File:Glacier-ice shelf interactions.svg - Wikimedia Commons
- ️Fri May 23 2008
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| Description | Glacier-ice shelf interactions: In a stable glacier-ice shelf system, the glacier's downhill movement is offset by the buoyant force of the water on the front of the shelf. Warmer temperatures destabilize this system by lubricating the glacier's base and creating melt ponds that eventually carve through the shelf. Once the ice shelf retreats to the grounding line, the buoyant force that used to offset glacier flow becomes negligible, and the glacier picks up speed on its way to the sea. |
| Date | 23 May 2008 |
| Source | http://nsidc.org/sotc/iceshelves.html |
| Author | Original Image by Ted Scambos and Michon Scott, National Snow and Ice Data Center. Redrawn by Sagredo⊙☿♀♁♂♃♄ |
File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 17:36, 27 May 2014 |  | 800 × 489 (572 KB) | Szczureq (talk | contribs) | converted '''everything''' to paths to prevent blackboxing |
| 17:31, 27 May 2014 |  | 800 × 489 (344 KB) | Szczureq (talk | contribs) | removed black boxes... finally? | |
| 11:57, 5 November 2012 |  | 800 × 489 (346 KB) | Szczureq (talk | contribs) | Inkscape lied - reverted to version as of 00:11, 21 May 2012 | |
| 11:53, 5 November 2012 |  | 800 × 489 (86 KB) | Szczureq (talk | contribs) | removed even more invisible objects (incl. black box-generating); paths converted to text | |
| 00:11, 21 May 2012 |  | 800 × 489 (346 KB) | Sagredo (talk | contribs) | removed invisible objects | |
| 23:53, 20 May 2012 |  | 800 × 489 (469 KB) | Sagredo (talk | contribs) | use stroke to path to try to remove black boxes in wikipedia renderings | |
| 23:52, 20 May 2012 | No thumbnail | 800 × 489 (469 KB) | Sagredo (talk | contribs) | use stroke to path to try to remove black boxes in wikipedia renderings | |
| 19:35, 23 May 2008 |  | 1,200 × 734 (455 KB) | Sagredo (talk | contribs) | {{Information |Description=Glacier-ice shelf interactions: In a stable glacier-ice shelf system, the glacier's downhill movement is offset by the buoyant force of the water on the front of the shelf. Warmer temperatures destabilize this system by lubricat | |
| 19:23, 23 May 2008 |  | 1,200 × 734 (118 KB) | Sagredo (talk | contribs) | {{Information |Description=Glacier-ice shelf interactions: In a stable glacier-ice shelf system, the glacier's downhill movement is offset by the buoyant force of the water on the front of the shelf. Warmer temperatures destabilize this system by lubricat | |
| 19:21, 23 May 2008 |  | 1,200 × 734 (118 KB) | Sagredo (talk | contribs) | {{Information |Description=Glacier-ice shelf interactions: In a stable glacier-ice shelf system, the glacier's downhill movement is offset by the buoyant force of the water on the front of the shelf. Warmer temperatures destabilize this system by lubricat |
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| Width | 800 |
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| Height | 489.36575 |