the sea (e.g., Surtsey (Thordarson, 2000)), indicating that for a first order estimate of lava
emplacement, MrLavaLoba is an appropriate model. This model is incapable, however, of
providing information on time-evolving changes, such as rate of lava advancement. It is
therefore suitable for long-term planning and the consideration of potential economic damages
from modeled flows, which
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