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The equilibrium line of a glacier is the imaginary line that separates the accumulation zone from the wastage zone. (:

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βˆ™ 13y ago
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βˆ™ 6mo ago

The equilibrium line of a glacier is the boundary where there is an equal balance between the amount of ice gained through snow accumulation and the amount lost through melting or iceberg calving. It divides the accumulation zone (above the equilibrium line) from the ablation zone (below the equilibrium line). Glaciers will advance or retreat depending on the position of their equilibrium line.

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Q: What is the equilibrium line of a glacier?
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Related questions

How does the glacial budget control the migration of the equilibrium line?

The glacial budget, which consists of accumulation and ablation of ice mass, directly influences the position of the equilibrium line on a glacier. If accumulation exceeds ablation, the equilibrium line moves towards the glacier's top, leading to glacier advance. Conversely, if ablation exceeds accumulation, the equilibrium line shifts downslope, causing glacier retreat.


Which parts of glaciers and its triburitaries moves most quickly?

The center of a glacier and its tributaries usually move faster than the edges due to the ice flow being concentrated in the middle. This is known as glacier flow dynamics, where the center is under more pressure due to the mass of ice pushing down on it.


What is The line dividing the zone of accumulation from the zone of ablation on a valley glaciers is called?

The line dividing the zone of accumulation from the zone of ablation on a valley glacier is called the equilibrium line. This line marks the point where accumulation (snowfall) equals ablation (melting and sublimation), influencing the glacier's overall mass balance and movement.


What situation allows a glaciers size to be maintained?

a glacier has a snowline at the same height as the wastage line.


What is a line of low hills formed by rock pushed at the front of a glacier?

A moraine is a line of low hills formed by rock and debris pushed to the front of a glacier as it advances. This material is deposited as the glacier melts, creating distinctive landforms in its path.


How are conditions of pressure and temperature at which two phases coexist in equilibrium shown on a phase diagram?

On a phase diagram, the conditions of pressure and temperature at which two phases coexist in equilibrium are represented by a line. This line is called the phase boundary or phase equilibrium line. It separates the regions where the two phases exist in equilibrium from the region where only one phase is present.


An ice front is likely to be stationary when the glacier does what?

An ice front is likely to be stationary when the rate of ice accumulation in the glacier matches the rate of ice loss due to melting or calving at the front. This equilibrium state is known as a stable glacier front, where there is no net advance or retreat of the ice front.


What is the name of a curved line on a graph?

price or equilibrium A curve


What are terminal moraine?

Terminal moraines are ridges of glacial debris deposited at the furthest point reached by a glacier. They mark the end of a glacier's advance and can be seen as a line of debris and rocks left behind as the glacier melts and retreats. These moraines are called "terminal" because they are found at the glacier’s terminus.


Where the Siachen glacier is located in Pakistan?

The Siachen Glacier is located in the eastern Karakoram range in the Himalaya Mountains, just east of the Line of Control between India-Pakistan.


How many road miles between SC and Glacier National Park?

The driving distance from the South Carolina state line to Glacier National Park is about 2,254 road miles.


Is the car in equilibrium a car that travels at a constant speed in straight line?

Yes