Measurement of effusion rate is a primary objective for studies that model lava flow and
magma system dynamics, as well as for monitoring efforts during on-going eruptions …

Volcanic eruptions are commonly preceded, accompanied, and followed by variations of a
number of detectable geophysical and geochemical manifestations. Many remote sensing …

We present a 30 year long data set of satellite‐derived time‐averaged lava discharge rates
(TADR) for Mount Etna volcano (Sicily, Italy), spanning 1980–2010 and comprising 1792 …

Prediction of the emplacement of volcanic mass flows (lava flows, pyroclastic density
currents, debris avalanches and debris flows) is required for hazard and risk assessment …

Invasion of inhabited areas and destruction of human property by lava flows represents the
greatest volcanic hazard at Mount Etna (Italy) in the short term, based on the character of the …

The linkages between ecology and geomorphology can be difficult to identify because of
physical complexity and the limitations of the current theoretical representations in these two …

The 2001 Etna eruption was characterized by a complex temporal evolution with the
opening of seven eruptive fissures, each feeding different lava flows. This work describes a …

Satellite-based surveillance of volcanic hot spots and plumes can be coupled with 17
modeling to allow ensemble-based approaches to crisis response. We complete benchmark …

Mount Etna produces frequent eruptions from its summit craters and from fissures on its
flanks. The flank fissures trend approximately radially to the summit, and are mainly …

The 1669 AD flank eruption was the most destructive event on Etna volcano in historical
times (∼ 700 BC) and provided, because of the presence of numerous quarries and …