Fig. 2From: Monitoring volcanic activity with distributed acoustic sensing using the Tongan seafloor telecommunications cableCable depth and DAS records for the entire observation period. a Seafloor depth along the cable route was derived from the ETOPO Global Relief Model (NOAA 2022). b DAS records plotted against length of cable from the landing station at Nuku’alofa, Tonga. DAS strain waveforms were band-pass filtered between 1 and 20 Hz and their absolute amplitudes are plotted at log scaleBack to article page