Original file (SVG file, nominally 800 × 489 pixels, file size: 572 KB)
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| DescriptionGlacier-ice shelf interactions.svg | 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 | |
| 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⊙☿♀♁♂♃♄ |
| Public domainPublic domainfalsefalse |
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This work is in the public domain in the United States because it is a work prepared by an officer or employee of the United States Government as part of that person’s official duties under the terms of Title 17, Chapter 1, Section 105 of the US Code.
Note: This only applies to original works of the Federal Government and not to the work of any individual U.S. state, territory, commonwealth, county, municipality, or any other subdivision. This template also does not apply to postage stamp designs published by the United States Postal Service since 1978. (See § 313.6(C)(1) of Compendium of U.S. Copyright Office Practices). It also does not apply to certain US coins; see The US Mint Terms of Use.
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| This file has been identified as being free of known restrictions under copyright law, including all related and neighboring rights. | ||
https://creativecommons.org/publicdomain/mark/1.0/PDMCreative Commons Public Domain Mark 1.0falsefalse
| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 17:36, 27 May 2014 | | 800 × 489 (572 KB) | Szczureq | converted '''everything''' to paths to prevent blackboxing |
| 17:31, 27 May 2014 |  | 800 × 489 (344 KB) | Szczureq | removed black boxes... finally? | |
| 11:57, 5 November 2012 |  | 800 × 489 (346 KB) | Szczureq | Inkscape lied - reverted to version as of 00:11, 21 May 2012 | |
| 11:53, 5 November 2012 |  | 800 × 489 (86 KB) | Szczureq | removed even more invisible objects (incl. black box-generating); paths converted to text | |
| 00:11, 21 May 2012 |  | 800 × 489 (346 KB) | Sagredo | removed invisible objects | |
| 23:53, 20 May 2012 |  | 800 × 489 (469 KB) | Sagredo | 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 | use stroke to path to try to remove black boxes in wikipedia renderings | |
| 19:35, 23 May 2008 |  | 1,200 × 734 (455 KB) | Sagredo | {{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 | {{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 | {{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 |
This file contains additional information, probably added from the digital camera or scanner used to create or digitize it.
If the file has been modified from its original state, some details may not fully reflect the modified file.
| Width | 800 |
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| Height | 489.36575 |
