Ficheru:Glacier-ice shelf interactions.svg
Tamañu de la vista previa PNG d'esti ficheru SVG: 800 × 489 pixels. Otres resoluciones: 320 × 196 pixels | 640 × 391 pixels | 1024 × 626 pixels | 1280 × 782 pixels | 2560 × 1565 pixels.
Ficheru orixinal (ficheru SVG, 800 × 489 píxels nominales, tamañu de ficheru: 572 kB)
Historial del ficheru
Calca nuna fecha/hora pa ver el ficheru como taba daquella.
Data/Hora | Miniatura | Dimensiones | Usuariu | Comentariu | |
---|---|---|---|---|---|
actual | 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 pay 2012 | 800 × 489 (346 kB) | Szczureq | Inkscape lied - reverted to version as of 00:11, 21 May 2012 | ||
11:53 5 pay 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 | Ensin miniatura | 800 × 489 (469 kB) | Sagredo | use stroke to path to try to remove black boxes in wikipedia renderings | |
19:35 23 may 2008 | 1200 × 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 | 1200 × 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 | 1200 × 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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