Gunung Tambora: Béda antara owahan

Konten dihapus Konten ditambahkan
Arupako (parembugan | pasumbang)
c →‎top: éjaan, replaced: yaiku → ya iku (3) using AWB
Arupako (parembugan | pasumbang)
c éjaan, replaced: Indonesia → Indonésia (7) using AWB
Larik 1:
[[Gambar:tambora volc.jpg|thumb|right|300px|Pasawangan gunung Tambora]]
[[File:Caldera Mt Tambora Sumbawa IndonesiaIndonésia.jpg|thumb|300px|Kawah Gunung Tambora.]]
{{Infobox Gunung
|nama=Tambora
|gambar=Caldera Mt Tambora Sumbawa IndonesiaIndonésia.jpg
|caption=[[Kaldera]] Gunung Tambora
|lokasi=[[Kepulauan Sunda Kecil]], [[IndonesiaIndonésia]])
|negara=IndonesiaIndonésia
|kota=[[Yogyakarta]]
|tipe=[[stratovolcano]]
Larik 18:
Gunung mapan ana ing sisih lor lan kidul ya iku awujud [[kerak oseanik]].<ref name="Degens1989"/> Tambora kabentuk déning [[Subduksi|zona subduksi]] ana ing ngisoré.<ref name="Degens1989"/> Perkara iki ningkataké kadhuwuran Tambora nganti tekan 4.300 [[meter|m]]<ref name="Stothers1984">{{cite journal|last=Stothers|first=Richard B.| journal=[[Science]]|title=The Great Tambora Eruption in 1815 and Its Aftermath| volume =224|issue=4654|date=1984|pages=1191–1198|url= http://dx.doi.org/10.1126/science.224.4654.1191}}</ref> kang ndadèkaké gunung iki tau dadi salah siji puncak paling dhuwur ana ing [[Nusantara]] lan mededi [[dapur magma]] kang gedhé ing gunung iki.<ref name="Degens1989"/> Mbutuhaké wektu saabad kanggo ngisi menèh [[dapur magma]] kang ana ing gunung iki.<ref name="Degens1989"/>
 
Aktivitas vulkanik gunung iki ana ing pucuké nalika sasi [[April]] taun [[1815]] nalika iku gunung iki mbledhos ana ing skala pitu [[Volcanic Explosivity Index]].<ref name="Degens1989">{{cite journal|last=Degens|first=E.T.|coauthors=Buch, B|title=Sedimentological events in Saleh Bay, off Mount Tambora|journal=Netherlands Journal of Sea Research|volume=24|issue=4|url= http://dx.doi.org/10.1016/0077-7579(89)90117-8|pages=399–404|date =1989}}</ref> Bledhosan iki dadi bledhosan paling gedhé nalika ana jeblugan [[tlaga Taupo]] taun [[1815]].<ref name="Oppenheimer2003">{{cite journal|last=Oppenheimer|first=Clive|title=Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (IndonesiaIndonésia) 1815|journal=Progress in Physical Geography|volume=27|issue=2|date=2003|pages=230–259|url=http://dx.doi.org/10.1191/0309133303pp379ra}}</ref>
 
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Larik 50:
| [[Pinatubo]] || [[1991]] || align="center" | 34 || align="center" | 6 || align="center" | −0,5 || 1202
|-
| 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 (IndonesiaIndonésia) 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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Larik 58:
 
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[[Kategori:IndonesiaIndonésia]]