Σακουρατζίμα: Διαφορά μεταξύ των αναθεωρήσεων
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Γραμμή 46:
Sakurajima was formed by later activity within the caldera, beginning about 13,000 years ago.<ref>{{cite web |url = http://www.activolcans.info/fiche.php?NomVolcan=Sakurajima |title = Sakurajima at Activolcan.info |accessdate = 2007-08-03 |work = |language=French}}</ref> It lies about {{convert|8|km|sigfig=1|abbr=on}} south of the centre of the caldera. Its first eruption in recorded history occurred in 963 CE.<ref name="VOWO2">{{cite web |url = http://volcano.oregonstate.edu/volcanoes/volc_images/north_asia/sakura.html |title = Sakura-jima, Japan |work = VolcanoWorld |publisher = Oregon State University |accessdate = 2008-10-12 |archiveurl = http://web.archive.org/web/20080801055601/http://volcano.oregonstate.edu/volcanoes/volc_images/north_asia/sakura.html <!--Added by H3llBot--> |archivedate = 2008-08-01 }}</ref> Most of its eruptions are [[strombolian]],<ref name="VOWO2"/> affecting only the summit areas, but larger [[plinian]] eruptions have occurred in 1471–1476, 1779–1782 and 1914.<ref>{{cite web |url = http://hakone.eri.u-tokyo.ac.jp/unzen/sakura/geol.html |title = Sakurajima at the Earthquake Research Institute, University of Tokyo. |accessdate = 2007-08-03 }}</ref>
Volcanic activity at ''Kita-dake'' ended around 4,900 years ago: subsequent eruptions have been centered on ''Minami-dake''.<ref>{{cite gvp |vnum = 0802-08= |name = Sakura-jima |accessdate = 2007-08-04 }}</ref>. Since 2006 activity has centred on Showa crater, to the East of the summit of Minami-dake.<ref>{{cite journal|last=Iguchi|first=Masato|title=Forecasting volcanic activity of Sakurajima|journal=Proceedings of IAVCEI 2013 Scientific Assembly.|date=20 July 2013|url=http://www.iavcei2013.com/iavcei_hp/PDF/0A2_Key-02.pdf|accessdate=18 August 2013}}</ref>
===1914 eruption===
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