Effluxus Pyroclasticus
Effluxus pyroclasticus sive nubes ardens est frequens exitiosusque eruptionum vulcanicarum nonnullarum eventus.
Est corpus celere fluidicum gasii calidi, cineris et saxi (qui simul tephra nominantur) qui de sipunculo? vulcanico defundi celeritate 150 km/h potest, gasio nonnumquam 100-800 °C temperatura. Fluxus praecipites humi proximi delabi solent, celeritate ex proclivitate, et effluxus magnitudine pendente.
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