0 a very large, circular hollow that remains when the central part of a volcano falls in after an eruption
A small, possibly ephemeral caldera lake is a likely source.
Cooling units and composite sheets in relation to caldera structure.
Eruption of the ignimbrites is envisaged as a series of poorly expanded flows possibly with incorporated fall material generated by foundering of a caldera floor.
The sedimentary breccias were probably formed from talus and/or other types of colluvium that were shed from the ring-fracture fault scarp of the caldera.
These minerals may have formed by recrystallization of pre-existing weak advanced-argillic alteration at the southern margin of the caldera structure.
This suggests that eruptive hiatuses in the extracaldera record may reflect effusive activity and stratovolcano or shield-building phases within the summit caldera.
A caldera lake is occasionally established in the present caldera following snowmelt.
It is possible that this embayment is a caldera or lateral collapse structure.
中文繁体
破火山口(火山爆發後,中心塌陷而形成的巨大圓形凹陷)…
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喷火山口(火山爆发后,中心塌陷而形成的巨大中空)…
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caldeira vulcânica…
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kaldera…
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