Kīlauea's ongoing eruption: a rising lava lake
It has been an exciting week at Kīlauea Volcano as the summit eruption that began on the evening of December 20th continues. The eruption remains confined within Halema‘uma‘u crater. Monitoring data show no signs of activity migrating from the summit into the rift zones, nor indications of summit collapse like those in 2018.
The primary hazard from this eruption at this time is vog (volcanic air pollution) produced by the gases emitted at the summit. USGS Hawaiian Volcano Observatory (HVO) scientists continue to closely monitor the eruption.
As last week’s “Volcano Watch” went to press, lava
continued to erupt from two vents
on the west and north sides of Halema‘uma‘u crater at a combined rate of approximately 30 cubic m (1060 cubic ft) per second. The rise of the lava lake
was slowing due to the funnel-like shape of Halema‘uma‘u.
By Christmas night, the lava lake had risen slightly above the level of the north vent
, which to this point was the dominant source of lava for the eruption. Lava
fountaining from the north vent, which built an amphitheater-shaped cone surrounding it, drove circulation in the lava lake apparent in the motion of the crust
Early in the morning on December 26th, the biggest change in eruptive activity was observed. At approximately 3 a.m. HST, activity at the west vent increased dramatically as the fountaining at the north vent died out. HVO scientists observing the lake witnessed lava draining back into the north vent and the lake level dropped 5 meters (26 feet) over the next few hours. This left a â€˜bathtub ring’ around the edge of the lake, marking the lake’s high point. The change in active vent also saw a decrease in sulfur dioxide (SO2
) gas output, down from 16,000–20,000 tonnes per day on December 25th to 3,800 tons per day on December 30th.
The lava lake level has been rising slowly again since December 27th and, as of writing this article, it has reached a new peak elevation of 701 m (2300 feet) above sea level (asl) and depth of 184 m (603 feet). The erupted volume to this point is more than 20 million cubic meters (700 million cubic feet) or about 8,000 Olympic-sized swimming pools! The eruption rate has decreased to approximately 10 cubic m (353 cubic ft) per second. On December 30, the lake measured 800 m (875 yd) east-west and 530 m (580 yd) north-south, covering an area of 33 hectares (82 acres). Lava continues to erupt from the west vent.
One of the most common questions that HVO gets is, “When will the lake be visible from an open area of Hawai‘i Volcanoes National Park?” and “Will the lava lake fill Halema‘uma‘u?” These questions are difficult to answer because the activity within Halema‘uma‘u is dynamic. After the eruption first started, the lava lake rose rapidly both due to the shape of the base of Halema‘uma‘u (inverted cone) and the initially high rates of lava being erupted.
Since then, the rate of lava being erupted has varied, especially as activity shifted from the north to the west vent, with associated lava drainback into the inactive north vent and a temporary decrease in lake level. However, HVO has done some preliminary calculations to try and answer these questions using topographic models and the most recent eruption rate.
The lava lake should be visible from Kīlauea Overlook once it reaches an elevation just over 780 m (2560 ft) asl, then another 5 m (16 ft) of rise will have it overflowing the lowermost rim of Halema‘uma‘u on the northeast side. Since the lava lake is currently at about 701 m (2300 feet) asl, it has about 80 m (262 ft) to rise before it reaches the level of visibility. When it does so depends on the rate of lava being erupted.
Assuming a constant eruption rate of 10 cubic m (353 cubic ft) per second, it would take approximately forty-five days for lava to fill Halema‘uma‘u to just over 780 m (2560 ft) asl, therefore becoming visible from Kīlauea Overlook. Several days later it would start overflowing the lowermost rim of Halema‘uma‘u at just below 800 m (2625 ft) asl. However, it would likely take longer as the eruption rate has been fluctuating and generally decreasing. If lava did overflow Halema‘uma‘u, it would then need to fill the extensive down-dropped block area before overflowing onto the main caldera
HVO continues to closely monitor this eruption in Halema‘uma‘u at Kīlauea’s summit. Check the HVO website for photo, video, and text updates: www.usgs.gov/hvo.
Volcano Activity Update
Kīlauea Volcano is erupting. Its USGS Volcano Alert level is at WATCH (https://www.usgs.gov/natural-hazards/volcano-hazards/about-alert-levels). Kīlauea updates are issued daily.
Activity is confined to Halema‘uma‘u with lava
erupting from vents
on the northwest side of the crater. Over the past 24 hours, the lava lake
depth measurements have ranged from 181 m to 185 m (593 to 608 ft) deep. Preliminary analysis of sulfur dioxide emission
rates measured Wednesday (Dec. 30) show that the rates are about 3,800 tonnes/day, in the range of values common for the pre-2018 lava lake. Summit tiltmeters recorded neither inflationary nor deflationary tilt over the past two days. Seismicity
remained elevated but stable, with steady elevated tremor and a few minor earthquakes
. For the most current information on the eruption, see https://www.usgs.gov/volcanoes/kilauea/current-eruption.
Mauna Loa is not erupting and remains at Volcano Alert Level ADVISORY. This alert level does not mean that an eruption is imminent or that progression to eruption from current level of unrest is certain. Mauna Loa updates are issued weekly.
This past week, about 60 small-magnitude earthquakes were recorded beneath the upper-elevations of Mauna Loa; most of these occurred at depths of less than 8 kilometers (about 5 miles). The largest recorded earthquake
was a M2.2 beneath the volcano's northwest flank on December 28 at 12:47 a.m. HST. The earthquake activity on Mauna Loa’s northwest flank, which began on December 4, 2020, has subsided to average long-term trends. Global Positioning System (GPS) measurements recorded contraction across the summit caldera
since mid-October with extension (summit inflation) resuming in the past few weeks, consistent with magma
supply to the volcano's shallow storage system. Gas concentrations and fumarole
temperatures at both the summit and Sulphur Cone on the Southwest Rift Zone remain stable. Webcam views have revealed no changes to the landscape over the past week. For more information on current monitoring of Mauna Loa Volcano, see: https://volcanoes.usgs.gov/volcanoes/mauna_loa/monitoring_summary.html.
There were 7 events with 3 or more felt reports in the Hawaiian Islands during the past week: a M2.8 earthquake 2 km (1 mi) E of Pāhala at 33 km (20 mi) depth on Dec. 28 at 1:26 p.m. HST, a M2.8 earthquake 9 km (5 mi) ENE of Pāhala at 31 km (19 mi) depth occurred on Dec. 26 at 5:55 a.m. HST, a M2.2 earthquake 6 km (3 mi) ENE of Pāhala at 30 km (19 mi) depth occurred on Dec. 24 at 7:56 p.m. HST, a M1.7 earthquake 6 km (3 mi) ENE of Pāhala at 32 km (20 mi) depth occurred on Dec. 24 at 7:28 p.m. HST, a M3.6 earthquake 7 km (4 mi) ENE of Pāhala at 33 km (20 mi) depth occurred on Dec. 24 at 7:18 p.m. HST, a M3.3 earthquake 8 km (4 mi) NE of Pāhala at 32 km (19 mi) depth occurred on Dec. 24 at 7:13 p.m. HST, and a M1.7 earthquake 2 km (1 mi) SE of Pāhala at 33 km (20 mi) depth occurred on Dec. 24 at 7:12 p.m. HST.
HVO continues to closely monitor both Kīlauea’s ongoing eruption and Mauna Loa for any signs of increased activity.
Please visit HVO’s website for past Volcano Watch articles, Kīlauea and Mauna Loa updates, volcano photos, maps, recent earthquake info, and more. Email questions to askHVO@usgs.gov.
Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.