Pabedaan antaro revisi dari "Teori Malapatako Toba"

Konten dihapus Konten ditambahkan
Algazel (rundiang | jariah)
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Algazel (rundiang | jariah)
k tajamah infobox
Barih 14:
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| map-caption = [[Danau Toba]] adolah [[danau kawah]] nan tabantuak.
| impact = Second-most[[Gunuang barapi super|Latuihan super]] kaduo paliang recentbaru [[supervolcano#known supereruptions|supereruption]]; plungedmaakibaikan [[EarthBumi]] into 6 years ofmangalami [[volcanicmusim winterdingin vulkanik]] salamo 6 taun, possiblybakamungkinan significantjo changesparubahan tosignifikan regionalpado [[topographytopografi]] wilayah.<ref name="SavinoJones2007">{{cite book|author1=John Savino|author2=Marie D. Jones|title=Supervolcano: The Catastrophic Event That Changed the Course of Human History: Could Yellowstone Be Next|url=https://books.google.com/books?id=tSIa0VQn1NQC&pg=PA140|year=2007|publisher=Career Press|isbn=978-1-56414-953-4|page=140}}</ref>{{update after|2013|6|9}}
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Latuihan gadang Toba iolah [[Jinih latuihan gunuang barapi|erupsi]] ''[[Gunuang barapi super|Supervolcano]]'' nan balaku antaro 69,000 inggo 77,000 taun dulu, ditampek mano talataknyo [[Danau Toba]], di [[Sumatra]], [[Indonesia]], kini. Iko marupoan salah satu dari [[Daftar latuihan gunuang barapi gadang|latuihan tagadang]] di [[Bumi]]. '''Teori Malapatako Toba''' manyatoan paristiwa iko maakibaikan tajadinyo [[musim dingin vulkanik]] di dunia salamo 6–10 taun jo kamungkinan tajadinyo wakatu sajuak sudah tu salamo 1,000 taun.