A moraine.
Kames. Many are found in areas of kettles and moraines.
Glaciers form smooth hills by eroding and shaping the landscape as they move down a slope. The weight of the ice and the movement of the glacier over time smooth out the terrain beneath it, resulting in the formation of long smooth hills called drumlins.
These long smooth hills are known as drumlins, which are created by the movement of glaciers during the process of glaciation. As a glacier advances, it reshapes the landscape by depositing and sculpting materials, forming these distinctive elongated landforms. Drumlins are typically found in regions that were once covered by ice sheets during the last Ice Age.
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.
Hills are natural landforms that are characterized by a gentle slope or incline. They are usually formed by the movement of glaciers, erosion, or tectonic activity. Hills are smaller in size compared to mountains and are often used for recreational activities like hiking and skiing.
A Drum let is the proper term
A glacier formed long smooth hills are called drumlins. They are created when a glacier slides over the ground and reshapes the underlying material, depositing sediments and creating elongated, tear-shaped landforms. Drumlins are typically found in areas that were once covered by glaciers.
Kames. Many are found in areas of kettles and moraines.
Glaciers form smooth hills by eroding and shaping the landscape as they move down a slope. The weight of the ice and the movement of the glacier over time smooth out the terrain beneath it, resulting in the formation of long smooth hills called drumlins.
Kames. Many are found in areas of kettles and moraines.
These long smooth hills are known as drumlins, which are created by the movement of glaciers during the process of glaciation. As a glacier advances, it reshapes the landscape by depositing and sculpting materials, forming these distinctive elongated landforms. Drumlins are typically found in regions that were once covered by ice sheets during the last Ice Age.
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.
Two types of glacial deposits are moraines, which are formations of mixed sediment pushed by and deposited from a glacier, and drumlins, which are elongated hills made of glacial till that form parallel to the direction of ice flow.
Hills may be formed by an uplift of the land, or the wearing down of mountains, or a combination of both.
The difference is that a Roche Moutonée is an erosional landform whereas a drumlin is a depositional one. A Roche Moutonée is formed by a glacier moving over the top of the rock plucking one side giving it a jagged edge and abrading the other side giving it a smooth edge. A drumlin on the other hand is deposited by the glacier and are streamlined into elongated hills by the glacier. Drumlins are unknown as to how they are formed with there being many theories as to how they are made but one I feel sounds likely is that when it melts out of the subglacial layers it is lodged on the floor and is shaped by the glacier into the shape. Hope this helps you!
Glaciers push up mounds of dirt as the advance forward. When they recede, they leave these mounds of earth, debris and rock What are these mounds called? In my ancient memory, I thought they were called doldrums, but this doesn't seem to be right judging from the responses I have obtained from this site. The hills are called moraines or just a moraine.
A valley is the low ground area between two hills or mountains. It is typically formed by water erosion or glacier movement over time, creating a depressed area where a river or stream may flow through. Valleys can vary in size and shape depending on the surrounding landscape.