File:Reddish, strongly altered, augite-quartz monzodiorite (Duluth Complex, Mesoproterozoic, 1099 Ma; Twin Lakes East Skyline Parkway roadcut, Duluth, Minnesota, USA) 5.jpg

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English: Quartz monzodiorite in the Precambrian of Minnesota, USA.

This reddish-colored rock is a strongly altered, augite-quartz monzodiorite. It is part 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.

Quartz monzodiorite is a granite-like rock - a phaneritic (coarsely-crystalline), intrusive igneous rock. Compared with true granite, quartz monzodiorite has less quartz and less potassium feldspar. (See classification diagram, where "Q" = quartz, "A" = alkali feldspar/potassium feldspar, and "P" = plagioclase feldspar: www.alexstrekeisen.it/immagini/diagrammi/englishmonzonite...)

Geologic unit & age: Duluth Complex, late Mesoproterozoic, 1099 Ma

Locality: Twin Lakes East outcrop (Twin Ponds East outcrop) - roadcut along the northern side of Skyline Parkway, Duluth, northeastern Minnesota, USA (46° 46’ 43.77” North, 92° 07’ 16.40” West)
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Source https://www.flickr.com/photos/47445767@N05/22292003801/
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@N05/22292003801. It was reviewed on 19 June 2022 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

19 June 2022

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