File:Aplite (Laramie Anorthosite Complex, Mesoproterozoic; Sybille Canyon, Laramie Range, Wyoming, USA).jpg

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English: Aplite from the Precambrian of Wyoming, USA.

Igneous dikes are planar to irregularly-planar intrusions that cut across country rocks. They can be thin or extremely thick; they can be vertically- or obliquely-oriented. The rock seen here is from a zoned aplite-pegmatite dike that intruded anorthosite. Aplite is a finely-crystalline dike rock having a granitic composition. Pegmatite is a very coarsely-crystalline igneous rock, usually granitic.

Host rocks: Laramie Anorthosite Complex, Middle Proterozoic, ~1.4 Ga

Locality: roadcut on the northern side of Route 34, ~0.9 to 1.0 miles west of milepost 25, southwest of Poe Mountain & northeast of Morton Pass, Sybille Canyon, Laramie Range, southeastern Wyoming, USA
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Source https://www.flickr.com/photos/47445767@N05/51139354787/
Author James St. John

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This file is licensed under the Creative Commons Attribution 2.0 Generic license.
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/51139354787. It was reviewed on 6 May 2021 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

6 May 2021

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Date/TimeThumbnailDimensionsUserComment
current19:23, 6 May 2021Thumbnail for version as of 19:23, 6 May 20213,077 × 1,529 (3.42 MB)Ser Amantio di Nicolao (talk | contribs)Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/51139354787/ with UploadWizard

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