(ਭੂ-ਵਿਗਿਆਨ,

eskers's Usage Examples:

There are also glacial landforms such as eskers, kames, moraines, and kettle lakes that formed during the retreat of the.

The Esker Riada is a collection of eskers that passes through.

It contains a group of sinuous, branched ridges that resembles eskers that form when streams are under glaciers.

is a system of eskers that stretch across the middle of Ireland, between Dublin and Galway.

Features interpreted as eskers have been observed in the southern Phlegra Montes.

The retreating glacier also left eskers and erratics.

area contains very hilly terrain and glacial landforms, such as kettles, kames and eskers.

These eskers would indicate a large, thick sheet of ice.

erosional surfaces include: outwash plains, kames, kame terraces, kettle holes, eskers, varves, and proglacial lakes.

They include kames, kame terraces and eskers formed in ice contact and outwash fans and outwash.

include remnants of the last glacial period, where retreating glaciers left kames, eskers, and kettles.

They include kames, kame terraces and eskers formed in ice contact and outwash fans and outwash plains below the ice.

applied to drumlins and, in Maine, to both eskers and ridges known as "horsebacks".

Synonyms:

ridge,

Antonyms:

natural depression,