Images

Mauna Loa summit webcams have been down for several months due to wind damage at the radio telemetry site. On November 7, 2024, HVO staff visited the site and performed a partial fix that brought the webcams back online. Further visits will be needed to repair damaged solar panels. USGS photo by M. Patrick.

On August 2,2024, Hawaiian Volcano Observatory Gas Scientists flew via helicopter to the Sulfur Cone Multi-Gas instrumentation site on Mauna Loa's Southwest Rift Zone, which is at an elevation of 3,430 meters (11,240 feet) above sea level.

This photograph shows the inside of the Hawaiian Volcano Observatory (HVO) Multi-Gas site at Sulfur Cone. Currently, HVO has 2 of these continuous gas monitoring sites in operation on the Island of Hawai‘i. This one at Sulfur Cone high on Mauna Loa's Southwest Rift Zone, along with one at the summit of Kīlauea.

This photograph shows the inside of the Hawaiian Volcano Observatory (HVO) Multi-Gas site at Sulfur Cone. Currently, HVO has 2 of these continuous gas monitoring sites in operation on the Island of Hawai‘i. This one at Sulfur Cone high on Mauna Loa's Southwest Rift Zone, along with one at the summit of Kīlauea.

The continuously monitoring Multi-Gas instrument at Sulfur Cone is housed inside the black Pelican case shown here. Air is pulled into the instrument via a small pump to be analyzed for volcanic gases (Sulfur Dioxide, Hydrogen Sulfide, Carbon Dioxide and Water Vapor).

A Hawaiian Volcano Observatory gas scientist works on installing a newly calibrated Multi-Gas instrument at the Sulfur Cone gas monitoring site high up on Mauna Loa's Southwest Rift Zone at an elevation of 3,430 meters (11,240 feet) above sea level. USGS photo by M. Cappos.

Map of Island of Hawaiʻi, highlighting the four active or potentially active volcanoes of the Island, the number of people living on each volcano based on 2020 census data, major roads (transportation corridors) and minor roads (proxy for population density), when each volcano last erupted, and each volcano’s national threat assessment designation.

A benchmark on Mauna Loa being surveyed by GPS campaign instruments. The metal disk on the ground beneath the tripod is the benchmark, which is cemented to the lava flow surface. USGS photo by A. Ellis.

HVO staff are conducting the annual Mauna Loa GPS campaign. During the survey, GPS instruments are deployed at established benchmarks so that their recorded positions can be compared with those from previous years to discern subtle patterns of ground deformation associated with volcanic activity.

GPS campaign equipment being staged prior to deployment on Mauna Loa for the annual survey. Temporary GPS receivers and antennas are placed on tripods centered over benchmarks, which serve as a reference point for centering of the antenna. The equipment is left in place to collect data for a couple of days at each site.

This map shows recent deformation at Kīlauea from April 19 to May 5, 2024, as recorded by the Italian Space Agency's (AGI) 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 motion indicative of inflation as the magma reservoi

Aerial view of cone that the new MLDcam is located on, on the Southwest Rift Zone of Mauna Loa. An HVO geologist and field engineer installing the camera are silhouetted on top of the cone against the cloudy backdrop.

Distribution of permanent seismic stations and previously deployed seismic nodes in southern half of the Island of Hawai‘i. Shaded regions display the total footprint that nodal deployments this spring and summer will occupy. 

The new MSPwebcam can be remotely controlled at the observatory to zoom in on an area of interest on the Southwest Rift Zone of Mauna Loa. This photo looks north and shows the upper portion of Ocean View Estates. USGS photo by M. Patrick.

An HVO physical science technician installs a new webcam near South Point, looking north to monitor any future activity on Mauna Loa's Southwest Rift Zone. USGS photo by M. Patrick.

Plot showing the distance between two GPS stations on Mauna Loa from February 2022 to November 2023. Station MOKP is on the north side of Mokuʻāweoweo and station MLES is east of Mokuʻāweoweo. This plot shows how the distance between these two stations increased before the 2022 Mauna Loa eruption, indicating that the volcano was inflating.

Map showing the locations of earthquakes beneath Mauna Loa between October 31, 2023, and November 9, 2023. The earthquake colors indicate their depth. Most earthquakes have occurred at depths of 40–60 km (25–37 mi) beneath Mokuʻāweoweo, though some have occurred at shallower depths within 16 km (10 mi) of the ground surface. USGS map.

A view of Moku‘āweoweo (Mauna Loa's summit caldera) from the rim on the northwest side. The lava flows that flooded much of the caldera floor during the brief summit phase of the 2022 eruption are nearly indistinguishable from previous lava flows.

On November 8, 2023, Hawaiian Volcano Observatory staff visited the rim of Moku‘āweoweo (Mauna Loa's summit caldera) to service the MLcam and the MTcam. These cameras had been temporarily offline and not transmitting images.

Thumbnail image for Mauna Loa 2022 eruption anniversary video. Mauna Loa is Earth's largest active volcano and covers just over half of the Island of Hawaiʻi. It erupted most recently in November-December 2022, and it will erupt again.

An HVO gas scientist carrying portable gas sensor (yellow box) near Mauna Loa summit in June 2023. The white material on the ground in this photo is snow. USGS photo by P. Nadeau.