Images

Another GPS survey benchmark being occupied on Mauna Loa. The metal disk on the ground beneath the tripod is the benchmark, which is cemented to the lava flow surface.

Hawaiian Volcano Observatory geophysicists continue performing the annual GPS survey of Mauna Loa. Most Mauna Loa GPS campaign survey sites have been occupied every year since the early 1990s, whereas less active volcanoes Hualālai and Haleakalā are surveyed every 3–5 years.

The Vibroseis truck operating on Hilina Pali Road in Hawai‘i Volcanoes National Park on May 26, 2023. Throughout the month of May, the truck was generating seismic signals that will help to provide a new detailed view of shallow subsurface structures and the magma system beneath Kīlauea volcano’s summit.

The Vibroseis truck operating on Hilina Pali Road in Hawai‘i Volcanoes National Park on May 26, 2023. The vehicle belongs to the Natural Hazards Engineering Research Infrastructure (NHERI) experimental facility at the University of Texas at Austin, which is supported with funding from the National Science Foundation.

Map of the Mauna Loa 2022 eruptive fissures, shown as red lines. Red shaded area indicates lava flows produced during the eruption, around the fissure vent areas. Solid white line indicates mapped outer caldera boundary. White dotted line indicates inferred outer caldera boundary that is buried by historic Mauna Loa lava flows. Fissures on map were documented by C.

Lava samples collected near Mauna Loa’s fissure 3 vent (shown in this December 7 overflight photo) are glassy and contain bubbles and some very small (200 microns or 0.008 inches long) minerals like plagioclase and pyroxene, as shown in the grey-scale microscope image inset. USGS photos by Kendra J. Lynn. 

HVO geologists on an early morning helicopter overflight captured this scene of Kīlauea and Mauna Loa. The weather patterns at the time of the flight were causing the plume to stagnate and sit in Halema‘uma‘u, creating this haze shown in the caldera. Lava is still actively erupting within Halema‘uma‘u, seen here as the orange glow. USGS image by L. Gallant.

A view of HVO's old office building and the Jaggar Museum captured on an early morning overflight of Kīlauea summit. An inversion layer is sitting in the saddle between Kīlauea and Mauna Loa. An inversion layer forms when there is a temperature inversion of the atmosphere (warm air on top of cold air).

A tumbleweed of Pele’s hairs—collected near Saddle Road on November 29, 2022—viewed under a microscope. The scale bar in the lower right is 750 micrometers (0.03 inches) wide. The golden-brown glass strands are intertwined, whereas the thicker dark glass is rigid. The shape of the darker glass reflects the shape of the lava droplets as they quenched.

View from Kailua-Kona of Mauna Loa lava flows from the south caldera during the early morning hours of November 28, 2022. Photo courtesy of Ilya Bilyk. 

A tripod on Mauna Loa's summit and holding a GPS antenna for the Hawaiian Volcano Observatory's post-eruption survey of Mauna Loa was iced in during the recent Kona low storm. The ice broke away easily and there was no damage to the equipment.

Hawaiian Volcano Observatory geophysicist Ingrid Johanson checks on a survey-mode GPS instrument deployed near the summit of Mauna Loa. This survey will supplement HVO's network of continuous GPS instruments and provide higher spatial density of measurements for how Mauna Loa deformed during the recent eruption.

As of 7:00 a.m. on December 12, Hawaiian Volcano Observatory geologists observed only residual incandescence and no lava movement in the fissure 3 vent on the Northeast Rift Zone of Mauna Loa. The channels below the vent appear drained of lava and no longer feed the main flow front. USGS image by F. Trusdell. 

The Northeast Rift Zone eruption of Mauna Loa that began the evening of November 27, 2022, continues at greatly reduced levels as of December 12, 2022 (fifteenth full day). Only incandescence was observed within fissure 3 overnight. This morning, field crews heard small explosions accompanied by sprays of spatter from the west end of the fissure 3 vent.

The Northeast Rift Zone eruption of Mauna Loa that began the evening of November 27, 2022, continues at greatly reduced levels as of December 11, 2022 (fourteenth full day). Only incandescence was observed within fissure 3 overnight.

View of fissure 3 the morning of December 10, 2022. As of 7:00 a.m. on December 10, a lava pond replaced the fountains at the fissure 3 vent. The pond fed short lava flows that extended only 1.6 mi (2.6 km) from the vent but are already stagnating. USGS image by K. Mulliken. 

Aerial view of the fissure 3 cone on the Northeast Rift Zone of Mauna Loa. On December 10, 2022, Hawaiian Volcano Observatory geologists noted there are no fountains present in fissure 3. Only a lava pond is present with minor circulating activity. Photograph by K. Mulliken.

Aerial view of the fissure 3 cone on the Northeast Rift Zone of Mauna Loa. On December 10, 2022, Hawaiian Volcano Observatory geologists noted there are no fountains present in fissure 3. Only a lava pond is present with minor circulating activity. Photograph by K. Mulliken.

Aerial view of the fissure 3 cone on the Northeast Rift Zone of Mauna Loa. On December 10, 2022, Hawaiian Volcano Observatory geologists noted there are no fountains present in fissure 3. Only a lava pond is present with minor circulating activity. USGS image by J. Bard.

Just days, ago, lava was full in the channels from the fissure 3 eruption on Mauna Loa's Northeast Rift Zone. Over the past two days, the eruption output has greatly reduced. A pond of lava in the fissure 3 cone feeds short lava flows that extended only 1.6 mi (2.6 km) from the vent.

Just days, ago, lava was full in the channels from the fissure 3 eruption on Mauna Loa's Northeast Rift Zone. Over the past two days, the eruption output has greatly reduced. A pond of lava in the fissure 3 cone feeds short lava flows that extended only 1.6 mi (2.6 km) from the vent.