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Evidence of more complex eruption behaviour is also present in Harrat Rahat in the form of more evolved (trachytic) eruptions within a small region around 24°5′N.
The Ontake eruption provided an opportunity to examine the deposits from a phreatic eruption with a complex eruption sequence that reflects the effect of external water on the eruption dynamics.
The Ontake eruption provided an important opportunity to study proximal deposits from a phreatic eruption that provides a complex eruption sequence and reflects the effect of water on the eruption dynamics.
They can also last a relatively long period (e.g., ~8 months for the La Soufrière event, Guadeloupe, in 1975 1976), resulting in a difficult scenario that requires managing a complex eruption sequence (Feuillard et al. 1983; Hincks et al. 2014).
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Although they are small in volume, they can produce complex eruptions, involving multiple eruptive styles.
They observed a considerable overlap among patients with eczema of pregnancy, prurigo of pregnancy, and pruritic folliculitis, both clinically and histopathologically, so they grouped them within a new disease complex "atopic eruption of pregnancy".
Kimberlite geology reflects complex multiphase eruptions and depositional events.
They typically display a wide diversity of different geological units and lithofacies, reflecting complex multiphase eruptions and a diversity of primary volcanic and secondary reworking processes.
Previous eruptions within the AVF have exhibited complex multi-phase eruption sequences with an initiating phreatomagmatic phase followed by scoria cone development and lava flows (Kereszturi et al. 2013).
We have previously applied our clean-up model in a complex multi-phase eruption scenario detailed in Deligne et al. (2015), of which our L2 eruption scenario is based on.
Meteorological conditions are considered one of the major controls on short to medium range ash fall deposits, particularly for small to moderate magnitude eruptions (Mortazavi 2009) Whilst the effect of wind direction has been recognized for some time, the complex interactions of eruption plumes and meteorological conditions are still an active area of research (e.g. Woodhouse et al. 2013).
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