mountain glaciers
its not mountain glaciers but its valley glaciers
Valley Glaciers :)
Yes, Wisconsin has some small glaciers present in the northern part of the state. These glaciers are remnants from the last Ice Age and are mostly found in areas like the Kettle Moraine State Forest. However, they are very small compared to the massive glaciers found in places like Alaska or Greenland.
A cirque glacier is a small glacier that occupies a cirque or rests against the headwall of a cirque. A cirque is a deep, horseshoe-shaped hollow with steep walls which was created by erosive activity of glaciers.
A small mountain lake that forms in a cirque after a glacier melts is called a "tarn." Tarns are typically surrounded by steep cliffs and are often found in mountainous regions where glaciers once existed. They can vary in size and depth, and their formation is a result of glacial activity that carves out the landscape.
The small glaciers that exist in high mountainous areas were called mountain glaciers or cirque glaciers.
its not mountain glaciers but its valley glaciers
Valley Glaciers :)
a small mountainous country in Europe
Yes, Wisconsin has some small glaciers present in the northern part of the state. These glaciers are remnants from the last Ice Age and are mostly found in areas like the Kettle Moraine State Forest. However, they are very small compared to the massive glaciers found in places like Alaska or Greenland.
A cirque glacier is a small glacier that occupies a cirque or rests against the headwall of a cirque. A cirque is a deep, horseshoe-shaped hollow with steep walls which was created by erosive activity of glaciers.
A small ice mass that spreads outward on a land surface is known as a glacier. Glaciers form from accumulated snow that compresses into ice over time, and they move slowly due to gravity. They can vary in size and are typically found in mountainous regions or polar areas. As they advance, they can shape the landscape through erosion and deposition of sediment.
During the time of Pangaea, large ice sheets existed in regions of Africa that are now predominantly tropical or arid, particularly in parts of southern Africa. Specifically, glacial deposits from the late Paleozoic era indicate that glaciers once covered areas such as the present-day Cape of Good Hope and parts of what is now Namibia. These glaciers have long since melted, and Africa now has no significant glaciers, with the exception of a few small ice caps on Mount Kilimanjaro and the Rwenzori Mountains.
Most of Egypt by area is desert. However, the majority of the Egyptian population is concentrated in the small fertile areas along the Nile River. There are additionally mountainous areas in the Sinai Peninsula.
Virginia had cotton plantations in some parts but in the western more mountainous areas, it was small homes and subsistence farming. The plantations had slaves.
Yes, glaciers erode the base of mountains into basins called cirques through the process of glacial erosion. As a glacier moves down a mountainside, it plucks and abrasively scrapes the rock beneath, creating a bowl-shaped depression called a cirque. Over time, these cirques can deepen and widen, forming distinctive features in mountainous regions.
A cirque basin is a natural amphitheater-like depression formed by glacial erosion, typically found in mountainous regions. It is characterized by steep, often rocky walls and a relatively flat floor, which may contain a small lake or tarn. Cirques are created as glaciers carve out the landscape through processes of erosion and weathering, often serving as the origin point for valley glaciers. Over time, they can evolve into features such as U-shaped valleys as the glaciers advance and retreat.