Any effective volcanic risk mitigation strategy requires a scientific assessment of the future
evolution of a volcanic system and its eruptive behavior. Some consider the onus should be …

Plate motion and associated tectonics explain the location of magmatic systems along plate
boundaries [1], however, they cannot give satisfactory explanations of the origin of intra …

ABSTRACT INTRODUCTION that are commonly, but not exclusively, small in eruptive
volume. Monogenetic volcanic fields commonly consist of large numbers of volcanic clusters …

Abstract The Auckland Volcanic Field (AVF) with 49 eruptive centres in the last c. 250 ka
presents many challenges to our understanding of distributed volcanic field construction and …

Most flank eruptions within a central stratovolcano are triggered by lateral draining of
magma from its central conduit, and only few eruptions appear to be independent of the …

In the southern winter of 1970, a phreatomagmatic eruption occurred in the northern part of
Deception Island (South Shetland Archipelago, Antarctic Peninsula). The eruption, with no …

Volcanic activity typically switches between high-activity states with many eruptions and low-
activity states with few or no eruptions. We present a simple two-regime physics-informed …

We examine the application of Hidden Markov Models (HMMs) to volcanic occurrences. The
parameters in HMMs can be estimated from data by means of the Expectation …

Many accounts, anecdotal and statistical, have noted a causal effect on volcanic eruptions
from large, not too distant, earthquakes. Physical mechanisms have been proposed that …

Distributed “monogenetic” volcanic eruptions commonly occur in continental settings without
obvious structural alignments or rifting/extensional structures. Nevertheless, these may …