Based on visual observations from HVO crews and web camera views, HVO reported that during 25 June-1 July, lava flowed SE through a lava tube system from underneath Kilauea’s Thanksgiving Eve Breakout (TEB) and rootless shield complex to the Waikupanaha ocean entry. On 24 June, small episodic explosions at Waikupanaha propelled spatter about 50 m into the air; explosions were also noted on other days. The sulfur dioxide emission rate was 1,300 tonnes per day when measured on 24 June; the average background rate was about 2,000 tonnes per day. During 28 June-1 July, a small surface ‘a’a lava flow near the E boundary of the Royal Gardens subdivision advanced E. During 30 June-1 July, several surface flows from multiple points along the lava tube system were noted.
During the reporting period, Kilauea summit earthquakes were located beneath the summit area, along S-flank faults, and along the E and SW rift zones. Another 20-60 small earthquakes per day also occurred but were too small to be located. The vent in Halema’uma’u crater continued to produce a white plume with minor ash content that drifted mainly SW. Night-time incandescence was seen at the base of the plume. Seismic tremor was elevated. The sulfur dioxide emission rate was 900 tonnes per day when measured on 26 June. The background rate is 150-200 tonnes per day.
Source: US Geological Survey Hawaiian Volcano Observatory (HVO) – “Reports provided courtesy of the Smithsonian’s Global Volcanism Program and the US Geological Survey’s Volcano Hazards Program.”