Volcanism is one of the main mechanisms transferring mass and energy between the
interior of the Earth and the Earth's surface. However, the global mass flux of lava, volcanic …

One of the major problems with palaeoclimate investigations in volcanic regions is that
tephra inputs to lakes can cause changes in proxies analogous to those of climate forcing …

Volcanic seismology represents the main, and often the only, tool to forecast volcanic
eruptions and to monitor the eruption process. This book describes the main types of seismic …

When not laterally confined in valleys, pyroclastic flows create their own channel along the
slope by selecting a given flowing width. Furthermore, the lobe‐shaped deposits display a …

The 2010 pyroclastic density currents (PDC) at Merapi have presented a rare opportunity to
collect a uniquely detailed dataset of the source, extent, lateral variations and impact of …

La mayor parte de los grandes volcanes de nuestro país se encuentran ubicados en la parte
frontal de la Faja Volcánica Transmexicana y en otras zonas volcánicas aisladas. En este …

A series of pristine block-and-ash flow deposits from the May–June 2006 eruption of Merapi
represent an exceptional record of small-volume pyroclastic flows generated by gravitational …

Experiments on dry granular matter flowing down an inclined plane are performed in order
to study the dynamics of dense pyroclastic flows. The plane is rough, and always wider than …

The 18–24 January 1913 eruption of Colima Volcano consisted of three eruptive phases that
produced a complex sequence of tephra fall, pyroclastic surges and pyroclastic flows, with a …

Based on the stratigraphic record of the deposits, analysis of previous works, historic
archives, and eyewitness accounts the 1913 eruption of Volcán de Colima was …