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Esker - Wikipedia, the free encyclopedia
An esker is a long winding ridge of stratified sand and gravel, examples of which occur in glaciated and formerly glaciated regions of Europe and North America. Eskers are frequently several miles l...
en.wikipedia.org/wiki/Esker
The Physical Environment ... ;; Contents |Glossary | Atlas | Index |Blog|Podcasts| Earth Online | Updates ... The curving shape of an esker in Manitoba, Canada .
www.uwsp.edu/geo/faculty/ritter/glossary/E_G/esker.html www.uwsp.edu/geo/faculty/ritter/glossary/E_G/esker.html
Esker Sediments ... An esker (often known locally as a horseback) is a relatively narrow raised sedimentary deposit that winds across a landscape. Eskers are formed from glacial deposits. When a glacier is melting, rivers can form inside or underneath the ice.
www.unity.edu/facultypages/hopeck/PhysicalGeology/field... www.unity.edu/facultypages/hopeck/PhysicalGeology/fieldguide/esker/eskers.htm
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Fireworks Splice HTML ... Location of eskers throughout Canada's Arctic. ... The term esker comes from the Gaelic word eiscir, meaning "ridge". Eskers are sinuous ridges of gravel that have been deposited following the retreat of a glacier and can extend for many kilometres.
www.arctic.uoguelph.ca/cpe/environments/land/glaciers/f... www.arctic.uoguelph.ca/cpe/environments/land/glaciers/features/eskers.htm
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A classic esker, covered with forest, winds across northern Manitoba. ... The low ridge winding across the landscape of northern Manitoba, Canada, is a classic esker. When a great ice sheet covered central North America, about 10,000 years ago, a stream of meltwater ran beneath it at this location.
geology.about.com/library/bl/images/blesker.htm geology.about.com/library/bl/images/blesker.htm
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