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It also contains a glossary of volcanic terms and explanations of different types of eruptions.
They then examine different types of eruptions and the circumstances under which they are most likely to occur.
Various types of eruptions occur at volcanic lakes, ranging from phreatic to magmatic.
Hazards associated with these types of eruptions include ejection of crater lakes and generation of lahars (e.g., Kawah Ijen) and wet pyroclastic surges (e.g., Ruapehu).
This distribution reflects unique hazards with distance from the explosive vent for these types of eruptions in addition to the influence on volume estimates.
A complete record of eruption activity is required for a robust volcanic hazard assessment, characterising the types and magnitude of possible activity and the relative frequency of these different types of eruptions.
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We identified two types of eruption tremor, noise-like inharmonic waveforms and harmonic oscillatory signals.
There are two main types of eruption tremor at Tungurahua: noise-like inharmonic waveforms and harmonic oscillations.
We identified two types of eruption tremor at Tungurahua: noise-like inharmonic waveforms and harmonic oscillatory signals.
Similar precursory ground deformation has already been identified for Vulcanian eruptions at Sakurajima (Ishihara, 1990) and Montserrat (Voight et al., 1998, 1999), and the data presented here suggest that these precursory phenomena are also present before other types of eruption.
Some of them are distinctly related to Strombolian type of eruptions: such as the bomb-rich pyroclastic flow deposit described by Miyabuchi et al. (2006).
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