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Temporary GPS survey equipment has been deployed in Kīlauea south caldera area for additional measurements during the ongoing heightened unrest there.

HVO scientists have been closely monitoring the earthquakes in Kīlauea's summit region over the past weeks. Most earthquakes have occurred at depths of 1–2 miles (2–3 kilometers) below the surface, with no upward migration detected.

This photo shows one of several temporary GPS survey stations recently deployed in Kīlauea south caldera region. The instruments will record additional measurements during the ongoing heightened unrest. Patterns of earthquakes and ground deformation indicate that Kīlauea's summit is becoming increasingly pressurized.

Scientists temporarily deployed a handful of temporary GPS instruments at established benchmarks in Kīlauea south caldera region to better measure ground deformation during the ongoing unrest there. Steady rates of earthquakes have persisted in this area since August 22.

Last week, HVO staff installed a new webcam—the B2cam—on the down-dropped block within Kīlauea caldera and east rim of Halema‘uma‘u crater. This camera view replaces that of the B1cam, which was moved east during the June 2023 Halema‘uma‘u eruption because it was being exposed to intense heat.

A view to the west across Pago Pago harbor at Matafao Peak on Tutuila Island, American Samoa. Matafao Peak is the highest part of Tutuila Island at an elevation of 2,142 feet (653 meters) above sea level. It is part of the Matafao Peak National Natural Landmark. USGS photo by D. Downs.

A view of Rainmaker Mountain to the east of Pago Pago harbor on Tutuila Island, American Samoa. Rainmaker Mountain was mapped in the 1940s as a trachyte plug by geologist Harold Stearns. Dense jungle, the highest annual rainfall in American Samoa, and its steep cliffs make it a formidable mountain to summit. USGS photo by D. Downs.

On August 8, 2023, HVO field engineers visited the UWE tiltmeter station near Kīlauea summit. Field engineers serviced the instrument, which was experiencing temporary date outages. USGS photo by M. Cappos.

Early morning photo of the three islands that make up the Manuʻa Islands in American Samoa. Ofu Island is in the foreground, Olosega Island in the middle ground, and Taʻū Island is in the background. Ofu-Olosega islands and Taʻū Island are the tops of volcanoes, most of which are under the ocean surface. USGS photo by D. Downs.

A view of the northwest side of Taʻū Island in American Samoa. This island is a shield volcano with small scoria cones on its upper flanks and tuff cones at sea level. The history of this volcano is currently being studied to better understand the eruptions that built it. The light brown material in the foreground at sea level is part of a tuff cone at Faleāsao.

A view of the southeast side of Olosega Island (foreground), with Ofu Island visible in the background. These volcanoes have steep cliffs and are separated by a 50-foot (15 meter) channel. The steep cliff in the photo is a dike sticking out into the ocean that has been more resistant to weathering than surrounding lava flows. USGS photo by D. Downs.

A view looking at the basalt lava flows that make cliffs along the southwestern part of Tutuila Island, American Samoa. These flows are part of the Leone volcanic series and form the flattest part of Tutuila Island, where the airport and population center of Tafuna are located. USGS photo by D. Downs.

The view looks south along the basalt cliffs and beaches at Tula point on the eastern end of Tutuila Island, American Samoa. Tutuila Island is a shield volcano, formed by basalt flows that are 1-1.5 million years old.

Low-angle aerial view of the Great Crack and surrounding 1823 lava flows (dark gray) along Kīlauea’s lower Southwest Rift Zone. The crack is about 50 feet (15 meters) wide in this area with similar but variable depth, depending on the amount of rock rubble filling the opening. USGS photo by D. Downs.

Image of jetting eruption at Stromboli volcano Italy (left), the orientation of the sensor compared to the eruption direction (center) and a close image of the hovering UAS with sensor on tether below (right-Image courtesy David Fee).   

On July 27, 2023, an HVO geologist sampled tephra from one of Kīlauea's largest explosive eruptions (900 CE) that is preserved in soil found on the volcano's south flank near the coast.

This reference map depicts the volcanoes in the Manuʻa Islands, American Samoa, the site of seismic unrest between July and September 2022. Marked on the map are the locations of Hawaiian Volcano Observatory GPS and seismometers in the islands.

Hawaiian Volcano Observatory geologists and a National Park Service archaeologist hike west along the Hilina Pali Trail on July 26, 2023. USGS photo by D. Downs. 

This reference map depicts the Kīlauea summit region following the most recent eruption in June 2023. The provided statistics for that eruption were measured during a Hawaiian Volcano Observatory helicopter overflight just days after the June 19 eruptive pause.

During July, HVO staff and collaborators install temporary instruments to collect magnetotelluric (MT) data on Kīlauea. At each location, electrodes, induction-coil magnetometers, and data loggers are deployed for about a month. This photo shows a magnetometer in the foreground being buried in a narrow and shallow trench to minimize wind noise.

A USGS geophysicist measures contact resistance on electrodes at a temporary magnetotelluric site. The electrodes require electrical contact with the ground and are buried in shallow holes about the width and depth of a spade head. Data collected by the instruments will help to image the structure and fluids beneath the surface of Kīlauea.