The Hawaiian Volcano Observatory (HVO) has recorded over 130 earthquakes beneath the NE top of the Ka‘ōiki fault system, northwest of Kīlauea’s summit, on October 22 and 23, 2020. Other Kīlauea monitoring data streams remain stable and show no signs of increased activity.
The quakes are occurring in a cluster of about 2 km (1.2 miles) wide and 2 – 5 km (1 – 3 miles) below the surface, HVO said in a statement released 00:02 UTC on October 24.
The largest event in the sequence was a M3 earthquake, with the bulk of the events being less than M2 and not reported widely felt by residents. Reported felt events were described as weak shaking, with a maximum Intensity of III on the Modified Mercalli Intensity Scale.
Other monitoring data streams for Kīlauea and Mauna Loa, including ground deformation, gas, and imagery, show no signs of increased activity.
“Clustering of shallow earthquakes in this region does not mean an eruption is imminent,” HVO specialists said.
The observatory has recorded shallow earthquakes in this area for many decades across several eruptive cycles at both Kīlauea and Mauna Loa.
HVO said it continues to closely monitor geologic changes, seismicity, deformation, and gas emissions at Kīlauea and Mauna Loa volcanoes and will issue additional messages and alert level changes as warranted by changing activity.
Featured image credit: USGS/HVO