Answer: Cirques
One type of Alpine glacier is a cirque glacier, which forms in a bowl-shaped depression on the side of a mountain. These glaciers are typically small and may be found at the head of a valley or on a mountainside.
Glaciers can move in any direction, including backwards, but typically they move in the direction of their accumulating mass (downhill). Factors such as changes in temperature, pressure, and topography can influence the direction of glacier movement.
Glaciers fall under the category of physical geography, specifically geomorphology. They are large bodies of ice that form over long periods of time and have a significant impact on landscapes and ecosystems.
Glaciers are large masses of ice that move slowly over land. They shape the landscape by eroding rocks and soil, creating valleys, fjords, and lakes. As glaciers advance and retreat, they leave behind moraines, drumlins, and other landforms that reshape the geography of a region.
Answer: Cirques
One type of Alpine glacier is a cirque glacier, which forms in a bowl-shaped depression on the side of a mountain. These glaciers are typically small and may be found at the head of a valley or on a mountainside.
The glaciers helped to form many aspects of New England. This includes the mountains and the big lakes that are there.
Glaciers can move in any direction, including backwards, but typically they move in the direction of their accumulating mass (downhill). Factors such as changes in temperature, pressure, and topography can influence the direction of glacier movement.
Glaciers fall under the category of physical geography, specifically geomorphology. They are large bodies of ice that form over long periods of time and have a significant impact on landscapes and ecosystems.
Glaciers shaped the geography of the Midwest by carving out the Great Lakes, depositing glacial debris that formed the fertile soils of the region, and creating other landforms like moraines, drumlins, and kettles. The retreat of glaciers also left behind numerous lakes and rivers that support the agricultural and transportation networks in the region.
False
Glaciers are large masses of ice that move slowly over land. They shape the landscape by eroding rocks and soil, creating valleys, fjords, and lakes. As glaciers advance and retreat, they leave behind moraines, drumlins, and other landforms that reshape the geography of a region.
Glaciers shape the Earth's surface through processes like erosion, transportation of sediments, and deposition. As glaciers move, they scrape and carve the land, creating features like valleys, fjords, and cirques. When glaciers melt, they leave behind sediment and rock formations that contribute to the landscape.
Glaciers from the last ice age carved out the landscape of the Midwest by creating features such as flat plains, rolling hills, and numerous lakes. They also deposited sediments that formed fertile soils, which contribute to the region's agricultural productivity. Additionally, glaciers left behind moraines, eskers, and drumlins that can still be seen in the region today.
environment and society
That is impossible to answer. There is nothing to compare the Earth to if that scenario happened.