recessional$548559$ - translation to greek
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recessional$548559$ - translation to greek

GLACIALLY FORMED ACCUMULATION OF UNCONSOLIDATED GLACIAL DEBRIS
Glacial moraine; Glacial moraines; Moraines; Lateral moraine; Glacial Drift; Morainic; Morraine; Glacial debris; Morainic drift; Medial moraines; Ground moraine; Medial moraine; Ground moraines; Lateral moraines; Recessional moraine; Morainic gravel; Supraglacial moraine; Ablation moraine; Moraine stripe; Recessional moraines
  • 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.
  • Ground moraines create irregular, rolling topography.
  • The snow-free debris hills around the lagoon are lateral and terminal moraines of a [[valley glacier]] in [[Nepal]].
  • Lateral moraines above Lake Louise, Alberta, Canada.
  • Medial moraines, [[Nuussuaq Peninsula]], [[Greenland]].

recessional      
υποχωρητήριος

Definition

Moraine
·noun An accumulation of earth and stones carried forward and deposited by a glacier.

Wikipedia

Moraine

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).