Images

Energy from solar panels at the KPcam site is stored in large batteries, which power the camera. Images captured by the camera are relayed, via an antenna, back to the observatory. USGS image by M. Warren.

An HVO physical science technician checks the wiring on the new webcam, attached to the top of the mast, that looks towards the summit and Southwest Rift Zone of Kīlauea. USGS photo by M. Patrick.

An HVO geologist attaches the upgraded KPcam to the mast. Like all HVO webcams, the KPcam is in box that protects it against the weather and elements. USGS photo by M. Warren.

An HVO field engineer adjusts the view of the upgraded KPcam, which is fixed on a mast a couple meters (yards) above the ground surface. The camera is located on the south flank of Mauna Loa, at an elevation of about 2,000 meters (6,700 feet) above sea level, and provides expansive views to the southeast of Kīlauea. USGS photo by M. Warren.

The KPcam, a webcam on the flank of Mauna Loa that looks south towards Kīlauea summit and the Southwest Rift Zone, was upgraded on June 25 by HVO staff. The new webcam will provide a higher quality image and slightly wider field of view. This photo shows HVO physical science technicians removing the old webcam. USGS photo by M. Patrick.

This map shows deformation following the recent eruption at Kīlauea on June 3, 2024.  It covers from June 6 to June 13, 2024, and is recorded by the Italian Space Agency's (ASI) Cosmo-SkyMED satellite. Colored fringes denote areas of ground deformation, with more fringes indicating more deformation.  Each color cycle represents 1.5 cm (0.6 in) of

The two distinct clusters of earthquakes at Kīlauea during the four recent time periods of swarm activity. The event counts at the south caldera cluster increase while the counts at the upper East Rift Zone cluster diminish from the first to the fourth time periods.

This map shows recent deformation spanning the recent eruption at Kīlauea.  It covers from May 28 to June 6, 2024, and is recorded by the Italian Space Agency's (ASI) Cosmo-SkyMED satellite. Colored fringes denote areas of ground deformation, with more fringes indicating more deformation.  Each color cycle represents 1.5 cm (0.6 in) of ground mot

This reference map depicts the June 3, 2024, eruption along Kīlauea's Southwest Rift Zone. The lava flows are shown in pink, covering about 99 acres (40 hectares); this number represents a slight increase from that reported Monday, June 3, due to minor flow expansion in the hours following that morning's helicopter overflight.

During an overflight at approximately 8:15 a.m. HST on June 6, 2024, USGS Hawaiian Volcano Observatory scientists observed the extensive crack features on either side of the now inactive fissures from the June 3 Kīlauea Southwest Rift Zone eruption. Cracks range in length and are parallel to the fissure system. USGS photo by A.R. Nalesnik. 

During the Kīlauea Southwest Rift Zone eruption on June 3, fissures 3 and 4—located farther to the southwest than fissures 1 and 1— erupted the larger volumes of lava and continue to exhibit elevated gas emissions.

In addition to elevated volcanic gas emissions, other significant hazards also remain around the recent eruption site on the upper Southwest Rift Zone of Kīlauea.

Aerial overview of fissures 3 and 4 of the now paused Kīlauea Southwest Rift Zone eruption that began on June 3, 2024. During an overflight at approximately 8:15 a.m. HST on June 6, 2024, USGS Hawaiian Volcano Observatory scientists observed persistent gas emissions and no active lava. USGS Image by A.R. Nalesnik.

During the June 3, 2024, Southwest Rift Zone eruption, Fissures 1 and 2 (pictured here) had low erupted volumes compared to fissures 3 and 4. Fissures 1 and 2 were located closer to Kalupele (Kīlauea summit caldera), whereas fissures 3 and 4 are on the southwest section of the fissure system. USGS Image by A.R. Nalesnik.

The new seismometer at station KOSM on the Southwest Rift Zone of Kīlauea being buried in the ground, with permission from Hawai'i Volcanoes National Park. This photo was taken before the seismometer was totally buried.

The new seismometer at station KOSM on the Southwest Rift Zone of Kīlauea being buried in the ground, with permission from Hawai'i Volcanoes National Park. This photo was taken before the seismometer was totally buried.

On June 6, USGS Hawaiian Volcano Observatory field engineers installed a new seismometer on the Southwest Rift Zone of Kīlauea to monitor earthquakes. The new seismic station is co-located at an existing monitoring station consisting of a GPS and high-resolution gas monitoring equipment.

The recent Southwest Rift Zone eruption of Kīlauea produced small volumes of lava, and fountains left volcanic spatter on top of and beyond the extent of the newly erupted flows. The collected pieces of spatter range in size up to 4 inches (1 to 10 centimeters). USGS image by A.R. Nalesnik.

USGS Hawaiian Volcano Observatory field engineers visited the KOSM GPS station on June 6, 2024, to install a new seismic sensor, with permission from Hawai‘i Volcanoes National Park. The KOSM station is located southwest of the now inactive fissure 4 of the Southwest Rift Zone eruption of Kīlauea (the southwest-most fissure). USGS image by A.R. Nalesnik.

At the KOSM GPS located station on the Southwest Rift Zone eruption of Kīlauea, HVO field engineers installed a new seismic sensor, with permission from Hawai‘i Volcanoes National Park. USGS image by M. Warren on June 6, 2024.

USGS Hawaiian Volcano Observatory geologists visited the now inactive fissures that formed on June 3rd on the upper Southwest Rift Zone of Kīlauea. Looking through a hand lens, geologists recognize the abundance of olivine ranging from 1-3 mm (about 0.1 inch) in size in the spatter samples.