Recent data shows that Kīlauea volcano is not erupting and seismicity at the volcano’s summit, East Rift Zone, and Southwest Rift Zone is low and deformation is steady.

Earthquake activity at Kīlauea’s summit region was generally low over the past week. Overall, there were 120 earthquakes in the summit, all below magnitude-2.0. The tiltmeter at Uēkahuna, northwest of Kaluapele, the summit caldera, remained relatively flat with no significant changes over the past week. The tiltmeter at Sand Hill, southwest of Kaluapele, continues to show slow weak inflation (about 4 microradians over the past week). The most recent measurement of the sulfur dioxide (SO2) emission rate from the summit was approximately 70 tonnes per day on October 17, a value representative of noneruptive conditions at Kīlauea.

Shallow earthquake counts in the upper and middle East Rift Zone (ERZ) have returned to low levels following the small uptick last week. There were approximately 70 located earthquakes in the middle ERZ, and approximately 70 in the upper ERZ as well, with most below magnitude-2.0. Deformation remains steady in the ERZ, as recorded by GPS instruments and tiltmeters. There are no indications of any changes downrift in the lower East Rift Zone.

Kīlauea erupted briefly in and near Nāpau Crater from September 15–20, 2024. Lava flows from this eruption covered more than 880,000 square meters (217 acres) of Nāpau Crater and areas to the west.

Since that most recent eruption, unrest has continued at low levels at the summit and on the ERZ of Kīlauea. Rates of seismicity and ground deformation have greatly decreased since the eruption, but geophysical data show that magma is continuing to move at a low rate into the volcano. Future intrusions and eruptions could occur with continued magma supply.

HVO continues to closely monitor Kīlauea and is in contact with Hawai‘i Volcanoes National Park and the Hawai‘i County Civil Defense Agency.