The retreat of Icelandic glacier Múlajökull, which is an outlet glacier of Hofsjökull, recently exposed a 50 drumlin cluster, which serves as the basis for improved understanding of drumlin formation.
The literature also documents extensive drumlin fields in England, Scotland and Wales, Switzerland, Poland, Estonia, Sweden, around Lake Constance north of the Alps, County Monaghan, County Mayo, County Cavan, County Fermanagh and County Down in Ireland, Germany, Hindsholm in Denmark, Finland and Greenland.
They are called drumlins.
A group of drumlins are referred to as a (basket of eggs)
Drumlins are caused by both erosion and deposition. These drumlins are found in the lowlands of Scotland and are small egg shaped hills.
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.
Farmers often plant crops on drumlins because their soil is deep and well-drained.
Drumlins are found on a hill
deposition
Agriculture
Drumlins
When glaciers advance or retreat, the sediments left behind create a moraine. Drumlins are created by the flow of glaciers that mold sediment into streamlined, elongated hills.
Inverted spoon, occurring in swarms.
drumlins