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Summary
| Description |
Anchor ice formations can be seen on the sea floor under the sea ice here at Cape Armitage off of Ross Island in McMurdo Sound, Antarctica. Anchor ice formations will 'cycle', meaning that they will become bouyant enough to lift the rock or gravel that they are attached to off of the sea floor, and will float away in the current or attach to the underside of the sea ice. New anchor ice formations are constantly forming during the coldest periods of the year, September to December. photo by Paul Cziko, DeVries/Cheng lab, University of Illinois, Urbana-Champaign, USA. |
| Date | 14 March 2006 (original upload date) |
| Source | No machine-readable source provided. Own work assumed (based on copyright claims). |
| Author | No machine-readable author provided. Pcziko assumed (based on copyright claims). |
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. |
  
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This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license. | |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 05:59, 14 March 2006 | | 1,600 × 1,200 (22 KB) | Pcziko | Anchor ice formations can be seen on the sea floor under the sea ice here at Cape Armitage off of Ross Island in McMurdo Sound, Antarctic. Anchor ice formations will 'cycle', meaning that they will become bouyant enough to lift the rock or gravel that the |
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