Images

The crater floor of Halema‘uma‘u at the summit of Kīlauea is covered with lava flows erupted since the current eruption began on September 29, 2022. These lava flows are a patchwork of different ages, with overflows and ooze-outs along the margin of the crater floor covering new portions of the crater floor at different times.

Unlike permanent seismic stations, which are placed farther apart and cover the entire Island of Hawai‘i, the temporary seismic nodes will be tightly grouped in order to more densely record earthquake signals across the region surrounding Pāhala.

Hawaiian Volcano Observatory (HVO) staff, along with collaborators from the University of Hawai‘i at Mānoa, are installing seismic nodes on the Southwest Rift Zone of Kīlauea this week as part of a project funded by the Additional Supplemental Appropriations for Disaster Relief Act of 2019 (H.R. 2157).

The magnetotelluric (MT) instruments pose no health risk to people or animals and over 1–2 days will collect data that will inform HVO and collaborating scientists about the subsurface structure and fluids.

Photo of the lava lake within Halema‘uma‘u Crater, at the summit of Kīlauea, taken at 11:47 a.m. HST on June 2, 2022. The photo is looking towards the northeast, with the west vent and active lava lake on the left side of the photo, partially obscured by abundant fumes. USGS photo by J.M. Chang.

View looking north of the active lava lake within Halema‘uma‘u Crater, at the summit of Kīlauea, during a volcano monitoring field shift on June 2, 2022. Spattering of lava occurred intermittently along the edges of the active lava lake basin, as shown by the orange areas on the north side of the basin.

During the first half of June, Hawaiian Volcano Observatory (HVO) staff, along with collaborators from other parts of USGS,  temporarily deployed instruments to collect ground-based magnetotelluric (MT) data to image structure and fluids beneath the surface of Kīlauea.

HVO staff and collaborators install temporary instruments to collect magnetotelluric (MT) data on Kīlauea volcano’s south flank. At each location, electrodes, induction-coil magnetometers, and data loggers are deployed for 1–2 days. This photo shows a magnetometer being prepared for burial in a narrow and shallow trench to minimize wind noise.

At each magnetotelluric (MT) site, three electrodes are installed. The electrodes require electrical contact with the ground and are buried in shallow holes about the width and depth of a spade head. The electrode is encapsulated in a canvas bag filled with bentonite, and water is poured in the electrode hole to improve the contact resistance.

Telephoto view of the west vent within Halema‘uma‘u Crater, at the summit of Kīlauea. USGS photo taken by J.M. Chang at 12:01 p.m. HST from the south rim. USGS photo by J.M. Chang.

Lava lake activity continues in Halema‘uma‘u, at the summit of Kīlauea Volcano. A small stream of lava was pouring into a small pond northwest of the main lava lake, near the west vent. USGS photo by M. Patrick.

This map of the Kīlauea summit is mostly identical to the May 16, 2022, eruption reference map, but also included here are west to east topographic profiles across the caldera.

Unoccupied aircraft systems (UAS) flights on May 18, 2022, allowed for aerial visual and thermal imagery to be collected of Halema‘uma‘u crater at the summit of Kīlauea. The active lake surface is limited to the western portion of the crater.

Unoccupied aircraft systems (UAS) flights on May 18, 2022, allowed for aerial visual and thermal imagery to be collected of Halema‘uma‘u crater at the summit of Kīlauea. The active lake surface is limited to the western portion of the crater.

A view of the active lava lake within Halema‘uma‘u, taken during a Kīlauea summit monitoring field shift on the morning of May 18, 2022. The active lake is draining into the small pond on the right of the photograph. Spattering along the margins of the lake is common, seen here in the center of the photograph.

The feature shown in the photograph is a drainage outlet for the active lava lake of Halema‘uma‘u, a crater within the summit caldera of Kīlauea volcano. Surface plates from the active lake surface are dragged into the outlet and churned up. A small standing wave, about 1 meter or 1 yard tall, is present in the center of the outlet structure.

The vent within Halema‘uma‘u, at the summit of Kīlauea, was degassing during a field observation visit on the morning of May 18, 2022. The vent is 56 feet tall (17 meters) and has a small puka (hole) visible with bright red glowing lava within on the right side of the photograph.

A view of Isaac Hale Beach Park (also known as Pohoiki) in the lower Puna District on the Island of Hawai‘i. Lava from the 2018 Kīlauea lower East Rift Zone eruption, emplaced in late July 2018, is visible on the left. USGS photo taken during a helicopter overflight on May 12, 2022, by N. Deligne.

 Ahuʻailāʻau (the cone built during the eruption of Fissure 8) was the most active vent during the 2018 lower East Rift Zone eruption of Kīlauea on the Island of Hawai‘i. During a USGS Hawaiian Volcano Observatory routine monitoring overflight on May 12, 2022, the prominent feature was visible in the row of fissures. USGS photo J. Schmith.

Kapoho Crater, with its lush green slopes, was surrounded by lava during the 2018 lower East Rift Zone eruption of Kīlauea. Lava flowed all the way around and into the center of the crater, covering the lower part of the cone. Now, the slopes of the crater form a Kīpuka, or area surrounded by younger lava flows. USGS photo by J. Schmith on May 12, 2022.

A view of the lava lake within Halema‘uma‘u at the summit of Kīlauea, taken during a helicopter overflight the morning of May 10, 2022. The image is taken from the east side of the crater looking to the west. The west vent cone complex can be seen in the far western side of the lake.