<prompt> Bhala okuqhubekayo kwalesi sigaba - Ukuqhuma kwaqhuma i-tephra futhi kwawisa intaba yaba i-caldera, manje equkethe ichibi lomgodi okuthiwa iHeaven Lake. Ukuqhuma kwaqala nge-Plinian column enamandla, futhi kwaphela ngokugeleza okukhulu kwe-pyroclastic. Isilinganiso se-Plinian ashfall kanye ne-coignimbrite ashfall ehlanganiswe cishe noLwandle lwaseJapane nasenyakatho yeJapane. Lolu ungqimba lomlotha luye lwabizwa ngokuthi umlotha waseBaegdusan-Tomakomai B-Tm. Cishe kwenzeka ebusika ngasekupheleni kuka - 946 A.D. Lokhu kwakungenye yezintaba-mlilo ezinkulu kakhulu futhi ezinodlame kakhulu eminyakeni engu-5000 edlule, kanye nokuqhuma kweMinoan kweThera, ukuqhuma kweHatepe kweLake Taupo cishe ngo-180 AD, ukuqhuma kuka-1257 kweNtaba iSamalas  <response>: eduze neNtaba iRinjani, nokuqhuma kweNtaba iTambora ngo-1815. 