Drumlins and eskers are found in glacial areas.
Drumlins are hills made of glacial sediment and till, while eskers are long ridges of glacial drift.
They are called drumlins.
Illinois was heavily glaciated. There are moraines, drumlins, eskers, kettles, kames, floodplaines, hills,ravines and gorges.http://traveltips.usatoday.com/ten-types-landforms-illinois-60315.html
an esker is formed by a Glacier
depositional
Glacier movement
b. eskers
Drumlins are formed by glacial movement; eskers from streams under the glacier.
Drumlins are found on a hill
Drumlins are caused by both erosion and deposition. These drumlins are found in the lowlands of Scotland and are small egg shaped hills.
When deposits of till build up, they can leave behind various landforms such as moraines, drumlins, eskers, and outwash plains. These features are created by the movement of glaciers and the deposition of sediments as the glacier retreats.
They are called drumlins.
Drumlins.
Illinois was heavily glaciated. There are moraines, drumlins, eskers, kettles, kames, floodplaines, hills,ravines and gorges.http://traveltips.usatoday.com/ten-types-landforms-illinois-60315.html
A group of drumlins are referred to as a (basket of eggs)
A glacial lake is a lake with origins in a melted glacier. Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks.
eskers
Eskers