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Glacier and Post-glacial rebound

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Glacier and Post-glacial rebound

Glacier vs. Post-glacial rebound

A glacier is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the lifting of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression.

Similarities between Glacier and Post-glacial rebound

Glacier and Post-glacial rebound have 16 things in common (in Unionpedia): Antarctica, Drumlin, Earth, Esker, Fresh water, Glacial period, Glacial striation, Glaciology, Global warming, Greenland, Ice sheet, Kettle (landform), Last glacial period, Patagonia, Sea level rise, U-shaped valley.

Antarctica

Antarctica is Earth's southernmost continent.

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Drumlin

A drumlin, from the Irish word droimnín ("littlest ridge"), first recorded in 1833, and in the classical sense is an elongated hill in the shape of an inverted spoon or half-buried egg formed by glacial ice acting on underlying unconsolidated till or ground moraine.

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Earth

Earth is the third planet from the Sun and the only astronomical object known to harbor life.

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Esker

An esker, eskar, eschar, or os, sometimes called an asar, osar, or serpent kame, is a long, winding ridge of stratified sand and gravel, examples of which occur in glaciated and formerly glaciated regions of Europe and North America.

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Fresh water

Fresh water (or freshwater) is any naturally occurring water except seawater and brackish water.

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Glacial period

A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances.

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Glacial striation

Glacial striations are scratches or gouges cut into bedrock by glacial abrasion.

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Glaciology

Glaciology (from Latin: glacies, "frost, ice", and Ancient Greek: λόγος, logos, "subject matter"; literally "study of ice") is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice.

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Global warming

Global warming, also referred to as climate change, is the observed century-scale rise in the average temperature of the Earth's climate system and its related effects.

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Greenland

Greenland (Kalaallit Nunaat,; Grønland) is an autonomous constituent country within the Kingdom of Denmark between the Arctic and Atlantic Oceans, east of the Canadian Arctic Archipelago.

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Ice sheet

An ice sheet is a mass of glacier ice that covers surrounding terrain and is greater than, this is also known as continental glacier.

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Kettle (landform)

A kettle (kettle hole, pothole) is a shallow, sediment-filled body of water formed by retreating glaciers or draining floodwaters.

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Last glacial period

The last glacial period occurred from the end of the Eemian interglacial to the end of the Younger Dryas, encompassing the period years ago.

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Patagonia

Patagonia is a sparsely populated region located at the southern end of South America, shared by Argentina and Chile.

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Sea level rise

A sea level rise is an increase in global mean sea level as a result of an increase in the volume of water in the world’s oceans.

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U-shaped valley

U-shaped valleys, trough valleys or glacial troughs, are formed by the process of glaciation.

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The list above answers the following questions

Glacier and Post-glacial rebound Comparison

Glacier has 195 relations, while Post-glacial rebound has 104. As they have in common 16, the Jaccard index is 5.35% = 16 / (195 + 104).

References

This article shows the relationship between Glacier and Post-glacial rebound. To access each article from which the information was extracted, please visit:

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