Skip to main content
Fig. 4 | Earth, Planets and Space

Fig. 4

From: Motivations for muon radiography of active volcanoes

Fig. 4

A south-east looking view of Stromboli. The “Sciara del Fuoco” structure and the active craters are indicated. Inversion of the Very Long Period (VLP) events generated by the volcanic explosions reveal a seismic source constituted by an oscillating dyke located between 220 and 260 m below the craters. (After Chouet et al., Source mechanisms of explosions at Stromboli Volcano, Italy, determined from moment-tensor inversion of very-long period data, J. Geophys. Res., 108(B1), doi:http://10.1029/2002JB001919, 2003. Copyright 2003 American Geophysical Union. Reproduced by permission of American Geophysical Union.)

Back to article page