File:Garnet-biotite rock (alteration halo around magnetite-rich meta-iron formation) (Archean, metamorphism at ~3.2 Ga & ~2.8 Ga; Quad Creek section - roadcut along the Beartooth Highway, Beartooth Mountains, Montana, USA) 2.jpg

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English: Garnet-biotite rock in the Precambrian of Montana, USA.

This rock is dominated by red garnet crystals and black biotite mica. It is part of an alteration halo around an outcrop of Archean-aged, magnetite-rich meta-iron formation. This material, and the meta-iron formation (depositional age ~3.3 Ga), formed during two metamorphic episodes in the Precambrian: 1) about 3.2 Ga (granulite-facies metamorphism); and 2) about 2.8 Ga (upper amphibolite facies metamorphism).

Locality: Quad Creek section (= locality of Mueller et al., 1987) - roadcut on southern side of Beartooth Highway (Rt. 212), immediately west of Quad Creek, between milepost 50 and milepost 51, southern side of Rock Creek Canyon, just north of the eroded edge of Beartooth Plateau, southwest of the town of Red Lodge, Beartooth Mountains, southern Montana, USA (45° 01' 41.27" North latitude, 109° 24' 55.31" West longitude)


Some info. from:

Mueller et al. (1987) - Geological Society of America Centennial Field Guide, Rocky Mountain Section, pp. 75-76.

Maier (2011) - Geology and Geochemistry of Hadean Zircon-Bearing Supracrustals from Quad Creek, Eastern Beartooth Mountains, Montana, USA. M.S. Thesis. University of Colorado. 59 pp.
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Source https://www.flickr.com/photos/47445767@N05/52615143730/
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@N05/52615143730. It was reviewed on 9 January 2023 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

9 January 2023

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