Kilauea volcano (Hawai'i): activity remains unchanged; lava flow continues to feed lava lake
Mon, 8 Mar 2021, 10:26 | BY: MARTIN
A small incandescent opening at the top of the west vent spatter cone (bottom-center) including gas plume (image: HVO)
Aerial view of Kīlauea's summit from 4 March (image: HVO)
The western portion of the lava lake in Halema'uma'u crater remains active and is supplied by the lava flow from the western fissure of the spatter cone. A small incandescent opening at the top of the west vent spatter cone is visible in the attached image.
The inactive eastern portion of the lake appears dark.
Sulfur dioxide (SO2) emissions remain at elevated levels and reached to a 1000 tonnes/day on 3 March as a result of the ongoing eruption. Volcanic gas emissions from the active west vent are being transported to the southwest.
On 4 March, HVO scientists conducted an overflight of Kīlauea's summit to document the ongoing eruption.
Laser rangefinder measurements indicate that lava has filled about 220 meters (772 ft) of Halema'uma'u.
Source: Hawaiian Volcano Observatory volcano activity update 8 March 2021
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Wed, 3 Mar 2021, 06:00
Kilauea volcano (Hawaiian Islands, USA) - Smithsonian / USGS Weekly Volcanic Activity Report for 3 March-9 March 2021 (Continuing Activity)
HVO reported that a vent on the inner NW wall of Kilauea's Halema`uma`u Crater continued to supply the lava lake during 2-8 March through a submerged inlet. The sulfur dioxide emission rate was 1,000 tons/day during 2-3 March, and 800 tons/day on 7 March. The depth of the western part of the lake fluctuated around 219-220 m. ... Read all
Wed, 24 Feb 2021, 06:00
Kilauea volcano (Hawaiian Islands, USA) - Smithsonian / USGS Weekly Volcanic Activity Report for 24 February-2 March 2021 (Continuing Activity)
HVO reported that a vent on the inner NW wall of Kilauea's Halema`uma`u Crater continued to supply the lava lake during 24 February-2 March. The depth of the western part of the lake deepened from 217 to 219 m. Lava effused from a submerged vent and rapidly developed a thin crust as it flowed E towards the main stagnant island. ... Read all
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