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.
Glaciation on interior plains can create unique landforms like drumlins, eskers, and outwash plains. The movement of glaciers can shape the landscape by depositing sediment and carving out valleys. Glaciation also leads to the formation of lakes and wetlands in the region.
Eskers are sort because meltwter from the glaiger passed throught the middle of the glaicer making a tunnel
an esker is formed by a Glacier
Some deposits of alpine glaciers include moraines (such as lateral, medial, and terminal moraines), drumlins, eskers, and outwash plains. These deposits are created as the glacier erodes, transports, and deposits sediment during its movement.
b. eskers
Drumlins and eskers are landforms created by glacial activity. Drumlins are elongated hills formed by the movement of glacial ice, which shapes the underlying sediment into a streamlined form as the glacier advances and retreats. In contrast, eskers are long, winding ridges of sediment deposited by meltwater streams that flow beneath or within a glacier, leaving behind layers of sand and gravel as the glacier retreats. Both features are indicators of past glacial processes and provide insights into the dynamics of ice movement.
Glacial till can be found in areas where glaciers have deposited material as they advance and retreat, such as moraines, drumlins, and eskers. It is commonly found in regions that have experienced glaciation, such as parts of North America, Europe, and Antarctica.
Drumlins are found on a hill
A drumlin is a smooth, elongated mound of glacial till formed by a moving glacier, while an esker is a long, winding ridge of sand and gravel deposited by a meltwater stream flowing in tunnels within or beneath a glacier. Drumlins are typically shaped like hills while eskers are long, narrow ridges.
Drumlins are caused by both erosion and deposition. These drumlins are found in the lowlands of Scotland and are small egg shaped hills.
The main types of glacial deposition are till, moraines, drumlins, eskers, and outwash plains. Till is unsorted sediment deposited directly by the glacier, while moraines are ridges of till deposited at the glacier's margin. Drumlins are smooth, elongated hills formed under glacial ice, eskers are winding ridges of sand and gravel deposited by meltwater streams, and outwash plains are flat areas of sorted sediment deposited beyond the glacier by meltwater.
Some glacial deposition features include moraines, drumlins, eskers, and outwash plains. These features are a result of the deposition of sediment and rocks carried by glaciers as they move and melt.
Moraines, drumlins, eskers, and outwash plains are glacial features that result from deposition. Moraines are ridges of till deposited along the edges of a glacier, drumlins are elongated hills of glacial till, eskers are long, winding ridges of sand and gravel, and outwash plains are flat areas of sand and gravel deposited by meltwater streams flowing away from the glacier.
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.
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.