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Synonyms

esker

American  
[es-ker] / ˈɛs kər /

noun

Geology.
  1. a serpentine ridge of gravelly and sandy drift, believed to have been formed by streams under or in glacial ice.


esker British  
/ ˈɛskɑː, ˈɛskə, -kə /

noun

  1. Also called: os.  a long winding ridge of gravel, sand, etc, originally deposited by a meltwater stream running under a glacier

"Collins English Dictionary — Complete & Unabridged" 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

esker Scientific  
/ ĕskər /
  1. A long, narrow, steep-sided ridge of coarse sand and gravel deposited by a stream flowing in or under a melting sheet of glacial ice. Eskers range in height from 3 m (9.8 ft) to more than 200 m (656 ft) and in length from less than 100 m (328 ft) to more than 500 km (310 mi).


Etymology

Origin of esker

First recorded in 1850–55, esker is from the Irish word eiscir ridge of mountains

Example Sentences

Examples are provided to illustrate real-world usage of words in context. Any opinions expressed do not reflect the views of Dictionary.com.

Some 15,000 years ago, when the Laurentide ice sheet receded from Vermont’s Northeast Kingdom, it left behind an esker, an upside-down riverbed of well-drained sand.

From New York Times • May 23, 2022

When the ice recedes, the sediment remains as a long sinuous ridge known as an esker.

From Textbooks • Jan. 1, 2017

When the ice recedes, the sediment will remain to form a long sinuous ridge known as an esker.

From Textbooks • Jan. 1, 2015

Does the eye make out A flight of ernes, rising from aits or aeries, Whose shadows track across a harsh terrain Of esker and arete?

From Time Magazine Archive

The area of coarse till is bounded on the north by a long sinuous esker of coarse gravel terminating in a flat fan, which is superposed on a field of fine till.

From Drainage Modifications and Glaciation in the Danbury Region Connecticut State of Connecticut State Geological and Natural History Survey Bulletin No. 30 by Sawyer-Harvey, Ruth