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Monday, October 9, 2023

Institute of National Remembrance

From Wikipedia, the free encyclopedia
Institute of National Remembrance
Instytut Pamięci Narodowej
AbbreviationIPN
Formation18 December 1998 (24 years ago)
PurposeEducation, research, archive, and identification. Commemorating the Struggle and Martyrdom. Prosecution of Crimes against the Polish Nation.
HeadquartersWarsaw, Poland
Location
  • 1 Kurtyki Street
Region served
Republic of Poland
Membership
Staff
Official language
Polish
President
Karol Nawrocki
Main organ
Council
Affiliations
Staff
Several hundred
Websitewww.ipn.gov.pl
RemarksThe IPN Headquarters in Warsaw co-ordinates the operations of eleven Branch Offices and their Delegations

The Institute of National RemembranceCommission for the Prosecution of Crimes against the Polish Nation (Polish: Instytut Pamięci Narodowej – Komisja Ścigania Zbrodni przeciwko Narodowi Polskiemu, abbreviated IPN) is a Polish state research institute in charge of education and archives which also includes two public prosecution service components exercising investigative, prosecution and lustration powers. The IPN was established by the Polish parliament by the Act on the Institute of National Remembrance of 18 December 1998 through reforming and expanding the earlier Main Commission for the Investigation of Crimes against the Polish Nation of 1991, which itself had replaced a body on Nazi crimes established in 1945.

In 2018, IPN's mission statement was amended by the controversial Amendment to the Act on the Institute of National Remembrance to include "protecting the reputation of the Republic of Poland and the Polish Nation". The IPN investigates and prosecutes Nazi and Communist crimes committed between 1917 and 1990, documents its findings, and disseminates them to the public. Some scholars have criticized the IPN for politicization, especially under Law and Justice governments.

The IPN began its activities on 1 July 2000. The IPN is a founding member of the Platform of European Memory and Conscience. Since 2020, the IPN headquarters have been located at Postępu 18 Street in Warsaw. The IPN has eleven branches in other cities and seven delegation offices.

Purpose

Main entrance

The IPN's main areas of activity, in line with its original mission statement, include researching and documenting the losses which were suffered by the Polish Nation as a result of World War II and during the post-war totalitarian period. The IPN informs about the patriotic traditions of resistance against the occupational forces, and the Polish citizens' fight for sovereignty of the nation, including their efforts in defence of freedom and human dignity in general.

According to the IPN, it is its duty to prosecute crimes against peace and humanity, as much as war crimes. Its mission includes the need to compensate for damages which were suffered by the repressed and harmed people at a time when human rights were disobeyed by the state, and educate the public about recent history of Poland. IPN collects, organises and archives all documents about the Polish Communist security apparatus active from 22 July 1944 to 31 December 1989.

Following the election of the Law and Justice party, the government formulated in 2016 a new IPN law. The 2016 law stipulated that the IPN should oppose publications of false information that dishonors or harms the Polish nation. It also called for popularizing history as part of "an element of patriotic education". The new law also removed the influence of academia and the judiciary on the IPN.

A 2018 amendment to the law, added article 55a that attempts to defend the "good name" of Poland. Initially conceived as a criminal offense (3 years of jail) with an exemption for arts and research, following an international outcry, the article was modified to a civil offense that may be tried in civil courts and the exemption was deleted. Defamation charges under the act may be made by the IPN as well as by accredited NGOs such as the Polish League Against Defamation. By the same law, the institution's mission statement was changed to include "protecting the reputation of the Republic of Poland and the Polish Nation".

Organisation

IPN was created by special legislation on 18 December 1998. The IPN is divided into:

  • Main Commission for the Prosecution of Crimes against the Polish Nation (Główna Komisja Ścigania Zbrodni Przeciwko Narodowi Polskiemu)
  • Bureau of Provision and Archivization of Documents (Biuro Udostępniania i Archiwizacji Dokumentów)
  • Bureau of Public Education (or Public Education Office, Biuro Edukacji Publicznej)
  • Lustration Bureau (Biuro Lustracyjne) (new bureau, since October 2006)
  • local chapters.

On 29 April 2010, acting president Bronislaw Komorowski signed into law a parliamentary act that reformed the Institute of National Remembrance.

Director

IPN is governed by the director, who has a sovereign position that is independent of the Polish state hierarchy. The director may not be dismissed during his term unless he commits a harmful act. Prior to 2016, the election of the director was a complex procedure, which involves the selection of a panel of candidates by the IPN Collegium (members appointed by the Polish Parliament and judiciary). The Polish Parliament (Sejm) then elects one of the candidates, with a required supermajority (60%). The director has a 5-year term of office. Following 2016 legislation in the PiS controlled parliament, the former pluralist Collegium was replaced with a nine-member Collegium composed of PiS supporters, and the Sejm appoints the director after consulting with the College without an election between candidates.

Leon Kieres

Leon Kieres

The first director of the IPN was Leon Kieres, elected by the Sejm for five years on 8 June 2000 (term 30 June 2000 – 29 December 2005). The IPN granted some 6,500 people the "victim of communism" status and gathered significant archive material. The IPN faced difficulties since it was new and also since the Democratic Left Alliance (containing former communists) attempted to close the IPN. The publication of Neighbors: The Destruction of the Jewish Community in Jedwabne, Poland by Jan T. Gross, proved to be a lifeline for the IPN as Polish president Aleksander Kwaśniewski intervened to save the IPN since he deemed the IPN's research to be important as part of Jewish-Polish reconciliation and "apology diplomacy".

Janusz Kurtyka

Janusz Kurtyka

The second director was Janusz Kurtyka, elected on 9 December 2005 with a term that started 29 December 2005 until his death in the Smolensk airplane crash on 10 April 2010. The elections were controversial, as during the elections a leak against Andrzej Przewoźnik accusing him of collaboration with Służba Bezpieczeństwa caused him to withdraw his candidacy. Przewoźnik was cleared of the accusations only after he had lost the election.

In 2006, the IPN opened a "Lustration Bureau" that increased the director's power. The bureau was assigned the task of examining the past of all candidates to public office. Kurtyka widened archive access to the public and shifted focus from compensating victims to researching collaboration.

Franciszek Gryciuk

Franciszek Gryciuk

In 1999, historian Franciszek Gryciuk was appointed to the Collegium of the IPN, which he chaired 2003–2004. From June 2008 to June 2011, he was vice president of the IPN. He was acting director 2010–2011, between the death of the IPN's second president, Janusz Kurtyka, in the 2010 Polish Air Force Tu-154 crash and the election of Łukasz Kamiński by the Polish Parliament as the third director.

Łukasz Kamiński

Łukasz Kamiński

Łukasz Kamiński, was elected by the Sejm in 2011 following the death of his predecessor. Kamiński headed the Wroclaw Regional Bureau of Public Education prior to his election. During his term, the IPN faced a wide array of criticism calling for an overhaul or even replacement. Critics founds fault in the IPN being a state institution, the lack of historical knowledge of its prosecutors, a relatively high number of microhistories with a debatable methodology, overuse of the martyrology motif, research methodology, and isolationism from the wider research community. In response, Kamiński implemented several changes, including organizing public debates with outside historians to counter the charge of isolationism and has suggested refocusing on victims as opposed to agents.

Jarosław Szarek

Jarosław Szarek

On 22 July 2016 Jarosław Szarek was appointed to head IPN. He dismissed Krzysztof Persak, co-author of the 2002 two-volume IPN study on the Jedwabne pogrom. In subsequent months, IPN featured in media headlines for releasing controversial documents, including some relating to Lech Wałęsa, for memory politics conducted in schools, for efforts to change Communist street names, and for legislation efforts. According to historian Idesbald Goddeeris, this marks a return of politics to the IPN.

Karol Nawrocki

Karol Nawrocki

On 23 July 2021 Karol Nawrocki was appointed to head IPN.

Public prosecutors in the IPN

Two components of the IPN are specialized parts of the Public Prosecution Service of Poland, namely the Main Commission for the Prosecution of Crimes against the Polish Nation and the Lustration Bureau. Each of these two components exercises its activities autonomically from other components of the Institute and is headed by a director who is ex officio Deputy Public Prosecutor General of Poland, while role of the IPN Director is in their case purely accessory and includes no powers regarding conducted investigations, being limited only to providing supporting apparatus and, when vacated, presenting candidates for the offices of the two directors to the Prosecutor General who as their superior has the discretionary power to appoint or reject them.

Main Commission for the Prosecution of Crimes against the Polish Nation

The Main Commission for the Prosecution of Crimes against the Polish Nation (Główna Komisja Ścigania Zbrodni Przeciwko Narodowi Polskiemu) is the oldest component of the IPN tracing its origins to 1945. It investigates and prosecutes crimes committed on Polish soil against Polish citizens as well as people of other citizenships wronged in the country. War crimes which are not affected by statute of limitations according to Polish law include:

  1. Crimes of the Soviet and Polish Communist regimes committed in the country from 17 September 1939 until the Fall of Communism on 31 December 1989.
  2. Deportations to the Soviet Union of Polish soldiers of Armia Krajowa, and other Polish resistance organizations as well as Polish inhabitants of the former Polish eastern territories.
  3. Pacifications of Polish communities between Vistula and Bug rivers in the years 1944 to 1947 by UB-NKVD,
  4. Crimes committed by the law enforcement agencies of the Polish People's Republic, particularly Ministry of Public Security of Poland and Main Directorate of Information of the Polish Army.
  5. Crimes under the category of war crimes and crimes against humanity.

Lustration Bureau

On 15 March 2007, an amendment to the Polish law regulating the IPN (enacted on 18 December 2006) came into effect. The change gave the IPN new lustration powers and expanded IPN's file access. The change was enacted by Law and Justice government in a series of legislative amendments during 2006 and the beginning of 2007. However, several articles of the 2006-7 amendments were held unconstitutional by Poland's Constitutional Court on 11 May 2007, though the IPN's lustration power was still wider than under the original 1997 law. These powers include loss of position for those who submitted false lustration declarations as well as a lustration process of candidates for senior office.

Other activities

Research

Archive at the former IPN headquarters at 28 Towarowa Street in Warsaw

The research conducted by IPN from December 2000 falls into four main topic areas:

  • Security Apparatus and Civil Resistance (with separate sub-projects devoted to Political Processes and Prisoners 1944–1956, Soviet Repressions and Crimes committed against Polish Citizens and Martial Law: a Glance after Twenty Years);
    • Functioning of the repression apparatus (state security and justice organs) – its organizational structure, cadres and relations with other state authority and party organs
    • Activities of the repression apparatus directed against particular selected social groups and organizations
    • Structure and methods of functioning of the People's Poland security apparatus
    • Security apparatus in combat with the political and military underground 1944–1956
    • Activities of the security apparatus against political emigreés
    • Security apparatus in combat with the Church and freedom of belief
    • Authorities dealing with social crises and democratic opposition in the years 1956–1989 f) List of those repressed and sentenced to death
    • Bibliography of the conspiracy, resistance and repression 1944–1989
  • War, Occupation and the Polish Underground;
    • deepening of knowledge about the structures and activities of the Polish Underground State
    • examination of the human fates in the territories occupied by the Soviet regime and of Poles displaced into the Soviet Union
    • assessment of sources on the living conditions under the Soviet and German Nazi occupations
    • evaluation of the state of research concerning the victims of the war activities and extermination policy of the Soviet and German Nazi occupiers
    • examining the Holocaust (Extermination of Jews) conducted by Nazis in the Polish territories
      • Response of the Polish Underground State to the extermination of Jewish population
      • The Polish Underground press and the Jewish question during the German Nazi occupation
  • Poles and Other Nations in the Years 1939–1989 (with a part on Poles and Ukrainians);
    • Poles and Ukrainians
    • Poles and Lithuanians
    • Poles and Germans
    • Communist authorities – Belarusians – Underground
    • Fate of Jewish people in the People's Republic of Poland
    • Gypsies in Poland
  • Peasants and the People's Authority 1944–1989 (on the situation of peasants and the rural policy in the years 1944–1989)
    • inhabitants of the rural areas during the creation of the totalitarian regime in Poland;
    • peasant life during the Sovietisation of Poland in the years 1948–1956;
    • attitudes of the inhabitants of rural areas towards the state-Church conflict in the years 1956–1970;
    • the role of peasants in the anti-Communist opposition of the 1970s and 1980s.

Education

The IPN's Public Education Office (BEP) vaguely defined role in the IPN act is to inform society of Communist and Nazi crimes and institutions. This vaguely defined role allowed Paweł Machcewicz, BEP's director in 2000, freedom to create a wide range of activities.

Researchers at the IPN conduct not only research but are required to take part in public outreach. BEP has published music CDs, DVDs, and serials. It has founded "historical clubs" for debates and lectures. It has also organized outdoor historical fairs, picnic, and games.

The IPN Bulletin [pl] (Polish: Biuletyn IPN) is a high circulation popular-scientific journal, intended for lay readers and youth. Some 12,000 of 15,000 copies of the Bulletin are distributed free of charge to secondary schools in Poland, and the rest are sold in bookstores. The Bulletin contains: popular-scientific and academic articles, polemics, manifestos, appeals to readers, promotional material on the IPN and BEP, denials and commentary on reports in the news, as well as multimedia supplements.

The IPN also publishes the Remembrance and Justice [pl] (Polish: Pamięć i Sprawiedliwość) scientific journal.

The IPN has issued several board games to help educate people about recent Polish history, including:

Naming of monuments

In 2008, the chairman of the IPN wrote to local administrations, calling for the addition of the word "German" before "Nazi" to all monuments and tablets commemorating Germany's victims, stating that "Nazis" is not always understood to relate specifically to Germans. Several scenes of atrocities conducted by Germany were duly updated with commemorative plaques clearly indicating the nationality of the perpetrators. The IPN also requested better documentation and commemoration of crimes that had been perpetrated by the Soviet Union.

The Polish government also asked UNESCO to officially change the name "Auschwitz Concentration Camp" to "Former Nazi German Concentration Camp Auschwitz-Birkenau", to clarify that the camp had been built and operated by Nazi Germany. In 2007, UNESCO's World Heritage Committee changed the camp's name to "Auschwitz Birkenau German Nazi Concentration and Extermination Camp (1940–1945)." Previously some German media, including Der Spiegel, had called the camp "Polish".

Publications

Since 2019, the Institute publishes the Institute of National Remembrance Review (ISSN 2658-1566), a yearly peer-reviewed academic journal in English, with Anna Karolina Piekarska as editor-in-chief..

Criticism

According to Georges Mink [fr], common criticisms of the IPN include its dominance in the Polish research field, which is guaranteed by a budget that far supersedes that of any similar academic institution; the "thematic monotony ... of micro-historical studies ... of no real scientific interest" of its research; its focus on "martyrology"; and various criticisms of methodology and ethics. Some of these criticisms have been addressed by Director Łukasz Kamiński during his tenure and who according to Mink "has made significant changes"; however, Minsk, writing in 2017, was also concerned with the recent administrative and personnel changes in IPN, including the election of Jarosław Szarek as director, which he posits are likely to result in further the politicization of the IPN. According to Valentin Behr, IPN research into the Communist era is valuable, positing that "the resources at its disposal have made it unrivalled as a research centre in the academic world"; at the same time, he said that the research is mostly focused on the era's negative aspects, and that it "is far from producing a critical approach to history, one that asks its own questions and is methodologically pluralistic." He added that in recent years that problem is being ameliorated as the IPN's work "has somewhat diversified as its administration has taken note of criticism on the part of academics."

According to Robert Traba, "under the ... IPN, tasks related to the 'national politics of memory' were – unfortunately – merged with the mission of independent academic research. In the public mind, there could be only one message flowing from the institute's name: memory and history as a science are one. The problem is that nothing could be further from the truth, and nothing could be more misleading. What the IPN’s message presents, in fact, is the danger that Polish history will be grossly over-simplified." Traba states that "at the heart of debate today is a confrontation between those who support traditional methods and categories of research, and those who support newly defined methods and categories. ... Broadening the research perspective means the enrichment of the historian's instrumentarium.'" He puts the IPN research, in a broad sense, in the former; he states that "[a] solid, workshop-oriented, traditional, and positivist historiography ... which defends itself by the integrity of its analysis and its diversified source base" but criticizes its approach for leading to a "falsely conceived mission to find 'objective truth' at the expense of 'serious study of event history', and a 'simplified claim that only 'secret' sources, not accessible to ordinary mortals', can lead to that objective truth." Traba quotes historian Wiktoria Śliwowska, who wrote: "The historian must strive not only to reconstruct a given reality, but also to understand the background of events, the circumstances in which people acted. It is easy to condemn, but difficult to understand a complicated past. ... [Meanwhile, in the IPN] thick volumes are being produced, into which are being thrown, with no real consideration, further evidence in criminating various persons now deceased (and therefore not able to defend themselves), and elderly people still alive – known and unknown." Traba posits that "there is ... a need for genuine debate that does not revolve around [the files] in the IPN archives, 'lustration,' or short-term and politically inspired discussions designed to establish the 'only real' truth", and suggests that adopting varied perspectives and diverse methodologies might contribute to such debate.

During PiS's control of the government between 2005 and 2007, the IPN was the focus of heated public controversies, in particular in regard to the pasts of Solidarity leader Lech Wałęsa and PZPR secretary Wojciech Jaruzelski. As a result, the IPN has been referred to as "a political institution at the centre of 'memory games'".

In 2008, two IPN employees, Sławomir Cenckiewicz and Piotr Gontarczyk, published a book, SB a Lech Wałęsa [pl] (The Security Service and Lech Wałęsa: A Contribution to a Biography) which caused a major controversy. The book's premise was that in the 1970s the Solidarity leader and later president of Poland Lech Wałęsa was a secret informant of the Polish Communist Security Service.

In 2018, the IPN hired Tomasz Greniuch, a historian who in his youth was associated with a far-right group. When he was promoted to a regional director of the Wrocław branch in February 2021, his past came to media attention and resulted in criticism of Greniuch and IPN. Greniuch issued an apology for his past behavior and resigned within weeks.

Organizational and methodological concerns

Valentin Behr writes that the IPN is most "concerned with the production of an official narrative about Poland's recent past" and therefore lacks innovation in its research, while noting that situation is being remedied under recent leadership. He writes that the IPN "has mainly taken in historians from the fringes of the academic field" who were either unable to obtain a prominent academic position or ideologically drawn to the IPN's approach, and that "in the academic field, being an 'IPN historian' can be a stigma"; Behr explains this by pointing to a generational divide in Polish academia, visible when comparing IPN to other Polish research outlets, and claims: "Hiring young historians was done deliberately to give the IPN greater autonomy from the academic world, considered as too leftist to describe the dark sides of the communist regime." He says that the IPN has created opportunities for many history specialists who can carry dedicated research there without the need for an appointment at another institution, and for training young historians, noting that "the IPN is now the leading employer of young PhD students and PhDs in history specialized in contemporary history, ahead of Polish universities".

Historian Dariusz Stola states that the IPN is very bureaucratic in nature, comparing it to a "regular continental European bureaucracy, with usual deficiencies of its kind", and posits that in this aspect the IPN resembles the former Communist institutions it is supposed to deal with, equally "bureaucratic, centralist, heavy, inclined to extensive growth and quantity rather than quality of production".

An incident which caused controversy involved the "Wildstein list", a partial list of persons who allegedly worked for the communist-era Polish intelligence service, copied in 2004 from IPN archives (without IPN permission) by journalist Bronisław Wildstein and published on the Internet in 2005. The list gained much attention in Polish media and politics, and IPN security procedures and handling of the matter came under criticism.

Continent

From Wikipedia, the free encyclopedia
Animated, colour-coded map showing the various continents. Depending on the convention and model, some continents may be consolidated or subdivided.

A continent is any of several large geographical regions. Continents are generally identified by convention rather than any strict criteria. A continent could be a single landmass or a part of a very large landmass, as in the case of Asia or Europe. Due to this, the number of continents varies; up to seven or as few as four geographical regions are commonly regarded as continents. Most English-speaking countries recognize seven regions as continents. In order from largest to smallest in area, these seven regions are Asia, Africa, North America, South America, Antarctica, Europe, and Australia. Different variations with fewer continents merge some of these regions; examples of this are merging North America and South America into America, Asia and Europe into Eurasia, and Africa, Asia, and Europe into Afro-Eurasia.

Oceanic islands are frequently grouped with a nearby continent to divide all the world's land into geographical regions. Under this scheme, most of the island countries and territories in the Pacific Ocean are grouped together with the continent of Australia to form the geographical region Oceania.

In geology, a continent is defined as "one of Earth's major landmasses, including both dry land and continental shelves". The geological continents correspond to seven large areas of continental crust that are found on the tectonic plates, but exclude small continental fragments such as Madagascar that are generally referred to as microcontinents. Continental crust is only known to exist on Earth.

The idea of continental drift gained recognition in the 20th century. It postulates that the current continents formed from the breaking up of a supercontinent (Pangaea) that formed hundreds of millions of years ago.

Definitions and application

By convention, continents "are understood to be large, continuous, discrete masses of land, ideally separated by expanses of water". In modern schemes with five or more recognized continents, at least one pair of continents is joined by land in some fashion. The criterion "large" leads to arbitrary classification: Greenland, with a surface area of 2,166,086 square kilometres (836,330 sq mi), is only considered the world's largest island, while Australia, at 7,617,930 square kilometres (2,941,300 sq mi), is deemed the smallest continent.

Earth's major landmasses all have coasts on a single, continuous World Ocean, which is divided into a number of principal oceanic components by the continents and various geographic criteria.

Extent

The most restricted meaning of continent is that of a continuous area of land or mainland, with the coastline and any land boundaries forming the edge of the continent. In this sense, the term continental Europe (sometimes referred to in Britain as "the Continent") is used to refer to mainland Europe, excluding islands such as Great Britain, Iceland, Ireland, and Malta while the term continent of Australia may refer to the mainland of Australia, excluding New Guinea, Tasmania, and other nearby islands. Similarly, the continental United States refers to "the 49 States (including Alaska but excluding Hawaii) located on the continent of North America, and the District of Columbia."

From the perspective of geology or physical geography, continent may be extended beyond the confines of continuous dry land to include the shallow, submerged adjacent area (the continental shelf) and the islands on the shelf (continental islands), as they are structurally part of the continent.

From this perspective, the edge of the continental shelf is the true edge of the continent, as shorelines vary with changes in sea level. In this sense the islands of Great Britain and Ireland are part of Europe, while Australia and the island of New Guinea together form a continent.

Map of island countries: these states are often grouped geographically with a neighbouring continental landmass

As a cultural construct, the concept of a continent may go beyond the continental shelf to include oceanic islands and continental fragments. In this way, Iceland is considered a part of Europe, and Madagascar a part of Africa. Extrapolating the concept to its extreme, some geographers group the Australian continental landmass with other islands in the Pacific Ocean into one "quasi-continent" called Oceania. This divides the entire land surface of Earth into continents or quasi-continents.

Separation

The criterion that each continent is a discrete landmass is commonly relaxed due to historical conventions and practical use. Of the seven most globally recognized continents, only Antarctica and Australia are completely separated from other continents by the ocean. Several continents are defined not as absolutely distinct bodies but as "more or less discrete masses of land". Africa and Asia are joined by the Isthmus of Suez, and North America and South America by the Isthmus of Panama. In both cases, there is no complete separation of these landmasses by water (disregarding the Suez Canal and the Panama Canal, which are both narrow and shallow, as well as human-made). Both of these isthmuses are very narrow compared to the bulk of the landmasses they unite.

North America and South America are treated as separate continents in the seven-continent model. However, they may also be viewed as a single continent known as America. This viewpoint was common in the United States until World War II, and remains prevalent in some Asian six-continent models. The single American continent model remains a common view in France, Greece, Hungary, Italy, Malta, Portugal, Spain, and Latin American countries.

The criterion of a discrete landmass is completely disregarded if the continuous landmass of Eurasia is classified as two separate continents (Asia and Europe). Physiographically, Europe and the Indian subcontinent are large peninsulas of the Eurasian landmass. However, Europe is considered a continent with its comparatively large land area of 10,180,000 square kilometres (3,930,000 sq mi), while the Indian subcontinent, with less than half that area, is considered a subcontinent. The alternative view—in geology and geography—that Eurasia is a single continent results in a six-continent view of the world. Some view separation of Eurasia into Asia and Europe as a residue of Eurocentrism: "In physical, cultural and historical diversity, China and India are comparable to the entire European landmass, not to a single European country. [...]." However, for historical and cultural reasons, the view of Europe as a separate continent continues in almost all categorizations.

If continents are defined strictly as discrete landmasses, embracing all the contiguous land of a body, then Africa, Asia, and Europe form a single continent which may be referred to as Afro-Eurasia. Combined with the consolidation of the Americas, this would produce a four-continent model consisting of Afro-Eurasia, America, Antarctica, and Australia.

When sea levels were lower during the Pleistocene ice ages, greater areas of continental shelf were exposed as dry land, forming land bridges between Tasmania and the Australian mainland. At those times, Australia and New Guinea were a single, continuous continent known as Sahul. Likewise, Afro-Eurasia and the Americas were joined by the Bering Land Bridge. Other islands, such as Great Britain, were joined to the mainlands of their continents. At that time, there were just three discrete landmasses in the world: Africa-Eurasia-America, Antarctica, and Australia-New Guinea (Sahul).

Number

There are several ways of distinguishing the continents:

Color-coded map showing the various continents. Similar shades exhibit areas that may be consolidated or subdivided.
Number Continents
Four continents     Afro-Eurasia
(Old World or World Island)
   America
(New World)
  Antarctica   Australia
Five continents   Africa    Eurasia    America   Antarctica   Australia
Six continents   Africa    Eurasia   North America   South America   Antarctica   Australia
  Africa   Asia   Europe    America   Antarctica   Australia
Seven continents   Africa   Asia   Europe   North America   South America   Antarctica   Australia

In the English-speaking countries, geographers often use the term Oceania to denote a geographical region which includes most of the island countries and territories in the Pacific Ocean, as well as the continent of Australia.

In some non-English-speaking countries, such as China, Poland, and Russia, Oceania is considered a proper continent because their equivalent word for "continent" has a rather different meaning which can be interpreted as "a major division of land including islands" (leaning towards a region) rather than "land associated with a large landmass" (leaning towards a landmass).

Area and population

The following table provides areas given by Encyclopædia Britannica for each continent in accordance with the seven-continent model, including Australasia along with Melanesia, Micronesia, and Polynesia as parts of Oceania. It also provides populations of continents according to 2021 estimates by the United Nations Statistics Division based on the United Nations geoscheme, which includes all of Egypt (including the Isthmus of Suez and the Sinai Peninsula) as a part of Africa, all of Armenia, Azerbaijan, Cyprus, Georgia, Indonesia, Kazakhstan, and Turkey (including East Thrace) as parts of Asia, all of Russia (including Siberia) as a part of Europe, all of Panama and the United States (including Hawaii) as parts of North America, and all of Chile (including Easter Island) as a part of South America.

Areas and population estimates
Continent Area Population
km2 sq mi % of total land 2021 estimate % of total
Asia 44,614,000 17,226,000 29.6% 4.7 billion 60%
Africa 30,365,000 11,724,000 20.2% 1.4 billion 17%
North America 24,230,000 9,360,000 16.4% 600 million 7.6%
South America 17,814,000 6,878,000 11.9% 430 million 5.6%
Antarctica 14,200,000 5,500,000 9.4% 0 0%
Europe 10,000,000 3,900,000 6.8% 750 million 9.8%
Oceania 8,511,000 3,286,000 5.7% 40 million 0.5%

Not usually considered a continent in certain countries.

Other divisions

Supercontinents

Reconstruction of the supercontinent Pangaea approximately 200 million years ago.

Apart from the current continents, the scope and meaning of the term continent includes past geological ones. Supercontinents, largely in evidence earlier in the geological record, are landmasses that comprise most of the world's cratons or continental cores. These have included Vaalbara, Kenorland, Columbia, Rodinia, Pannotia, and Pangaea. Over time, these supercontinents broke apart into large landmasses which formed the present continents.

Subcontinents

The Indian subcontinent

Certain parts of continents are recognized as subcontinents, especially the large peninsulas separated from the main continental landmass by geographical features. The most widely recognized example is the Indian subcontinent. The Arabian Peninsula, Southern Africa, the Southern Cone of South America, and Alaska in North America might be considered further examples.

In many of these cases, the "subcontinents" concerned are on different tectonic plates from the rest of the continent, providing a geological justification for the terminology. Greenland, generally reckoned as the world's largest island on the northeastern periphery of the North American Plate, is sometimes referred to as a subcontinent. This is a significant departure from the more conventional view of a subcontinent as comprising a very large peninsula on the fringe of a continent.

Where the Americas are viewed as a single continent (America), it is divided into two subcontinents (North America and South America) or three (Central America being the third). When Eurasia is regarded as a single continent, Asia and Europe are treated as subcontinents.

Submerged continents

Zealandia, the largest submerged landmass or continent

Some areas of continental crust are largely covered by the ocean and may be considered submerged continents. Notable examples are Zealandia, emerging from the ocean primarily in New Zealand and New Caledonia, and the almost completely submerged Kerguelen Plateau in the southern Indian Ocean.

Microcontinents

Some islands lie on sections of continental crust that have rifted and drifted apart from a main continental landmass. While not considered continents because of their relatively small size, they may be considered microcontinents. Madagascar, the largest example, is usually considered an island of Africa, but its divergent evolution has caused it to be referred to as "the eighth continent" from a biological perspective.

Geological continents

Geologists use four key attributes to define a continent:

  1. Elevation – The landmass, whether dry or submerged beneath the ocean, should be elevated above the surrounding ocean crust.
  2. Geology – The landmass should contain different types of rock: igneous, metamorphic, and sedimentary.
  3. Crustal structure – The landmass should consist of the continental crust, which is thicker and has a lower seismic velocity than the oceanic crust.
  4. Limits and area – The landmass should have clearly-defined boundaries and an area of more than one million square kilometres.

With the addition of Zealandia in 2017, Earth currently has seven recognized geological continents: Africa, Antarctica, Australia, Eurasia, North America, South America, and Zealandia. Due to lacking the presence of Precambrian cratonic rocks, Zealandia's status as a geological continent has been disputed by some geologists. However, a study conducted in 2021 found that part of the submerged continent is indeed Precambrian, twice as old as geologists had previously thought, which is further evidence that supports the idea of Zealandia being a geological continent.

All seven geological continents are spatially isolated by geologic features.

History of the concept

Early concepts of the Old World continents

The Ancient Greek geographer Strabo holding a globe showing Europa and Asia

The term "continent" translates the Greek word ἤπειρος, meaning "landmass, terra firma", the proper name of Epirus and later especially used for Asia (i.e. Asia Minor).

The first distinction between continents was made by ancient Greek mariners who gave the names Europe and Asia to the lands on either side of the waterways of the Aegean Sea, the Dardanelles strait, the Sea of Marmara, the Bosporus strait and the Black Sea. The names were first applied just to lands near the coast and only later extended to include the hinterlands. But the division was only carried through to the end of navigable waterways and "... beyond that point the Hellenic geographers never succeeded in laying their finger on any inland feature in the physical landscape that could offer any convincing line for partitioning an indivisible Eurasia ..."

Ancient Greek thinkers subsequently debated whether Africa (then called Libya) should be considered part of Asia or a third part of the world. Division into three parts eventually came to predominate. From the Greek viewpoint, the Aegean Sea was the center of the world; Asia lay to the east, Europe to the north and west, and Africa to the south. The boundaries between the continents were not fixed. Early on, the Europe–Asia boundary was taken to run from the Black Sea along the Rioni River (known then as the Phasis) in Georgia. Later it was viewed as running from the Black Sea through Kerch Strait, the Sea of Azov and along the Don River (known then as the Tanais) in Russia. The boundary between Asia and Africa was generally taken to be the Nile River. Herodotus in the 5th century BC objected to the whole of Egypt being split between Asia and Africa ("Libya") and took the boundary to lie along the western border of Egypt, regarding Egypt as part of Asia. He also questioned the division into three of what is really a single landmass, a debate that continues nearly two and a half millennia later.

Eratosthenes, in the 3rd century BC, noted that some geographers divided the continents by rivers (the Nile and the Don), thus considering them "islands". Others divided the continents by isthmuses, calling the continents "peninsulas". These latter geographers set the border between Europe and Asia at the isthmus between the Black Sea and the Caspian Sea, and the border between Asia and Africa at the isthmus between the Red Sea and the mouth of Lake Bardawil on the Mediterranean Sea.

Medieval T and O map showing the three continents as domains of the sons of Noah—Asia to Sem (Shem), Europe to Iafeth (Japheth), and Africa to Cham (Ham).

There was no sense of continental identity within the Roman Empire. However, following the fall of the Western Roman Empire, the culture that developed in its place, linked to Latin and the Catholic church, began to associate itself with the concept of "Europe". Through the Roman period and the Middle Ages, a few writers took the Isthmus of Suez as the boundary between Asia and Africa, but most writers continued to consider it the Nile or the western border of Egypt (Gibbon). In the Middle Ages, the world was usually portrayed on T and O maps, with the T representing the waters dividing the three continents. By the middle of the 18th century, "the fashion of dividing Asia and Africa at the Nile, or at the Great Catabathmus [the boundary between Egypt and Libya] farther west, had even then scarcely passed away".

European arrival in the Americas

Christopher Columbus sailed across the Atlantic Ocean to the Caribbean in 1492, sparking a period of European exploration of the Americas. But despite four voyages to the Americas, Columbus never believed he had reached a new continent—he always thought it was part of Asia.

In 1501, Amerigo Vespucci and Gonçalo Coelho attempted to sail around what they considered the southern end of the Asian mainland into the Indian Ocean, passing through Fernando de Noronha. After reaching the coast of Brazil, they sailed along the coast of South America much farther south than Asia was known to extend, confirming that this was a land of continental proportions. On return to Europe, an account of the voyage, called Mundus Novus ("New World"), was published under Vespucci's name in 1502 or 1503, although it seems that it had additions or alterations by another writer. Regardless of who penned the words, Mundus Novus credited Vespucci with saying, "I have discovered a continent in those southern regions that is inhabited by more numerous people and animals than our Europe, or Asia or Africa", the first known explicit identification of part of the Americas as a continent like the other three.

Within a few years, the name "New World" began appearing as a name for South America on world maps, such as the Oliveriana (Pesaro) map of around 1504–1505. Maps of this time, though, still showed North America connected to Asia and showed South America as a separate land.

Universalis Cosmographia, Waldseemüller's 1507 world map—the first to show the Americas separate from Asia

In 1507 Martin Waldseemüller published a world map, Universalis Cosmographia, which was the first to show North and South America as separate from Asia and surrounded by water. A small inset map above the main map explicitly showed for the first time the Americas being east of Asia and separated from Asia by an ocean, as opposed to just placing the Americas on the left end of the map and Asia on the right end. In the accompanying book Cosmographiae Introductio, Waldseemüller noted that the earth is divided into four parts, Europe, Asia, Africa, and the fourth part, which he named "America" after Amerigo Vespucci's first name. On the map, the word "America" was placed on part of South America.

The word continent

From the 16th century the English noun continent was derived from the term continent land, meaning continuous or connected land and translated from the Latin terra continens. The noun was used to mean "a connected or continuous tract of land" or mainland. It was not applied only to very large areas of land—in the 17th century, references were made to the continents (or mainlands) of Isle of Man, Ireland and Wales and in 1745 to Sumatra. The word continent was used in translating Greek and Latin writings about the three "parts" of the world, although in the original languages no word of exactly the same meaning as continent was used.

While continent was used on the one hand for relatively small areas of continuous land, on the other hand geographers again raised Herodotus's query about why a single large landmass should be divided into separate continents. In the mid-17th century, Peter Heylin wrote in his Cosmographie that "A Continent is a great quantity of Land, not separated by any Sea from the rest of the World, as the whole Continent of Europe, Asia, Africa." In 1727, Ephraim Chambers wrote in his Cyclopædia, "The world is ordinarily divided into two grand continents: the old and the new." And in his 1752 atlas, Emanuel Bowen defined a continent as "a large space of dry land comprehending many countries all joined together, without any separation by water. Thus Europe, Asia, and Africa is one great continent, as America is another." However, the old idea of Europe, Asia and Africa as "parts" of the world ultimately persisted with these being regarded as separate continents.

Beyond four continents

The Sanskrit text Rig Veda often dated 1500 BCE has the earliest mention of seven continents in the Earth, the text claims that the Earth has seven continents and Lord Vishnu Measured the entire universe from his first foot from the land of Earth which has 7 continents.

ato devā avantu no yato viṣṇurvicakrame |
pṛthivyāḥ saptadhāmabhiḥ ||

idaṃ viṣṇurvi cakrame tredhā ni dadhe padam |
samūḷhamasya pāṃsure ||

trīṇi padā vi cakrame viṣṇurghopā adābhyaḥ |
ato dharmāṇi dhārayan ||

The Gods be gracious unto us even from the place whence Vishnu strode
Through the seven regions of the earth!

Through all this world strode Vishnu; thrice his foot he planted, and the whole
Was gathered in his footstep's dust.

Vishnu, the Guardian, he whom none deceiveth, made three steps; thenceforth
Establishing his high decrees.

—RigVeda transliteration of Book 1, Hymn 22, Verses 16-18 —RigVeda translation by Ralph T.H. Griffith (1896) of Book 1, Hymn 22, Verses 16–18
Rigveda page in Sanskrit

In regard to the above-quoted verses, it is commonly accepted that there are Seven Continents or 'regions of the earth'. A. Glucklich adds that 'In the Matsya Purana, for instance, there is a seven-part map of the world ... [it has] one centre, where an immense mountain – Mount Meru (or Maha Meru, Great Meru) – stands ... The continents encircle the mountain in seven concentric circles ... It seems clear that the Himalayas were the approximate location of Mt. Meru and the text is clear that the earth has seven continents.

Hollandia Nova, 1659 map prepared by Joan Blaeu based on voyages by Abel Tasman and Willem Jansz, this image shows a French edition of 1663

From the late 18th century, some geographers started to regard North America and South America as two parts of the world, making five parts in total. Overall though, the fourfold division prevailed well into the 19th century.

Europeans discovered Australia in 1606, but for some time it was taken as part of Asia. By the late 18th century, some geographers considered it a continent in its own right, making it the sixth (or fifth for those still taking America as a single continent). In 1813, Samuel Butler wrote of Australia as "New Holland, an immense island, which some geographers dignify with the appellation of another continent" and the Oxford English Dictionary was just as equivocal some decades later. It was in the 1950s that the concept of Oceania as a "great division" of the world was replaced by the concept of Australia as a continent.

Antarctica was sighted in 1820 during the First Russian Antarctic Expedition and described as a continent by Charles Wilkes on the United States Exploring Expedition in 1838, the last continent identified, although a great "Antarctic" (antipodean) landmass had been anticipated for millennia. An 1849 atlas labelled Antarctica as a continent but few atlases did so until after World War II.

Over time, the western concept of dividing the world into continents spread globally, replacing conceptions in other areas of the world. The idea of continents continued to become imbued with cultural and political meaning. In the 19th century during the Meiji period, Japanese leaders began to self-identify with the concept of being Asian, and renew relations with other "Asian" countries while conceiving of the idea of Asian solidarity against western countries. This conception of an Asian identity, as well as the idea of Asian solidarity, was later taken up by others in the region, such as Republican China and Vietnam.

From the mid-19th century, atlases published in the United States more commonly treated North and South America as separate continents, while atlases published in Europe usually considered them one continent. However, it was still not uncommon for American atlases to treat them as one continent up until World War II. From the 1950s, most U.S. geographers divided the Americas into two continents. With the addition of Antarctica, this made the seven-continent model. However, this division of the Americas never appealed to Latin Americans, who saw their region spanning an América as a single landmass, and there the conception of six continents remains dominant, as it does in scattered other countries.

Some geographers regard Europe and Asia together as a single continent, dubbed Eurasia. In this model, the world is divided into six continents, with North America and South America considered separate continents.

Geology

Geologists use the term continent in a different manner from geographers. In geology, a continent is defined by continental crust, which is a platform of metamorphic and igneous rock, largely of granitic composition. Continental crust is less dense and much thicker than oceanic crust, which causes it to "float" higher than oceanic crust on the dense underlying mantle. This explains why the continents form high platforms surrounded by deep ocean basins.

Some geologists restrict the term continent to portions of the crust built around stable regions called cratons. Cratons have largely been unaffected by mountain-building events (orogenies) since the Precambrian. A craton typically consists of a continental shield surrounded by a continental platform. The shield is a region where ancient crystalline basement rock (typically 1.5 to 3.8 billion years old) is widely exposed at the surface. The platform surrounding the shield is also composed of ancient basement rock, but with a cover of younger sedimentary rock. The continents are accretionary crustal "rafts" that, unlike the denser basaltic crust of the ocean basins, are not subjected to destruction through the plate tectonic process of subduction. This accounts for the great age of the rocks comprising the continental cratons.

The margins of geologic continents are either active or passive. An active margin is characterised by mountain building, either through a continent-on continent collision or a subduction zone. Continents grow by accreting lighter volcanic island chains and microcontinents along these active margins, forming orogens. At a passive margin, the continental crust is stretched thin by extension to form a continental shelf, which tapers off with a gradual slope covered in sediment, connecting it directly to the oceanic crust beyond. Most passive margins eventually transition into active margins: where the oceanic plate becomes too heavy due to cooling, it disconnects from the continental crust, and starts subducting below it, forming a new subduction zone.

Principal tectonic plates of the continents and the floor of the oceans

There are many microcontinents, or continental fragments, that are built of continental crust but do not contain a craton. Some of these are fragments of Gondwana or other ancient cratonic continents: Zealandia, which includes New Zealand and New Caledonia; Madagascar; the northern Mascarene Plateau, which includes the Seychelles. Other islands, such as several in the Caribbean Sea, are composed largely of granitic rock as well, but all continents contain both granitic and basaltic crust, and there is no clear boundary as to which islands would be considered microcontinents under such a definition. The Kerguelen Plateau, for example, is largely volcanic, but is associated with the breakup of Gondwanaland and is considered a microcontinent, whereas volcanic Iceland and Hawaii are not. The British Isles, Sri Lanka, Borneo, and Newfoundland were on the margins of the Laurasian continent—only separated from the main continental landmass by inland seas flooding its margins.

The movement of plates has caused the continual formation and breakup of continents, and occasionally supercontinents, in a process called the Wilson Cycle. The supercontinent Columbia or Nuna formed during a period of 2.0–1.8 billion years ago and broke up about 1.5–1.3 billion years ago. The supercontinent Rodinia is thought to have formed about 1 billion years ago and to have embodied most or all of Earth's continents, and broken up into eight continents around 600 million years ago. The eight continents later reassembled into another supercontinent called Pangaea; Pangaea broke up into Laurasia (which became North America and Eurasia) and Gondwana (which became the remaining continents).

Cellular automaton

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