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Mount Sinabung is a Pleistocene-to-Holocene stratovolcano. [11] It is located in a relatively cool area on a fertile plateau with mountains bounding the north. [12] The summit crater of the volcano has a complex, longer form due to vents migrating on the N-S line. [11]
Mount Sinabung [22] 2,460 8,070 21 East Nusa Tenggara: Mount Mutis [23] 2,427 7,963 22 ... Mount Parung [41] 687 2,254 37 South Papua: slope of Star Mountains [42] 310
The 1815 eruption of Mount Tambora on Sumbawa and the 1257 eruption of Mount Samalas on Lombok were among the largest in the last two millennia, ranking 7 on the VEI scale. [14] The Sunda Arc subduction zone was also the site of one of the largest known eruptions of the Cenozoic , the VEI 8 Toba supereruption on Sumatra , which expelled 2,800 ...
Mount Sinabung in North Sumatra province was shooting smoke and ash as high as 1,000 meters (3,280 feet) into the air and hot ash clouds were blowing 3 kilometers (1.8 miles) to the southeast ...
In this long-exposure photo by Binsar Bakkara, hot lava flows from the crater of Mount Sinabung as seen from a location about 6 kilometers (3.7 miles) from the volcano, in Tiga Kicat, in Indonesia ...
For full definitions and explanations of topographic prominence, key col, and parent, see topographic prominence. In particular, the different definitions of the parent of a peak are addressed at length in that article. Height on the other hand simply means elevation of the summit above sea level.
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