Gunung Tambora: Béda antara owahan
Konten dihapus Konten ditambahkan
Tanpa ringkesan besutan |
Tanpa ringkesan besutan |
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Larik 36:
| [[Pinatubo]] || [[1991]] || align="center" | 34 || align="center" | 6 || align="center" | −0,5 || 1202
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| colspan=6 | <span style="font-size:smaller;">Sumber: Oppenheimer (2003),<ref name="Oppenheimer2003">{{cite journal|last=Oppenheimer|first=Clive|title=Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (Indonesia) 1815|journal=Progress in Physical Geography|volume=27|issue=2|date=2003|pages=230–259|url=http://dx.doi.org/10.1191/0309133303pp379ra}}</ref> dan ''Smithsonian Global Volcanism Program'' untuk VEI.</ref>{{cite web|title=Large Holocene Eruptions|publisher=[[Smithsonian Institution]]|work=Global Volcanism Program|accessdate=7 November|accessyear=2006|url=http://www.volcano.si.edu/world/largeeruptions.cfm}}</ref></span>
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