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Glaciers form U-shaped valleys. They make striations, drumlins, kettlelakes, eratics, moraines and cirque.
Michigan was once covered by glaciers, which put an enormous amount of weight on the ground, compressing it. With the glaciers gone the ground is rebounding, and the resulting shifts can produce earthquakes. There may also be old faults left over from the formation of the continent or produced by stresses within the North American plate.
Glaciers move slowly.
the moutains glaciers are melting.
Glaciers move slowly.
Eskers were formed by depositional processes. They are long, winding ridges of sand and gravel that were deposited by meltwater streams flowing in tunnels beneath glaciers during the last Ice Age.
three of the five glaciers for erosional are plucking, abrasion and striane
Glaciers form U-shaped valleys. They make striations, drumlins, kettlelakes, eratics, moraines and cirque.
Erosional features in areas with valley glaciers include U-shaped valleys, cirques (bowl-shaped hollows at the head of glaciers), arêtes (sharp ridge between cirques), and hanging valleys (smaller valleys that join a main glacier valley). Glacial striations (scratches on bedrock caused by moving glacier ice) and moraines (piles of debris deposited by glaciers) are also common erosional features.
An erosional-depositional system refers to the process by which sediments are eroded from one location (such as a riverbed or coastline) and deposited in another location due to the action of natural forces like water, wind, or glaciers. This system shapes the Earth's surface by moving and redistributing sediments over time. Examples include rivers depositing sediment downstream or glaciers eroding and depositing material as they move.
The effects of the mountain glaciers on Canada included beautiful formation of distinctive features such as cirques, icebergs, and deep gorges.
Alpine Glacier produce a variety of erosional features. These features are usually rounded or polished grooves made by the glacier's passing. The features are called arete, Circque, horn, tarn, u shaped valley, and hanging valleys.
A mountain is classified as a volcano if it has a crater at the summit and is formed from volcanic activity. On the other hand, a horn is a sharp, pyramid-shaped peak formed by the erosional processes of glaciers. Examining the geological features and formation history of the mountain can help determine whether it is a volcano or a horn.
Desert landscapes are not typically formed by glaciers. Deserts are characterized by arid conditions with little to no precipitation, while glaciers are massive bodies of ice that reshape landscapes through erosional processes like scouring and deposition.
Glacial scarring refers to the erosional marks left behind by glaciers as they move across the Earth's surface. This can include striations, grooves, and other features carved into the bedrock by the movement of the glacier. Glacial scarring is a key indicator of past glacial activity in an area and provides valuable information about the history of ice sheets and glaciers.
Erratic refers to a type of glacial deposit that is transported by glaciers and deposited in locations far from their source, often as a result of ice movement during the last Ice Age. Therefore, erratic is associated with depositional processes.
Water is the single most important erosional agent on Earth. Through processes like rivers, rainfall, and glaciers, water has the power to shape and carve the Earth's surface over time.