火山
Online ISSN : 2189-7182
Print ISSN : 0453-4360
ISSN-L : 0453-4360
メラピ型火砕流の発生過程 : 雲仙普賢岳第6ドームでの観測結果
宇井 忠英隅田 まり大学合同観測班地質班荒牧 重雄大島 治鎌田 桂子小林 武彦小屋口 剛博佐藤 博明中川 光弘中田 節也藤井 敏嗣藤縄 明彦古山 勝彦三宅 康幸横瀬 久芳渡辺 一徳
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1993 年 38 巻 2 号 p. 45-52

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Small-scale pyroclastic flows due to the collapse of the lava dome have been frequently generated during the 1991-93 eruption of Unzen Volcano. We have recorded video footages which show the generation of pyroclastic flows during January-March 1992. Two types of phenomena have been observed : deformation of the lava dome due to flowage ; and a sudden discharge of gas and ash through fractures and peeling-off of rock fragments from the surface of cooling lava blocks. Pyroclastic flows were generated only in places on the lava dome where these precursory phenomena were frequently observed.

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© 1993 特定非営利活動法人日本火山学会
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