnesota, USA) 5 (22040450638).jpg

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Anorthosite in the Precambrian of Minnesota, USA.

This is part of a large anorthosite xenolith that is hosted in gabbro of the widespread Duluth Complex, a ~1.1 billion year old suite of igneous rocks in northeastern Minnesota that is associated with volcanism in the Lake Superior segment of the ancient Mid-Continent Rift System.

Anorthosite is a mafic, phaneritic (coarsely-crystalline), intrusive igneous rock dominated by the mineral plagioclase feldspar - (Ca,Na)Al2Si2O8 - calcium sodium aluminosilicate.

The brownish areas are a weathering crust.

Geologic unit & age of host rocks (not seen in this photo): anorthosite series, Duluth Complex, late Mesoproterozoic, 1099 Ma

Age of anorthosite xenolith: unknown, but Precambrian, likely derived from the lower crust

Locality: Keene Creek East outcrop - roadcut along the northern side of Skyline Parkway, Duluth, northeastern Minnesota, USA (46° 45’ 08.52” North, 92° 10’ 29.93” West)
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Source Anorthosite xenolith (anorthosite series, Duluth Complex, Mesoproterozoic, 1099 Ma; Keene Creek East Skyline Parkway roadcut, Duluth, Minnesota, USA) 5
Author James St. John

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/22040450638 (archive). It was reviewed on 9 October 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

9 October 2019

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Date/TimeThumbnailDimensionsUserComment
current06:17, 9 October 2019Thumbnail for version as of 06:17, 9 October 20194,000 × 3,000 (4.42 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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