Sinuous collapse chains and skylights in lunar and Martian volcanic regions have often
been interpreted as collapsed lava tubes (also known as pyroducts). This hypothesis has …

Squeeze-ups are common features of basaltic lava flow-fields on Earth. Squeeze-ups,
rootless autointrusions of lava, drive intraflow resurfacing of active flow-fields, and the term is …

Monitoring for assessment of natural disasters, such as volcanic eruptions, presents a
methodological challenge for the scientific community. Here, we present Unmanned Aerial …

Effusive activity at Stromboli is uncommon, and the 2002–2003 flank eruption gave us the
opportunity to observe and analyze a number of complex volcanic processes. In particular …

During an eruption, time scales of topographic change are fast and involve vertical and
planimetric evolution of millimeters to meters as the event progresses. Repeat production of …

The 11–13 January 2011 eruptive episode at Etna volcano occurred after several months of
increasing ash emissions from the summit craters, and was heralded by increasing SO2 …

The∼ 80 ka Lathrop Wells volcano (southern Nevada, USA) preserves evidence for a range
of explosive processes and emplacement mechanisms of pyroclastic deposits and lava …

A “lava morphotype” refers to the recognizable and distinctive characteristics of the surface
morphology of a lava flow after solidification, used in a similar way to a sedimentary facies …

Five Pleistocene basaltic volcanoes in Crater Flat (southern Nevada) demonstrate the
complexity of eruption processes associated with small-volume basalts, and the effects of …

Bathymetry data collected with a multibeam echo sounder around Pico Island, Azores
(Portugal), reveal a remarkable series of lava flows on the island's shelf with a variety of …