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List of glaciers

List of glaciers is a science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand List of glaciers rather than just read about it. In short: A glacier (US: GLAY-shər) or (UK: ) 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. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features.

List of glaciers — main illustration
List of glaciers — illustration

Key takeaways

  • List of glaciers belongs to science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect List of glaciers to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of List of glaciers from memory before moving on to harder problems.

Reference excerpt

A glacier (US: GLAY-shər) or (UK: ) 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. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. Because glacial mass is affected by long-term climate changes, e.g., precipitation, mean temperature, and cloud cover, glacial mass changes are considered among the most sensitive indicators of climate change. There are about 198,000 to 200,000 glaciers in the world. Catalogs of glaciers include:

World Glacier Inventory World Glacier Monitoring Service Global Land Ice Measurements from Space (GLIMS) Glacier Database Randolph Glacier Inventory (RGI)

Glaciers by continent

Africa

Africa, specifically East Africa, has contained glacial regions, possibly as far back as the last glacier maximum 10 to 15 thousand years ago. Seasonal snow does exist on the highest peaks of East Africa as well as in the Drakensberg Range of South Africa, the Stormberg Mountains, and the Atlas Mountains in Morocco. Currently, the only remaining glaciers on the continent exist on Mount Kilimanjaro, Mount Kenya, and the Rwenzori.

Antarctica

There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. The lists include outlet glaciers, valley glaciers, cirque glaciers, tidewater glaciers and ice streams. Ice streams are a type of glacier and many of them have "glacier" in their name, e.g. Pine Island Glacier. Ice shelves are listed separately in the List of Antarctic ice shelves. For the purposes of these lists, the Antarctic is defined as any latitude further south than 60° (the continental limit according to the Antarctic Treaty System). There are also glaciers in the subantarctic. This includes one snow field (Murray Snowfield). Snow fields are not glaciers in the strict sense of the word, but they are commonly found at the accumulation zone or head of a glacier. For the purposes of this list, Antarctica is defined as any latitude further south than 60° (the continental limit according to the Antarctic Treaty).

Asia

List of glaciers in Bhutan List of glaciers in India List of glaciers in Nepal List of glaciers in Pakistan

Europe

The majority of Europe's glaciers are found in the Alps, Caucasus and the Scandinavian Mountains (mostly Norway) as well as in Iceland. Iceland has the largest glacier in Europe, Vatnajökull Glacier, that covers between 8,100 and 8,300 km2 in area and 3,100 km3 in volume. Norway alone has more than 2500 glaciers (including very small ones) covering an estimated 1% of mainland Norway's surface area. Several of mainland Europe's biggest glaciers are found here including; Jostedalsbreen (the largest in mainland Europe at 487 km2), Vestre Svartisen (221 km2), Søndre Folgefonna (168 km2) and Østre Svartisen (148 km2). The two Svartisen glaciers used to be one connected entity during the Little Ice Age but has since separated.

List of glaciers in Iceland List of glaciers in Norway List of glaciers in Svalbard List of glaciers in Russia List of glaciers in Switzerland Southernmost glacial mass in Europe

North America

There are a number of glaciers existing in North America, currently or in recent centuries. In the United States, these glaciers are located in nine states, all in the Rocky Mountains or further west. The southernmost named glacier among them is the Lilliput Glacier in Tulare County, east of the Central Valley of California. Mexico has about two dozen glaciers, all of which are located on Pico de Orizaba (Citlaltépetl), Popocatépetl and Iztaccíhuatl, the three tallest mountains in the country.

List of glaciers in Canada List of glaciers in Greenland List of glaciers in Mexico List of glaciers in the United States

Oceania

No glaciers remain on the Australia mainland or Tasmania. A few, like the Heard Island glaciers are located in the territory of Heard Island and McDonald Islands in the southern Indian Ocean. New Guinea has the Puncak Jaya glacier. New Zealand contains many glaciers, mostly located near the Main Divide of the Southern Alps in the South Island. They are classed as mid-latitude mountain glaciers. There are eighteen small glaciers in the North Island on Mount Ruapehu. An inventory of South Island glaciers compiled in the 1980s indicated there were about 3,155 glaciers with an area of at least one hectare (2.5 acres). Approximately one sixth of these glaciers covered more than 10 hectares. These include:

Fox Glacier Franz Josef Glacier Hooker Glacier Mueller Glacier Murchison Glacier Tasman Glacier Volta Glacier

South America

Glaciers in South America develop exclusively on the Andes and are subject of the Andes various climatic regimes namely the Tropical Andes, Dry Andes and the Wet Andes. Apart from this there is a wide range of latitudes on which glaciers develop from 5000 m in the Altiplano mountains and volcanoes to reaching sealevel as tidewater glaciers from San Rafael Lagoon (45° S) and southwards. South America hosts two large ice fields, the Northern and Southern Patagonian Ice Fields, of which the latter is the second largest contiguous body of glaciers in extrapolar regions. The glaciers of Venezuela are located in the mountains of the Sierra Nevada de Mérida. In 1910, maps made by the explorer Alfredo Jahn showed the Sierra Nevada glaciers covering about 1,000 hectares (2,500 acres). An ice trade at that time saw ice men or hieleros transporting glacier ice by mule or on foot to Mérida for sale, a six hour journey. Venezuela's glacier coverage shrank to about 280 hectares (700 acres) in 1952, and 80 hectares (200 acres) in 1985. The last remaining glacier, located on Pico Humboldt, was estimated to cover 10 hectares (25 acres) in 2011.

Remote islands

Christensen Glacier – Bouvet Island, Atlantic Ocean Cook Glacier – Kerguelen Islands, Indian Ocean Fortuna Glacier – South Georgia Island, Atlantic Ocean Jacka Glacier – Anzac Peak, Heard Island, Indian Ocean Mawson Peak – Heard Island, Indian Ocean Posadowsky Glacier – Bouvet Island, Atlantic Ocean

… excerpt ends here. Continue reading the full article.

Illustrations

List of glaciers illustration
List of glaciers: Furtwängler Glacier (foreground) as it appeared in August 2014. Behind the glacier are snowfields and the Northern Icefield.
Furtwängler Glacier (foreground) as it appeared in August 2014. Behind the glacier are snowfields and the Northern Icefield.
List of glaciers: Canada Glacier in Antarctica
Canada Glacier in Antarctica
List of glaciers: Chenega Glacier, an active glacier in Alaska
Chenega Glacier, an active glacier in Alaska
List of glaciers: Animated map of the extent of the glaciers of the Carstens Range from 1850 to 2003
Animated map of the extent of the glaciers of the Carstens Range from 1850 to 2003

Worked examples

Example 1 — a first encounter with List of glaciers

Start with the simplest possible case. Write down what List of glaciers claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to List of glaciers before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about List of glaciers ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of List of glaciers

In research
List of glaciers appears in science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses List of glaciers in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
List of glaciers is common in secondary-school and first-year university syllabi. It links to neighbouring topics Glaciers, Lists of glaciers, Natural environment-related lists, so understanding it makes those chapters shorter.
In everyday life
Look for List of glaciers outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study List of glaciers in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what List of glaciers means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain List of glaciers out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is List of glaciers in simple terms?

A glacier (US: GLAY-shər) or (UK: ) 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. Glaciers slowly deform and flow due to stresses induced by t…

Why does List of glaciers matter?

Because it connects several science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study List of glaciers?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on List of glaciers.

Tags

  • Glaciers
  • Lists of glaciers
  • Natural environment-related lists

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