File:Pikes Peak (Pikes Peak Granite, Mesoproterozoic, 1.08 Ga; central Colorado, USA) 1.jpg
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| Description |
English: Pikes Peak (looking west from between Colorado Springs and Manitou Springs). All of the pinkish-red rocks are granites of the Pikes Peak Batholith (1.08 b.y.).
One of the most visited mountain peaks in the American Cordillera is central Colorado’s Pikes Peak. The rocks of this mountain & surrounding area represent the Pikes Peak Batholith, a fairly large, late Mesoproterozoic-aged igneous intrusion that was emplaced 1.08 billion years ago. Published research on the Pikes Peak Batholith has shown that several igneous facies are present (e.g., Hutchinson, 1987). Reference cited: Hutchinson, R.M. 1987. Granite-tectonics of the Pikes Peak intrusive center of Pikes Peak composite batholith, Colorado. Geological Society of America Centennial Field Guide 2: 331-334. |
| Date | |
| Source | https://www.flickr.com/photos/47445767@N05/15025082765/ |
| 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@N05/15025082765 (archive). It was reviewed on 24 December 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 20:27, 24 December 2019 | | 3,006 × 1,311 (1.85 MB) | Ser Amantio di Nicolao (talk | contribs) | User created page with UploadWizard |
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