Pabedaan antaro revisi dari "Eurasia"

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←Mambuek laman baisi "{{Tarjamah}} '''Eurasia''' ({{IPAc-en|j|ʊəˈr|eɪ|ʒ|ə}}) is the largest continental area on Earth, comprising all of Europe and Asia.<ref>{..."
 
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'''Eurasia''' ({{IPAc-en|j|ʊəˈr|eɪ|ʒ|ə}}) adolah banua paliang gadang di bumi nan marupokan gabuangan dari Eropa jo Asia. Utamonyo di balahan bumi utara jo timur, mambantang dari Kapulauan Britania jo Samananjuang Iberia di barat inggo ka Kapulauan Japang jo Indonesia di timur. Daratannyo dibatehi Lautan Atlantik jo Afrika di barat, Lautan Pasifik di timur, Lautan Arktik di utara, jo Afrika, Lauik Mediterania, sarato Lautan Hindia di selatan. Pambagian antaro duo banua, Eropa jo Asia, tajadi dek konstruksi sijarak sosial di kaduo banua ko, sadangkan indak ado bateh jaleh nan mambateh sacaro fisik di antaro kaduonyo sainggo disabuik sabagai banua paliang gadang dari anam, limo, atau ampek banua di bumi (bagantuang pado pambagian banua nan dianuik). Dalam geologi, Eurasia acok dianggap sabagai daratan gadang nan kaku (''a single rigid megablock''). Namun, kakakuan Eurasia masih dipadebatkan manuruik data paleomagnetik.
'''Eurasia''' ({{IPAc-en|j|ʊəˈr|eɪ|ʒ|ə}}) is the largest [[Continent|continental]] area on [[Earth]], comprising all of [[Europe]] and [[Asia]].<ref>{{cite web|url=http://www.geolsoc.org.uk/en/Education%20and%20Careers/Ask%20a%20Geologist/Continents%20Supercontinents%20and%20the%20Earths%20Crust/Continental%20Divide|title=Continental Divide|last=Nield|first=Ted|work=Geological Society|archive-url=https://web.archive.org/web/20131203005136/http://www.geolsoc.org.uk/en/Education%20and%20Careers/Ask%20a%20Geologist/Continents%20Supercontinents%20and%20the%20Earths%20Crust/Continental%20Divide|archive-date=3 December 2013|access-date=8 August 2012|url-status=live}}</ref><ref name="NatlGeo">{{cite web|url=https://www.nationalgeographic.org/encyclopedia/continent/|title=How many continents are there?|publisher=[[National Geographic Society]]|archive-url=https://web.archive.org/web/20190716045120/https://www.nationalgeographic.org/encyclopedia/continent/|archive-date=16 July 2019|access-date=27 July 2017|quote=By convention there are seven continents: [[Asia]], [[Africa]], [[North America]], [[South America]], [[Europe]], [[Australia (continent)|Australia]], and [[Antarctica]]. Some geographers list only six continents, combining [[Europe]] and [[Asia]] into Eurasia. In parts of the world, students learn that there are just five continents: Eurasia, Australia (Oceania), Africa, Antarctica, and the [[Americas]].}}</ref> Primarily in the [[Northern Hemisphere|Northern]] and [[Eastern Hemisphere|Eastern Hemispheres]], it spans from the [[British Isles]] and the [[Iberian Peninsula]] in the west to the [[Japanese archipelago]] in the east. The continental landmass is bordered by the [[Atlantic Ocean]] and [[Africa]] to the west, the [[Pacific Ocean]] to the east, the [[Arctic Ocean]] to the north, and by [[Africa]], the [[Mediterranean Sea]], and the [[Indian Ocean]] to the south.<ref>{{cite web|url=http://geography.about.com/od/learnabouttheearth/a/What-Is-Eurasia.htm|title=What is Eurasia?|publisher=geography.about.com|archive-url=https://web.archive.org/web/20121118165606/http://geography.about.com/od/learnabouttheearth/a/What-Is-Eurasia.htm|archive-date=18 November 2012|access-date=17 December 2012|url-status=live}}</ref> The division between Europe and Asia as two continents is a historical [[social construct]], as they have no clear physical separation between them; thus, in some parts of the world, Eurasia is recognized as the largest of the six, five, or four continents on [[Earth]].<ref name="NatlGeo" /> In geology, Eurasia is often considered as a single rigid megablock. However, the rigidity of Eurasia is debated based on [[paleomagnetic]] data.<ref>{{Cite journal|last=Pavlov|first=V.E.|year=2012|title=Siberian Paleomagnetic Data and the Problem of Rigidity of the Northern Eurasian Continent in the Post Paleozoic|journal=Izvestiya, Physics of the Solid Earth|volume=48|issue=9–10|pages=721–737|bibcode=2012IzPSE..48..721P|doi=10.1134/S1069351312080022|s2cid=129745964}}</ref><ref>{{Cite journal|last1=Li|first1=Yong-Xiang|last2=Shu|first2=Liangshu|last3=Wen|first3=Bin|last4=Yang|first4=Zhenyu|last5=Ali|first5=Jason R.|date=1 September 2013|title=Magnetic inclination shallowing problem and the issue of Eurasia's rigidity: insights following a palaeomagnetic study of upper Cretaceous basalts and redbeds from SE China|journal=Geophysical Journal International|language=en|volume=194|issue=3|pages=1374–1389|bibcode=2013GeoJI.194.1374L|doi=10.1093/gji/ggt181|issn=0956-540X|doi-access=free}}</ref>
 
Eurasia malingkuangi 36,2% total area tanah di Bumi, sarato tampek untuak nagara paliang laweh di dunia, Rusia. Daratannyo diuni labiah dari 5 miliar urang, sarupo 70% populasi manusia. Manusia partamo alah mauni Eurasia antaro 60.000 inggo 125.000 taun nan lalu. Banyak pulau gadang cando Britania Raya, Islandia, Irlandia, jo Sri Lanka, ataupun Japang, Filipina, jo sabagian gadang pulau Indonesia, acok dimasuakkan dalam Eurasia, walaupun tapisah dari kasinambuangan dareknyo.
 
Sacaro fisiografi, Eurasia marupokan ciek banua. Konsep Eropa jo Asia sabagai banua nan tapisah
 
'''Eurasia''' ({{IPAc-en|j|ʊəˈr|eɪ|ʒ|ə}}) is the largest [[Continent|continental]] area on [[Earth]], comprising all of [[Europe]] and [[Asia]].<ref>{{cite web|url=http://www.geolsoc.org.uk/en/Education%20and%20Careers/Ask%20a%20Geologist/Continents%20Supercontinents%20and%20the%20Earths%20Crust/Continental%20Divide|title=Continental Divide|last=Nield|first=Ted|work=Geological Society|archive-url=https://web.archive.org/web/20131203005136/http://www.geolsoc.org.uk/en/Education%20and%20Careers/Ask%20a%20Geologist/Continents%20Supercontinents%20and%20the%20Earths%20Crust/Continental%20Divide|archive-date=3 December 2013|access-date=8 August 2012|url-status=live}}</ref><ref name="NatlGeo">{{cite web|url=https://www.nationalgeographic.org/encyclopedia/continent/|title=How many continents are there?|publisher=[[National Geographic Society]]|archive-url=https://web.archive.org/web/20190716045120/https://www.nationalgeographic.org/encyclopedia/continent/|archive-date=16 July 2019|access-date=27 July 2017|quote=By convention there are seven continents: [[Asia]], [[Africa]], [[North America]], [[South America]], [[Europe]], [[Australia (continent)|Australia]], and [[Antarctica]]. Some geographers list only six continents, combining [[Europe]] and [[Asia]] into Eurasia. In parts of the world, students learn that there are just five continents: Eurasia, Australia (Oceania), Africa, Antarctica, and the [[Americas]].}}</ref> Primarily in the [[Northern Hemisphere|Northern]] and [[Eastern Hemisphere|Eastern Hemispheres]], it spans from the [[British Isles]] and the [[Iberian Peninsula]] in the west to the [[Japanese archipelago]] in the east. The continental landmass is bordered by the [[Atlantic Ocean]] and [[Africa]] to the west, the [[Pacific Ocean]] to the east, the [[Arctic Ocean]] to the north, and by [[Africa]], the [[Mediterranean Sea]], and the [[Indian Ocean]] to the south.<ref>{{cite web|url=http://geography.about.com/od/learnabouttheearth/a/What-Is-Eurasia.htm|title=What is Eurasia?|publisher=geography.about.com|archive-url=https://web.archive.org/web/20121118165606/http://geography.about.com/od/learnabouttheearth/a/What-Is-Eurasia.htm|archive-date=18 November 2012|access-date=17 December 2012|url-status=live}}</ref> The division between Europe and Asia as two continents is a historical [[social construct]], as they have no clear physical separation between them; thus, in some parts of the world, Eurasia is recognized as the largest of the six, five, or four continents on [[Earth]].<ref name="NatlGeo" /> In geology, Eurasia is often considered as a single rigid megablock. However, the rigidity of Eurasia is debated based on [[paleomagnetic]] data.<ref>{{Cite journal|last=Pavlov|first=V.E.|year=2012|title=Siberian Paleomagnetic Data and the Problem of Rigidity of the Northern Eurasian Continent in the Post Paleozoic|journal=Izvestiya, Physics of the Solid Earth|volume=48|issue=9–10|pages=721–737|bibcode=2012IzPSE..48..721P|doi=10.1134/S1069351312080022|s2cid=129745964}}</ref><ref>{{Cite journal|last1=Li|first1=Yong-Xiang|last2=Shu|first2=Liangshu|last3=Wen|first3=Bin|last4=Yang|first4=Zhenyu|last5=Ali|first5=Jason R.|date=1 September 2013|title=Magnetic inclination shallowing problem and the issue of Eurasia's rigidity: insights following a palaeomagnetic study of upper Cretaceous basalts and redbeds from SE China|journal=Geophysical Journal International|language=en|volume=194|issue=3|pages=1374–1389|bibcode=2013GeoJI.194.1374L|doi=10.1093/gji/ggt181|issn=0956-540X|doi-access=free}}</ref>
 
Eurasia covers around {{convert|55,000,000|km2|mi2}}, or around 36.2% of the [[Earth]]'s total land area; and is home to the [[List of countries and dependencies by area|largest country in the world]], [[Russia]]. The landmass contains well over 5&nbsp;billion people, equating to approximately 70% of the [[human population]]. Humans first settled in Eurasia between 60,000 and 125,000 years ago. Some major islands, including [[Great Britain]], [[Iceland]], [[Ireland]], and [[Sri Lanka]], as well as those of [[Japan]], the [[Philippines]], and most of [[Indonesia]], are often included in the popular definition of Eurasia, despite being separate from the contiguous landmass.