Fasciculus:Glacier-ice shelf interactions.svg

Size of this PNG preview of this SVG file: 800 × 489 elementa imaginalia. Aliae mensurae: 320 × 196 elementa imaginalia | 640 × 391 elementa imaginalia | 1 024 × 626 elementa imaginalia | 1 280 × 782 elementa imaginalia | 2 560 × 1 565 elementa imaginalia.

Sua resolutio ‎(fasciculus SVG, nominale 800 × 489 elementa imaginalia, magnitudo fasciculi: 572 chiliocteti)

Hic fasciculus apud Vicimedia Communia iacet; in aliis inceptis adhiberi potest. Contenta paginae descriptionis fasciculi subter monstrantur.

Summarium

DescriptioGlacier-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.
Datum	23 Maius 2008
Fons	http://nsidc.org/sotc/iceshelves.html
Auctor	Original Image by Ted Scambos and Michon Scott, National Snow and Ice Data Center. Redrawn by Sagredo^{⊙☿♀♁♂♃♄}

Potestas usoris

	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.
This file has been identified as being free of known restrictions under copyright law, including all related and neighboring rights.

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Historia fasciculi

Presso die vel tempore fasciculum videbis, sicut tunc temporis apparuit.

	Dies/Tempus	Minutio	Dimensiones	Usor	Sententia
recentissima	17:36, 27 Maii 2014		800 × 489 (572 chiliocteti)	Szczureq	converted '''everything''' to paths to prevent blackboxing
	17:31, 27 Maii 2014		800 × 489 (344 chiliocteti)	Szczureq	removed black boxes... finally?
	11:57, 5 Novembris 2012		800 × 489 (346 chiliocteti)	Szczureq	Inkscape lied - reverted to version as of 00:11, 21 May 2012
	11:53, 5 Novembris 2012		800 × 489 (86 chiliocteti)	Szczureq	removed even more invisible objects (incl. black box-generating); paths converted to text
	00:11, 21 Maii 2012		800 × 489 (346 chiliocteti)	Sagredo	removed invisible objects
	23:53, 20 Maii 2012		800 × 489 (469 chiliocteti)	Sagredo	use stroke to path to try to remove black boxes in wikipedia renderings
	23:52, 20 Maii 2012	Nulla minutio	800 × 489 (469 chiliocteti)	Sagredo	use stroke to path to try to remove black boxes in wikipedia renderings
	19:35, 23 Maii 2008		1 200 × 734 (455 chiliocteti)	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 Maii 2008		1 200 × 734 (118 chiliocteti)	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 Maii 2008		1 200 × 734 (118 chiliocteti)	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