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Summary
| Description |
Canyon passage in a cave in Virginia, USA. Skyline Caverns is developed in structurally tilted carbonates (mixed dolostones and limestones) of the Rockdale Run Formation (Beekmantown Group, Lower Ordovician). Cave passages vary significantly in their size, sinuousity, and cross-section shape. Passages that are taller than they are wide are called canyon passages - they form in the vadose zone (above the water table). Locality: Skyline Caverns, Front Royal, central Warren County, northern Virginia, USA |
| Date | |
| Source | Canyon passage (Skyline Caverns, Front Royal, Virginia, USA) 2 |
| Author | James St. John |
Licensing
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@N05/28393169636 (archive). It was reviewed on 31 August 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 19:19, 31 August 2019 | | 3,000 × 4,000 (4.57 MB) | LittleT889 | Transferred from Flickr via #flickr2commons |
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