Documenting surface magmatic activity at Mount Etna using ATSR remote sensing

Analysis of thermally generated night-time volcanic radiances recorded with a 1-km pixel size at 1.6 and 11 mum during 1991-1993 and 1996-1999 for Mou nt Etna shows that lava flows extending beyond the summit craters can be di stinguished from vent activity. The two phenomena plot in different regions of feature space when the mean volcanic radiance (per anomalous pixel) at 11 mum is plotted against the mean volcanic radiance at 1.6 mum. The distin ct feature space characteristics of lava flow fields are apparent within 1- 2 days of the onset of each effusive event. Such a plot also enables lava f low fields being fed by open channels to be distinguished from tube-fed flo w fields. Rank order analysis of the total 1.6-mum volcanic radiance series shows that vent activity and lava flows belong to different populations, a nd offers further scope for remotely identifying changes in eruptive state.