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If there is a significant difference between the eruption frequency of the two (Fig. 7) for the past 2000 years, then there is a bias and we must adjust our Southeast Asian eruption probabilities.
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Generally, there were no substantial differences between the mean eruption times of the children in the present study and other studies involving African populations (Tables 5 and 6).
The difference between the 2011 Shinmoe-dake eruption without precursory tilt changes and earthquakes and the Izu-Oshima fissure eruption, and the Izu-Tobu, and Miyakejima eruptions are probably due to whether a conduit exists or not.
There was no significant difference between the levels of tooth eruption and types of impacted teeth removed in either group.
The difference between the 2007 and 2014 eruptions can be explained if a relatively large magma intruded before the 2007 eruption but no or a small magma intrusion occurred before the 2014 eruption.
The difference between the 2007 and 2014 eruptions can be explained if a relatively large magma intrusion occurred before the 2007 eruption but no or a small magma intrusion before the 2014 eruption.
Other factors that could lead to observed differences in the eruption times between the two studies are that the previous study [ 13] was a national estimate based on a smaller sample of children (n = 622).
The ~ 30-year difference between the age of the youngest specimen and the eruption could be explained by temporal changes in ΔR (Hirabayashi et al. 2017).
Discuss the differences between two different eruptions (the volume and distribution): An eruption with a plume height of 2 km, and duration of 20 minutes, vs. An eruption with a plume height of 15 km, and duration of 2 hours.
This temperature difference between the two causes violent water-lava interactions that make up the eruption.
We suggest that different pre-eruption evolution and magnetic configuration in the two regions might have contributed to the difference between the two ARs.
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