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Southern Patagonian Ice Field

Southern Patagonian Ice Field 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 Southern Patagonian Ice Field rather than just read about it. In short: The Southern Patagonian Ice Field (Spanish: Campo de Hielo Patagónico Sur), located at the Southern Patagonic Andes between Chile and Argentina, is the world's second largest contiguous extrapolar ice field. It is the bigger of two remnant parts of the Patagonian Ice Sheet, which covered all of southern Chile during the last glacial period, locally called the Llanquihue glaciation.

Southern Patagonian Ice Field — main illustration
Southern Patagonian Ice Field — illustration

Key takeaways

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

Reference excerpt

The Southern Patagonian Ice Field (Spanish: Campo de Hielo Patagónico Sur), located at the Southern Patagonic Andes between Chile and Argentina, is the world's second largest contiguous extrapolar ice field. It is the bigger of two remnant parts of the Patagonian Ice Sheet, which covered all of southern Chile during the last glacial period, locally called the Llanquihue glaciation.

Geography

The Southern Patagonian Ice Field extends from parallels 48° 15′ S to 51° 30′ S for approximately 350 kilometres (220 mi), and has an approximate area of 16,480 km2 (6,360 sq mi), of which 14,200 km2 (5,500 sq mi) belong to Chile and 2,600 km2 (1,000 sq mi) belong to Argentina. The ice mass feeds dozens of glaciers in the area, among which are the Upsala (765 km2 or 295 sq mi), Viedma (978 km2 or 378 sq mi) and Perito Moreno (258 km2 or 100 sq mi) in the Los Glaciares National Park in Argentina, and the Pío XI Glacier or Bruggen Glacier (1,265 km2 or 488 sq mi, the largest in area and longest in the Southern Hemisphere outside of Antarctica), O'Higgins (820 km2 or 320 sq mi), Grey (270 km2 or 100 sq mi) and Tyndall (331 km2 or 128 sq mi) in Chile. The glaciers going to the west flow into the fjords of the Patagonian channels of the Pacific Ocean; those going to the East flow into the Patagonian lakes Viedma and Argentino, and eventually, through the rivers de la Leona and Santa Cruz, to the Atlantic Ocean. An important part of the ice field is protected under different national parks, such as the Bernardo O'Higgins and Torres del Paine in Chile, and the aforementioned Los Glaciares in Argentina. There are two known volcanoes under the ice field: Lautaro and Viedma. Due to their inaccessibility they are among the least researched volcanoes in Chile and Argentina. In 1980, Chile planned Route 8 as a section of the Carretera Austral west of the ice field, which has not been built. Circo de los Altares is an important hiking place.

History

Exploration Thorough explorations include the expeditions of Federico Reichert (1913–1914), Alberto de Agostini (1931), and Harold William Tilman and Jorge Quinteros (1955–1956), as well as Eric Shipton (1960–61). The first (North-South) crossing of the field was accomplished in 1998 by Pablo Besser, Mauricio Rojas, José Montt, and Rodrigo Fica. Nevertheless, some areas of the field remain largely unexplored. From the air, initial exploration was conducted in 1928–29 by Gunther Plüschow after whom a glacier is named. From April 1944 to April 1945, the United States Army Air Forces conducted an aerial survey using the Trimetrogon method at the request of the Chilean government.

Borderline

The boundary between Argentina and Chile in the area was established by the 1881 treaty and delimited in 1898 by the experts of both countries working in the demarcation of the border, and which differences led to the 1902 award, in which they agreed they did not have differences on the part of the border between Fitz Roy and Stokes. The award is established "to perpetuity" by both countries under British tutelage. The map published by the British Crown, as part of the documentation of the 1902 award, illustrates a clear demarcation line (from the Fitz Roy to the Stokes) to the east of the Southern Patagonian Ice Fields, leaving most of the territory in question in the Chilean side. The 1902 award considered that in that area the high peaks are water dividing and therefore there was no dispute. Both experts, Francisco Pascasio Moreno from Argentina and Diego Barros Arana from Chile, agreed on the border between Mount Fitz Roy and Stokes (nowadays Cervantes). Since 1898, the demarcation of the border in the ice field, between the two mountains, was defined on the next mountains and their natural continuity: Fitz Roy, Torre, Huemul, Campana, Agassiz, Heim, Mayo, and Stokes/Cervantes. In 1914, the Mariano Moreno range was visited by an expedition; however, Francisco Pascasio Moreno already knew of its existence. Argentina started to question the border, arguing that the border should be in the Mariano Moreno range. In 1994, the Laguna del Desierto dispute was solved which involved territory of the Ice Field; an international tribunal awarded almost the whole zone to Argentina. After a refused appeal in 1995, Chile accepted the award. Since then, Chile has had a small corridor to access Mount Fitz Roy, and the Marconi Pass was defined as an international border crossing point. The Southern Patagonian Ice Field section of the border is the last remaining land border issue between Chile and Argentina. On August 1, 1991, the governments of Chile and Argentina agreed on a borderline, but the agreement was never ratified by the Argentine legislature. Later, in 1998, both governments agreed to redraw the borderline between Mount Fitz Roy and Daudet. Section A of the agreement (between Cerro Murallón and Daudet) and a small part of B (from Fitz Roy to a point defined to the west) was drawn; however, they also agreed that section B (from Fitz Roy to Murallón) would wait until completion of a detailed 1:50,000 scale map of the area with further negotiations. To date, this one section remains the final non-concluded boundary section and has been an irritant in Argentina-Chile relations.

Controversies after the 1998 agreement

In February 2006, Ricardo Lagos appeared in a photo with the head of the Air Force, General Osvaldo Sarabia, in the undemarcated area; this caused controversy with Argentina. In 2006, the Argentine Instituto Geográfico Militar (IGM) (today Instituto Geográfico Nacional) edited a map without a note about the undefined border but showed the Argentine claims as the official borderline. After Chilean diplomatic protests, the Argentine government withdrew the map and urged Chile to expedite the demarcation of the international border according to the 1998 agreement. On August 24, 2006, the Argentine Undersecretary of Tourism stated that the maps used by the Secretariat of Tourism's website were official because they were approved by the National Geographic Institute of Argentina. In 2006, president of Chile Michelle Bachelet and president of Argentina Néstor Kirchner held a meeting over the cartographic controversy. Kirchner served as the governor of the Santa Cruz Province from 1991 to 2003.

… excerpt ends here. Continue reading the full article.

Worked examples

Example 1 — a first encounter with Southern Patagonian Ice Field

Start with the simplest possible case. Write down what Southern Patagonian Ice Field 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 Southern Patagonian Ice Field 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 Southern Patagonian Ice Field 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 Southern Patagonian Ice Field

In research
Southern Patagonian Ice Field 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 Southern Patagonian Ice Field 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
Southern Patagonian Ice Field is common in secondary-school and first-year university syllabi. It links to neighbouring topics Bodies of ice of Magallanes Region, Glaciers of Argentina, Glaciers of Aysén Region, so understanding it makes those chapters shorter.
In everyday life
Look for Southern Patagonian Ice Field 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 Southern Patagonian Ice Field in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Southern Patagonian Ice Field 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 Southern Patagonian Ice Field out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Southern Patagonian Ice Field in simple terms?

The Southern Patagonian Ice Field (Spanish: Campo de Hielo Patagónico Sur), located at the Southern Patagonic Andes between Chile and Argentina, is the world's second largest contiguous extrapolar ice field. It is the bigger of two remnant parts of the Patagonian Ice Sheet, which covered all of sou…

Why does Southern Patagonian Ice Field 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 Southern Patagonian Ice Field?

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 Southern Patagonian Ice Field.

Tags

  • Bodies of ice of Magallanes Region
  • Glaciers of Argentina
  • Glaciers of Aysén Region
  • Ice fields of South America
  • Landforms of Argentina
  • Landforms of Santa Cruz Province, Argentina
  • Última Esperanza Province

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