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File:Glacier-ice shelf interactions.svg - Wikipedia

  • ️Fri May 23 2008

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File:Glacier-ice shelf interactions.svg

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Date/TimeThumbnailDimensionsUserComment
current17:36, 27 May 2014Thumbnail for version as of 17:36, 27 May 2014800 × 489 (572 KB)Szczureqconverted '''everything''' to paths to prevent blackboxing
17:31, 27 May 2014Thumbnail for version as of 17:31, 27 May 2014800 × 489 (344 KB)Szczureqremoved black boxes... finally?
11:57, 5 November 2012Thumbnail for version as of 11:57, 5 November 2012800 × 489 (346 KB)SzczureqInkscape lied - reverted to version as of 00:11, 21 May 2012
11:53, 5 November 2012Thumbnail for version as of 11:53, 5 November 2012800 × 489 (86 KB)Szczureqremoved even more invisible objects (incl. black box-generating); paths converted to text
00:11, 21 May 2012Thumbnail for version as of 00:11, 21 May 2012800 × 489 (346 KB)Sagredoremoved invisible objects
23:53, 20 May 2012Thumbnail for version as of 23:53, 20 May 2012800 × 489 (469 KB)Sagredouse stroke to path to try to remove black boxes in wikipedia renderings
23:52, 20 May 2012No thumbnail800 × 489 (469 KB)Sagredouse stroke to path to try to remove black boxes in wikipedia renderings
19:35, 23 May 2008Thumbnail for version as of 19:35, 23 May 20081,200 × 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 2008Thumbnail for version as of 19:23, 23 May 20081,200 × 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 2008Thumbnail for version as of 19:21, 23 May 20081,200 × 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

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Width800
Height489.36575