Source: US Geological Survey
Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.
On July 10, HVO field engineers strapped snowshoes on as they prepared to work in the closed area of Hawaiʻi Volcanoes National Park, southwest of the
two eruptive vents in Halemaʻumaʻu. With each step, the ground crunched and their feet sunk a little. The large footprint of snowshoes keep the field engineers walking on top of the frothy pumice everywhere, rather than through it. Tiny pieces of volcanic glass shimmered in the air, which was filled with the soft sound of clinking glass. They wore full-face respirators to protect themselves from these particles, called tephra.
Tephra is a word for any volcanic material that is erupted and travels through the air before landing on the ground. It includes very small particles, such as volcanic ash, as well as light and frothy rocks full of holes called reticulite, more robust rocks like scoria, larger pieces called bombs, and ever-present Pele’s Hair.
Lava fountains of the ongoing episodic eruption in Halemaʻumaʻu have created a growing tephra blanket downwind of the eruptive vents. On the crater rim closest to the vents, the tephra is as thick as 80 feet (25 meters). Lava flows fed by these fountaining episodes have also covered nearly 850 acres (344 hectares) of Halemaʻumaʻu crater floor, up to 236 feet (72 meters) thick in some areas.
HVO staff have moved several monitoring stations that were located in areas too close to lava flows or areas buried by falling tephra. The instruments themselves remained functional and most, including the F1 thermal camera, KWcam, B1cam, and continuous laser rangefinder, have been redeployed near the V1 streaming camera, an area less likely to be impacted by the eruption. The B2cam on the crater floor underwent a full melt down, but its solar power supply survived and was airlifted to the south rim to power the new V3 livestream camera.
Several other monitoring stations are located farther away from the vents but are still being impacted by the eruption. The instruments at these stations, many of which measure volcanic gas, are positioned southwest of the summit because that direction is usually downwind of summit eruptions during common trade wind conditions. Being downwind of the ongoing eruption means that, in addition to the gas they are designed to measure, the stations are subjected to tephra fall.
Infrastructure at monitoring stations in this area can be covered by tephra depending on the wind direction during an eruptive episode. Following eruptive episodes, HVO staff have visited these sites dig them out and to remove tephra from solar panels, restoring power to the station.
Sulfur dioxide emission rates, which HVO measures to help track eruptive activity, are not possible when this part of the network is down. HVO staff are exploring other methods for obtaining sulfur dioxide emission rates. In the meantime, numerous measurements during past pauses and eruptive episodes allow us to generally estimates these emissions during different types of activity. During past eruptive pauses, sulfur dioxide emission rates have been measured as around 1,200-1,500 tonnes per day During past eruptive episodes, sulfur dioxide emission rates have been measured up to 75,000 tonnes per day. It’s likely that sulfur dioxide emission rates have been even higher during recent eruptive episodes, though measurements have not been possible.
High lava fountains can also temporarily block radio telemetry, preventing data flow from monitoring stations. Most telemetry paths have been re-routed to avoid this issue, but several instruments, including the Sandhill tiltmeter, Cone Peak (CNPK) GPS, and several seismic stations (WRM, SDH, CPKD, OTLD), may continue to be affected during episodes with high lava fountains.
The area southwest of eruptive vents can be difficult to access. Depending on the wind direction during lava fountaining episodes, more tephra can blanket the landscape (and access road) to the southwest with every episode. After each episode, HVO staff assess the feasibility of visiting monitoring sites with staff safety being the primary priority.
Although a small portion of the Kīlauea monitoring network is being impacted by the summit eruption, HVO is still able to adequately monitor Kīlauea. Maintaining the instrument network during eruptions is one of the challenges that comes with monitoring one of the most active volcanoes on Earth.
Volcano Activity Updates
Kīlauea has been erupting episodically within the summit caldera since December 23, 2024. Its USGS Volcano Alert level is WATCH.
Episode 28 of the Kīlauea summit eruption in Halemaʻumaʻu crater occurred on July 9, with approximately 9 hours of fountaining from the north vent. The south vent did not activate and has been completely covered by new deposits. Summit region inflation since the end of episode 28, along with persistent tremor, suggests that another episode is possible though more time (and data) are needed before a forecast can be made. Sulfur dioxide emission rates are elevated in the summit region during active eruption episodes. No unusual activity has been noted along Kīlauea’s East Rift Zone or Southwest Rift Zone.
Mauna Loa is not erupting. Its USGS Volcano Alert Level is at NORMAL.
One earthquake was reported felt in the Hawaiian Islands during the past week: a M2.9 earthquake 10 km (6 mi) S of Volcano at 6 km (3 mi) depth on July 6 at 5:04 a.m. HST.
HVO continues to closely monitor Kīlauea and Mauna Loa.
Please visit HVO’s website for past Volcano Watch articles, Kīlauea and Mauna Loa updates, volcano photos, maps, recent earthquake information, and more. Email questions to askHVO@usgs.gov.
