(ভূতত্ত্ব

eskers's Usage Examples:

observed on the crater floor are believed to be eskers, which form when streams run under a glacier.

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

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

period left many eskers, deposits of sand and gravel up to 50 metres (160 ft) in height.

Wildlife and people use the elevated eskers as travel routes.

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

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

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

previous publications in that they are eskers.

Based on morphometrical and geomorphological analysis of the Argyre eskers and their immediate surroundings,.

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

The retreating glacier also left eskers and erratics.

other glacial features such as, kettles and eskers.

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

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

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

Glacial till has been shaped into a mosaic of ridges and eskers, sinuous, rounded ridges deposited by during glaciation.

eskers's Meaning':

(geology

Synonyms:

ridge;

Antonyms:

natural depression;