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three of the five glaciers for erosional are plucking, abrasion and striane

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Escher's are glacial features formed when .?

Escher's are glacial features formed when meltwater streams underneath a glacier, creating tunnels and channels that can collapse to form depressions on the glacier's surface. These features can disrupt or alter the glacier's flow and structure.


What are five different physical features that you can visit in Washington?

Mt. Saint Helans, Mt. hadems, Glacier Peak, Mt. baker, and the Columbus basin


The major natural features of antarctica?

ice ..Glacier.


Who is glacier national park named after?

Glacier National Park is not named for a person but for its glacial features and glacial landscape.


Which is a sign that a valley glacier has moved through an area?

A sign that a valley glacier has moved through an area is the presence of U-shaped valleys, which have been carved by the glacier's movement. Additionally, features like striations on bedrock, polished surfaces, and glacial moraines—accumulations of debris—often indicate past glacial activity. These features reflect the powerful erosive forces of the glacier as it advanced and retreated.


What are 2 ways that a glacier can deposit sediment?

Glaciers can deposit sediment through processes known as till and outwash. Till is unsorted sediment that is deposited directly by the glacier as it melts, forming features like moraines. Outwash occurs when meltwater from the glacier carries sediment away from the glacier's terminus, depositing it in sorted layers further downstream. Both processes contribute to the landscape and geological features shaped by glacial activity.


Features form when tension and compression build under the surface of a flowing glacier?

As glaciers move, the immense weight and pressure of the ice cause deformation in the underlying rock and sediment. Tension and compression build up beneath the glacier due to the flow dynamics, leading to the formation of features such as crevasses, ridges, and moraines. These features reflect the glacier's movement and the interactions between the ice and the landscape, revealing the complex processes at play beneath the surface. Ultimately, these geological formations provide insights into the glacier's history and behavior.


Is a glacier a concrete or abstract?

A concrete noun is a word for something that can be experienced by any of the five physical senses; something that can be seen, heard, smelled, tasted, or touched.A glacier can be seen and touched, the word glacier is a concrete noun.


Ridges that form along the sides of glacial valleys as a glacier melts are called what?

Ridges that form along the sides of glacial valleys as a glacier melts are called moraines. Specifically, lateral moraines are found along the edges of a glacier, while terminal moraines accumulate at the glacier's end. These features are composed of debris and sediment that the glacier has transported and deposited as it advances and retreats.


Erosional features produced by alpine glaciers?

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.


How can you tell which direction a glacier moved?

You can determine the direction a glacier moved by examining the features it left behind. Striations, which are scratches on rocks caused by the movement of the glacier, point in the direction of flow. Additionally, the shape of landforms such as moraines and drumlins can indicate the glacier's movement direction, with moraines forming at the glacier's edges and drumlins aligned in the direction of flow. Lastly, the orientation of glacial deposits can also provide clues about the glacier's path.


What are three glacial features formed by erosion?

Cirques are bowl-shaped depressions formed by glacial erosion at the head of a glacier. Arêtes are narrow ridges that separate two adjacent glacial valleys. Roche moutonnées are glacier-smoothed bedrock outcrops with a gentle up-glacier slope and a steep down-glacier slope.