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What (who) is recessional$548559$ - definition
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![Arctic push moraine in northern [[Ellesmere Island]], Grant Land](https://commons.wikimedia.org/wiki/Special:FilePath/Ellesmere Island 04.jpg?width=200 "Arctic push moraine in northern [[Ellesmere Island]], Grant Land")
![Moraines clearly seen on a side glacier of the [[Gorner Glacier]], [[Zermatt]], [[Switzerland]]. The '''lateral moraine''' is the high snow-free bank of debris in the top left hand quarter of the picture. The '''medial moraine''' is the double line of debris running down the centre-line of the glacier.](https://commons.wikimedia.org/wiki/Special:FilePath/Glacier.zermatt.arp.750pix.jpg?width=200 "Moraines clearly seen on a side glacier of the [[Gorner Glacier]], [[Zermatt]], [[Switzerland]]. The '''lateral moraine''' is the high snow-free bank of debris in the top left hand quarter of the picture. The '''medial moraine''' is the double line of debris running down the centre-line of the glacier.")
![Medial moraines, [[Nuussuaq Peninsula]], [[Greenland]].](https://commons.wikimedia.org/wiki/Special:FilePath/Nuussuaq-peninsula-moraines.jpg?width=200 "Medial moraines, [[Nuussuaq Peninsula]], [[Greenland]].")
![Moraine in [[Rocky Mountain National Park]], taken by [[Ansel Adams]] in 1941.](https://commons.wikimedia.org/wiki/Special:FilePath/Ansel Adams - National Archives 79-AA-M02.jpg?width=200 "Moraine in [[Rocky Mountain National Park]], taken by [[Ansel Adams]] in 1941.")
![Rila Mountain]], [[Bulgaria]].](https://commons.wikimedia.org/wiki/Special:FilePath/Icy-lake.jpg?width=200 "Rila Mountain]], [[Bulgaria]].")
![Lateral moraines of a retreating [[glacier]] in [[Engadin]].](https://commons.wikimedia.org/wiki/Special:FilePath/Moraines Surlej.jpg?width=200 "Lateral moraines of a retreating [[glacier]] in [[Engadin]].")
![Moraine of [[Lake Garda]].](https://commons.wikimedia.org/wiki/Special:FilePath/Colline moreniche del Lago Garda.JPG?width=200 "Moraine of [[Lake Garda]].")
Wikipedia
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A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet).
