Gunung Tambora: Béda antara owahan

Gunung mapan ana ing sisih lor lan kidul yaiku awujud [[kerak oseanik]].<ref name="Degens1989"/> Tambora kabentuk dening [[Subduksi|zona subduksi]] ana ing ngisore.<ref name="Degens1989"/> Perkara iki ingkatake ketinggian 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 ndadekake gunung iki tau dadi salah siji puncak paling dhuwur ana ing [[Nusantara]] lan mededi [[dapur magma]] kang gedhe ing gunung iki.<ref name="Degens1989"/> Mbutuhake wektu seabad kanggo ngisi meneh [[dapur magma]] kang ana ing gunung iki. <ref name="Degens1989"/>▼

Aktivitas vulkanik gunung iki ana ing pucuke nalika sasi [[April]] taun [[1815]] nalika kuwi gunung iki mbledos 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> Bledosan iki dadi bledosan paling gedhe nalika ana letusan [[danau 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 (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> ▼