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.
Drumlins are usually found in regions that were covered by glaciers during the last Ice Age, such as parts of North America and Europe. Eskers are commonly found in areas that were once covered by glaciers, including parts of Scandinavia, North America, and Siberia.
They are called drumlins.
Drumlins.
A group of drumlins are referred to as a (basket of eggs)
Drumlins are elongated, smoothly rounded hills with a steep side facing the direction of past ice movement. They can range in size from a few meters to over a kilometer in length and are typically composed of glacial till or glacial sediments. Drumlins are usually found clustered together in a group known as a drumlin field.
Farmers often plant crops on drumlins because their soil is deep and well-drained.
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.
deposition
Drumlins are long smooth hills that are usaully found in groups. Kame are small cone shaped hills of sand and gravel.
Erratics and drumlins are both types of geological formations associated with glacial activity. Erratics are large boulders transported and deposited by glaciers, often found in areas where the surrounding rock is different from the rock type of the erratic. Drumlins, on the other hand, are elongated hills formed from glacial till that has been shaped by the movement of ice. Both features provide evidence of past glacial movements and help in understanding the dynamics of glacial landscapes.
Drumlins