Pabedaan antaro revisi dari "Danau Toba"
Konten dihapus Konten ditambahkan
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kambang |
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Barih 34:
Akikaik nan erupsi Toba mambawo pado sabuah [[musim dingin vulkanik]] nan sataruihnyo manjadian suhu dunia bakurang antaro {{Convert|3|to|5|C-change|F-change}}, inggo {{Convert|15|C-change|F-change}} di latitud tinngi, lah ditarimo. Panilitian di [[Danau Malawi]] di Afrika Timur manunjuakan jumlah endapan abu dari Toba nan signifikan, tapi indak jo tando parubahan cuaco di Afrika Timur.<ref>{{cite journal|last=Lane|first=Christine S.|author2=Ben T. Chorn |author3=Thomas C. Johnson |date=29 April 2013|title=Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka|journal=Proceedings of the National Academy of Sciences|volume=110|issue=20|pages=8025–8029|url=http://www.pnas.org/content/110/20/8025.abstract?sid=b5741029-8930-4895-aacc-1c527df5e9be|bibcode = 2013PNAS..110.8025L |doi = 10.1073/pnas.1301474110 }}</ref>
== Geologi ==
[[File:Lake Toba, North Sumatra (71).JPG|thumb|Batu Gantung di Danau Toba]]
Kompleks [[kaldera]] Toba [[caldera]] di [[Sumatra Utara]] dibantuak dek ampek kawah gunuang barapi tatindiah nan babatehanan jo "barisan gunuang barapi" Sumatra. Kaldera nan paliang mudo jo nan kaampek marupoan kaldera [[Kuartener]] nan tagadang di dunia ({{convert|100|by|30|km|abbr=on}}) jo maminteh katigo-tigo kaldera nan labiah tuo.
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{{wide image|Lake Toba banner.jpg|1000px|Pamandangan panorama Danau Toba|left}}
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