Talk:Mount Sinabung

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WikiProject class rating[edit]

This article was automatically assessed because at least one WikiProject had rated the article as stub, and the rating on other projects was brought up to Stub class. BetacommandBot 05:59, 10 November 2007 (UTC)[reply]

Rename?[edit]

Should this article be moved to Mount Sinabung over the redirect? 64.85.223.249 (talk) 12:26, 29 August 2010 (UTC)[reply]

Yes, see Mount Etna and the translation of the Indonesia Gunung Sinabung, so I have been bold and done it. Davidelit (Talk) 16:20, 29 August 2010 (UTC)[reply]

Nonsensical statement[edit]

"Most of Indonesian volcanism stems from the Sunda Arc, created by the subduction of the Indian Plate under the Indo-Australian Plate."

This statement is nonsense. The boundary between the Indian plate and the Indo-Australian plate is under the sea way to the west of indonesia. of the "sunda arc" volcanoes are apparently near the boundary of the Indo-Australian plate and the Eurasian plate, according to the plate diagram on all of the plate pages.Eregli bob (talk) 09:22, 30 August 2010 (UTC)[reply]

Fixed. Thanks for the note. --Elekhh (talk) 10:21, 30 August 2010 (UTC)[reply]

GA review[edit]

I know this article is a long ways from approaching GA status, but I would like to have an independent opinion on what needs work...--Gniniv (talk) 08:52, 1 September 2010 (UTC)[reply]

In Category:GA-Class WikiProject Volcanoes articles there are a number of volcano GAs, which might be helpful to look at. A simple comparison will reveal that the current geology section is very thin, while the history section is non-existent. It is also likely that some exploration of geothermal energy has been conducted there. Elekhh (talk) 12:58, 1 September 2010 (UTC)[reply]

External links modified[edit]

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External links modified (February 2018)[edit]

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