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moraine$50323$ - ترجمة إلى اليونانية
GLACIALLY FORMED ACCUMULATION OF UNCONSOLIDATED DEBRIS AT THE EDGE OF A GLACIER
Terminal Moraines; End moraine; Push end moraine; Shove end moraine
![-wide}} terminal lobe of a glacier flowing down from the interior [[ice cap]] on top of the [[Byam Martin Mountains]], [[Bylot Island]], [[Nunavut]], [[Canada]]. Note the terminal moraine "bulldozed" at the ice front.](https://commons.wikimedia.org/wiki/Special:FilePath/Bylot Island Glacier (cropped).jpg?width=200 "-wide}} terminal lobe of a glacier flowing down from the interior [[ice cap]] on top of the [[Byam Martin Mountains]], [[Bylot Island]], [[Nunavut]], [[Canada]]. Note the terminal moraine \"bulldozed\" at the ice front.")
![[[Davidson Glacier]], [[Alaska]]. There is a glacier-fed lake in addition to the formation of a small channel heading in the southeast direction.](https://commons.wikimedia.org/wiki/Special:FilePath/Davidson Glacier1994 2008.jpg?width=200 "[[Davidson Glacier]], [[Alaska]]. There is a glacier-fed lake in addition to the formation of a small channel heading in the southeast direction.")
![Terminal moraine of [[Penny Ice Cap]], Baffin Island, Nunavut, Canada](https://commons.wikimedia.org/wiki/Special:FilePath/Penny Ice Cap Terminal Moraine.jpg?width=200 "Terminal moraine of [[Penny Ice Cap]], Baffin Island, Nunavut, Canada")
![Map of the ''[[Salpausselkä]]'' terminal moraines in [[Southern Finland]]](https://commons.wikimedia.org/wiki/Special:FilePath/Salpausselat-kartta.svg?width=200 "Map of the ''[[Salpausselkä]]'' terminal moraines in [[Southern Finland]]")
moraine
n. είδος χνουδωτού υφάσματος, σωροί λίθων σε τους πρόποδες παγόβουνου, σωροί λίθων στους πρόποδες παγόβουνου
تعريف
Moraine
·noun An accumulation of earth and stones carried forward and deposited by a glacier.
ويكيبيديا
Terminal moraine
A terminal moraine, also called end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front edge of the ice, is driven no further and instead is deposited in an unsorted pile of sediment. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice.
