The microstructure and mineralogy of volcanic rocks is varied and complex, and their
mechanical behaviour is similarly varied and complex. This review summarises recent …

With the emergence of portable broadband seismic instrumentation, availability of digital
networks with wide dynamic range, and development of new powerful analysis techniques …

Scientific theories of how subduction and plate tectonics began on Earth—and what the
tectonic structure of Earth was before this—remain enigmatic and contentious …

Magma transport in brittle rock occurs by diking. Understanding the dynamics of diking and
its observable consequences is essential to deciphering magma propagation in volcanic …

More than 800 million people live in proximity to active volcanoes and could be directly
impacted by potential eruptions. Mitigation of future volcanic hazards requires adequate …

The structure of upper crustal magma plumbing systems controls the distribution of
volcanism and influences tectonic processes. However, delineating the structure and …

An existing magma chamber is normally a necessary condition for the generation of a large
volcanic edifice. Most magma chambers form through repeated magma injections …

This work is aimed at reviewing the current state of the art in geosite selection, assessment,
and communication. We first highlight the main papers that have defined paramount …

To assess the probability of a volcanic eruption during an unrest period, we must understand
magma-chamber rupture and dyke propagation to the surface, as well as dyke arrest at …

The accuracy of elastic analytical solutions and numerical models, widely used in
volcanology to interpret surface ground deformation, depends heavily on the Young's …