Pabedaan antaro revisi dari "Eurasia"

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'''Eurasia''' adolah [[banua]] paliang gadang di [[bumi]] nan marupokan gabuangan dari [[Eropa]] jo [[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> 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, sarato Afrika, [[Lauik Mediterania]], jo [[Lautan Hindia]] di selatan.<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> Pambagian antaro duo banua, Eropa jo Asia, tajadi dek konstruksi sijarah sosial di kaduo banua ko, sadangkan indak ado bateh jaleh sacaro fisik di antaro kaduonyo inggo tasabuik 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'').<ref name="NatlGeo" /> Namun, kakakuan Eurasia masih dipadebatkan manuruik data paleomagnetik.<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>