Pabedaan antaro revisi dari "Teori Malapatako Toba"

Konten dihapus Konten ditambahkan
Algazel (rundiang | jariah)
k tajamah infobox
Algazel (rundiang | jariah)
k susun latak
Barih 3:
| photo = Image:Tobaeruption.png
| photo-size =
| caption = Gamba baa latuihan balaku dari kiro-kiro {{convert|42|km|btmi}} ateh [[Pulau Simeulue]].
| date = 74,100—75,900 taun dulu
| volcano = [[Danau Toba|Gunuang barapi super Toba]]
Barih 16:
| impact = [[Gunuang barapi super|Latuihan super]] kaduo paliang baru [[supervolcano#known supereruptions|supereruption]]; maakibaikan [[Bumi]] mangalami [[musim dingin vulkanik]] salamo 6 taun, bakamungkinan jo parubahan signifikan pado [[topografi]] 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}}
}}
{{clr}}
 
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.