熔岩锥，是以溢流产物为主形成的火山锥，火山碎屑物质常<10%，形态受熔岩性质的影响而不尽相同。
中间是一块巨大的汤碗形寄生熔岩锥，壮观的岩浆湖就被盛放在巨碗之中。
In the middle, contained in a giant soup-bowl-shaped spatter cone, was a stunning sight: a lake of lava.
此火山的主体是玄武岩，但是山坡却点缀著由石英安山岩（一种玻璃质、富含矽的熔岩）形成的熔岩锥和熔岩流。
The bulk of the volcano is basaltic , but the slopes are dotted with cones and lava flows consisting of glassy , silica - rich lavas called dacites.
此火山的主体是玄武岩，但是山坡却点缀著由石英安山岩(一种玻璃质、富含矽的熔岩)形成的熔岩锥和熔岩流。
The bulk of the volcano is basaltic, but the slopes are dotted with cones and lava flows consisting of glassy, silica - rich lavas called dacites.
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