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On Feb. 3, 2024, a team of HVO scientists documented new ground cracks in three areas of the Maunaiki Trail in the Ka‘ū Desert, caused by the intrusion southwest of Kīlauea’s summit caldera.
A magma river beneath Grindavik, Iceland, sparks a state of emergency, disrupting the village and raising concerns about volcanic reawakening.
The overall decrease in seismicity and deformation suggests that this event is waning.
Periods of increased earthquake activity and rates of ground deformation can be expected to continue in this region.
Based on past historical activity, this event is much more likely to continue as an intrusion, but there is still a possibility of it ending in an eruption.