drumlins
The smooth, canoe-shaped hills left by a passing glacier are known as "drumlins." These landforms are formed by the accumulation of glacial till, shaped by the movement of ice. Drumlins typically have a streamlined profile, with a steep side facing the direction of the glacier's advance and a gentler slope on the opposite side. They often occur in clusters and provide valuable insights into past glacial activity and flow patterns.
drumlins
drumlins
The smooth, canoe-shaped hills left by a passing glacier are known as "drumlins." These landforms are formed by the deposition of sediment beneath a glacier, which molds the material into streamlined shapes. Drumlins typically have a steeper side facing the direction of the glacier's movement and a gentler slope on the opposite side. They are often found in clusters and serve as indicators of past glacial activity.
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.
Drumlins are long smooth hills that are usaully found in groups. Kame are small cone shaped hills of sand and gravel.
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.
He shaped the clay into a beautiful bowl. The hills had been shaped by the running water.
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 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.
sand dunes
Volcanoes are usually cone shaped mountains or hills.