MVO reported that during 31 October-7 November the activity level at the Soufrière Hills lava dome was low and there was no evidence of lava extrusion. Photographs taken during an aerial inspection of the dome confirmed that the SE side was a very high (150-200 m) free-standing cliff not supported by talus. Erosion continued on the NE side and at the E and SE bases of the dome, further deepening the moat in the talus around the dome. The morphology of the top of the dome was complex and highly irregular with multiple steep lava protrusions separated by areas of lower elevation. Several spines and a bulbous shear lobe were visible. The Hazard Level remained at 3.
Source: Montserrat Volcano Observatory (MVO) – “Reports provided courtesy of the Smithsonian’s Global Volcanism Program and the US Geological Survey’s Volcano Hazards Program.”