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- Q3866635 subject Q7066307.
- Q3866635 abstract "Glacial motion is the motion of glaciers, which can be likened to rivers of ice. It has played an important role in sculpting many landscapes. Most lakes in the world occupy basins scoured out by glaciers. Glacial motion can be fast (up to 30 m/day, observed on Jakobshavn Isbræ in Greenland) or slow (0.5 m/year on small glaciers or in the center of ice sheets), but is typically around 1 metre/day.".
- Q3866635 thumbnail Glacial_lakes,_Bhutan.jpg?width=300.
- Q3866635 wikiPageExternalLink glacier_balance.html.
- Q3866635 wikiPageExternalLink glaciers.html.
- Q3866635 wikiPageExternalLink origin.html.
- Q3866635 wikiPageExternalLink glacier.html.
- Q3866635 wikiPageExternalLink 10af.html.
- Q3866635 wikiPageExternalLink ch18.htm.
- Q3866635 wikiPageExternalLink ch18_2.htm.
- Q3866635 wikiPageWikiLink Q1069.
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- Q3866635 wikiPageWikiLink Q30.
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- Q3866635 wikiPageWikiLink Q35666.
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- Q3866635 wikiPageWikiLink Q39816.
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- Q3866635 wikiPageWikiLink Q52139.
- Q3866635 wikiPageWikiLink Q556920.
- Q3866635 wikiPageWikiLink Q663753.
- Q3866635 wikiPageWikiLink Q7066307.
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- Q3866635 wikiPageWikiLink Q8008.
- Q3866635 wikiPageWikiLink Q869697.
- Q3866635 wikiPageWikiLink Q903816.
- Q3866635 comment "Glacial motion is the motion of glaciers, which can be likened to rivers of ice. It has played an important role in sculpting many landscapes. Most lakes in the world occupy basins scoured out by glaciers. Glacial motion can be fast (up to 30 m/day, observed on Jakobshavn Isbræ in Greenland) or slow (0.5 m/year on small glaciers or in the center of ice sheets), but is typically around 1 metre/day.".
- Q3866635 label "Glacial motion".
- Q3866635 depiction Glacial_lakes,_Bhutan.jpg.