Drumlins are caused by both erosion and deposition. These drumlins are found in the lowlands of Scotland and are small egg shaped hills.
Drumlins
drumlins
drumlins
drumlins
drumlins
These are called drumlins. Drumlins are smooth, elongated hills composed of till that have been shaped by the movement of an overriding glacier or continental ice sheet. They are typically oriented in the direction of ice flow and are common features in areas that were once covered by ice sheets during the last glacial period.
The glacial features that occur in swarms of long and smooth canoe-shaped hills are called drumlins. Drumlins are typically formed under moving glaciers and indicate the direction of ice flow. They are important indicators of past glacial activity and can be found in large numbers clustered together in areas that were once covered by ice sheets.
They are called drumlins.
Moraines are formations made of till (rock, sand, and clay) deposited by glaciers, while drumlins are elongated hills made of glacial deposits shaped by the moving ice. Moraines are typically ridges or mounds, while drumlins have a streamlined shape with a gentle slope facing the direction the glacier advanced.
An obovate leaf is tear-shaped or egg-shaped.
A group of drumlins are referred to as a (basket of eggs)