File:Half Dome (Sierra Nevada Mountains, California, USA) 4.jpg
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| Description |
English: Granodiorite in the Cretaceous of California, USA.
The granites at Half Dome are part of an extensive, Cretaceous-aged intrusive complex in eastern California called the Sierra Nevada Batholith. The complex consists of numerous individual plutons, many of which are old, cooled magma chambers that were originally beneath ancient subduction zone volcanoes. Half Dome itself is a large exfoliation dome bisected by vertical jointing. Geologic unit: Half Dome Granodiorite, Late Cretaceous, 89-93 Ma Locality: view from Glacier Point, Yosemite National Park, Sierra Nevada Mountains, eastern California, USA |
| Date | |
| Source | https://www.flickr.com/photos/47445767@N05/50042764608/ |
| 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@N05/50042764608. It was reviewed on 13 October 2020 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 | 00:48, 13 October 2020 | | 3,008 × 2,000 (5.45 MB) | Ser Amantio di Nicolao (talk | contribs) | Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/50042764608/ with UploadWizard |
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