Table S1: Sample list. Figure S1: Effects of the explosions. Figure S2: Relative abundance of the different clast lithologies in the different samples. Figure S3. Shape parameters relative to the grain-size class. Figure S4: Density distribution for the different lithologies of the coarse material. Figure S5: Pre-eruption topography of the area invaded by the lava flow. Supplemental Video S1: UAS video footage of the lava flow and the deposit of the explosion. Supplemental Data S1: Field and laboratory data.</p
Explosive activity at Mt. Etna from July 19 to August 7, 2001, provides a good case study to investi...
On 11 February 2014, a considerable volume (0.82 to 1.29 × 106 m3) of unstable and hot rocks detache...
Basaltic volcanism is the most widespread volcanic activity on Earth and planetary bodies. On Earth,...
On 16 November 2006 a flank collapse affected the unstable eastern slope of the South-East Crater (S...
On 16 November 2006 a flank collapse affected the unstable eastern slope of the South-East Crater (S...
co-auteur étrangerInternational audienceLow elevation flank eruptions represent highly hazardous eve...
Determining the volume of the various types of products of a highly frequent active volcano can be v...
We provide the dataset associated with the research data article “Shallow factors controlling the ex...
We present a detailed physical and geochemical analysis of a small-scale eruption at the type basalt...
International audience[1] Two unusual, highly explosive flank eruptions succeeded on Mount Etna in J...
Containing one pdf file with Supplemental Information (Fig. S1–S4 and list of references from Table ...
Rapid characterization of tephra from ongoing explosive eruptions can provide valuable insights into...
The 2002–03 flank eruption of Etna was characterized by two months of explosive activity that produc...
On 7 September 2008 a major ash explosion occurred from the SW summit crater of Stromboli volcano. T...
Invasion of inhabited areas and destruction of human property by lava flows represents the greatest ...
Explosive activity at Mt. Etna from July 19 to August 7, 2001, provides a good case study to investi...
On 11 February 2014, a considerable volume (0.82 to 1.29 × 106 m3) of unstable and hot rocks detache...
Basaltic volcanism is the most widespread volcanic activity on Earth and planetary bodies. On Earth,...
On 16 November 2006 a flank collapse affected the unstable eastern slope of the South-East Crater (S...
On 16 November 2006 a flank collapse affected the unstable eastern slope of the South-East Crater (S...
co-auteur étrangerInternational audienceLow elevation flank eruptions represent highly hazardous eve...
Determining the volume of the various types of products of a highly frequent active volcano can be v...
We provide the dataset associated with the research data article “Shallow factors controlling the ex...
We present a detailed physical and geochemical analysis of a small-scale eruption at the type basalt...
International audience[1] Two unusual, highly explosive flank eruptions succeeded on Mount Etna in J...
Containing one pdf file with Supplemental Information (Fig. S1–S4 and list of references from Table ...
Rapid characterization of tephra from ongoing explosive eruptions can provide valuable insights into...
The 2002–03 flank eruption of Etna was characterized by two months of explosive activity that produc...
On 7 September 2008 a major ash explosion occurred from the SW summit crater of Stromboli volcano. T...
Invasion of inhabited areas and destruction of human property by lava flows represents the greatest ...
Explosive activity at Mt. Etna from July 19 to August 7, 2001, provides a good case study to investi...
On 11 February 2014, a considerable volume (0.82 to 1.29 × 106 m3) of unstable and hot rocks detache...
Basaltic volcanism is the most widespread volcanic activity on Earth and planetary bodies. On Earth,...