File:Layered Gabbro of the Duluth Complex in Minnesota USA 01.jpg

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English: Layered gabbros of the troctolitic series in the Duluth Complex at a roadcut next to parking lot for the Thomson Hill Information Center, Skyline Parkway, northern side of Interstate 35, just west of the Route 2-Interstate 35 intersection, west of Duluth, Minnesota, USA. (Geology hammer for scale). The gabbro formed 1099 million years ago.
This is gabbro, a mafic, phaneritic, intrusive igneous rock composed principally of plagioclase feldspar and pyroxene. This rock 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. Layering is not commonly seen in intrusive igneous rocks. These layered gabbros are the result of repeated episodes of crystal settling in a magma chamber.
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Source https://www.flickr.com/photos/jsjgeology/21454438859/
Author James St. John (https://www.flickr.com/people/jsjgeology/)
Camera location46° 43′ 46.14″ N, 92° 12′ 25.27″ W Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/21454438859 (archive). It was reviewed on 25 May 2018 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

25 May 2018

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current19:23, 25 May 2018Thumbnail for version as of 19:23, 25 May 20184,000 × 3,000 (5.8 MB)FlickreviewR 2 (talk | contribs)Replacing image by its original image from Flickr
19:22, 25 May 2018Thumbnail for version as of 19:22, 25 May 20181,024 × 768 (442 KB)GeoWriter (talk | contribs)User created page with UploadWizard

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