Images

HVO staff at work in the electronics workshop. On the right side, two types of 3D printers are used to produce parts: sample holders made from bioplastic, and aerial drone parts made from carbon fiber and nylon. On the left side, a computer screen shows the inside structure of composite drone parts. USGS photo by F.

View from the south looking at the western, active part of the lava lake in Halema‘uma‘u crater at the summit of Kīlauea. Effusion into the lava lake is slow and steady with a few red-orange incandescent patches of lava visible within the flat black part of the lava lake. The perched margin of the active lava lake is visible around its perimeter. USGS photo by D.

View from the south looking at the active west vent in Halema‘uma‘u at Kīlauea summit. The vent is mostly obscured by a plume of steam and sulfur dioxide, with a little spatter visible. A lava flow is slowly entering the lava lake from the base of the scoria cone that has been constructed around the west vent. USGS photo by D. Downs.

Lava continues to eruption from a vent on the western wall of Halema‘uma‘u crater and flow into the lava lake. The active area of the lava lake remains similar in size to the previous week. In the foreground, a down-dropped block containing a segment of the old Crater Rim Drive can be seen. The southeast flank of Mauna Loa is in the background.

Lava erupts through a perched lava pond in the active western vent of Halema‘uma‘u crater, and supplies lava to the lava lake. Spatter bursts like the one seen here disrupt the pond surface nearly continuously and occasionally throw lava outside the vent, building up the cone. This burst is approximately 5 meters (16 feet) tall. USGS photo taken by B.

This reference map depicts the ongoing Kīlauea summit eruption on November 19, 2021. One eruptive vent is active within Halema‘uma‘u at this time, along the western edge of the rising lava lake.

A telephoto photograph of the roiling 4-7 meter (13-23 ft) lava fountains of the western vent in Halema‘uma‘u crater at the summit of Kīlauea. The spatter cone is nearly circular, with only one outlet letting lava cascade east into the lake. Concentric lava crust rings form around where lava enters the lake from a single source with persistent flux.

During a helicopter overflight on November 16, 2021, HVO scientists monitored a thermal steaming area near Heiheiahulu, on Kīlauea's middle East Rift Zone. The expanse of this thermal area has not changed or expanded significantly since the previous overflight of the area in March 2021.

Regional map of southeastern Idaho showing the relative location of Yellowstone National Park and the Stanley earthquake aftershocks. Yellowstone National Park (outlined in yellow) is at least 275 km away from the 2020 M_w6.5 Stanley earthquake. Several active faults (in red) are located between the Stanley earthquake and Yellowstone Caldera.

Cumulative number of aftershocks greater than magnitude 2.5 following the March 30, 2020, magnitude-6.5 Stanley earthquake in central Idaho. The black line shows the observed aftershocks, the red line shows the predicted number of aftershocks. Aftershocks are a normal and expected phenomenon following strong tectonic earthquakes.

The ongoing eruption at Kīlauea summit continues to fill Halemaʻumaʻu crater with lava. A gas plume rises from the active vent on the west (left) side of the crater as lava flows from the vent into the rising lava lake (black surface).

A helicopter overflight on November 16, 2021, at approximately 8:30 a.m. HST allowed for aerial visual and thermal imagery to be collected of Halema‘uma‘u crater at the summit of Kīlauea. The scale of the thermal map ranges from blue to red, with blue colors indicative of cooler temperatures and red colors indicative of warmer temperatures.

A helicopter overflight on November 16, 2021, at approximately 8:30 a.m. HST allowed for aerial visual and thermal imagery to be collected of Halema‘uma‘u crater at the summit of Kīlauea. The scale of the thermal map ranges from blue to red, with blue colors indicative of cooler temperatures and red colors indicative of warmer temperatures.

This thermal image is looking west and shows the lava lake in Halema‘uma‘u, at the summit of Kīlauea. The active lava on the surface is limited to the west side of the lake, near the west vent. The eastern portion is solidified at the surface, with small ooze-outs often active along the lake perimeter.

The elevation of the surface of the lava lake within Halema‘uma‘u crater has now risen slightly above the level of the lowest down-dropped block from the 2018 collapse of Kīlauea summit. Overnight on November 15, 2021, a lava break-out from the edge of the lake allowed lava to flow onto the surface on the block.

HVO geologists observed ongoing eruptive activity with Halema‘uma‘u crater during a helicopter overflight of the Kīlauea summit on the morning of November 16, 2021. Lava continues to erupt from a vent on the west side (far side in this photo) of Halema‘uma‘u. Low winds allowed the plume to rise vertically above the crater.

Aerial view looking northeast of the eastern half of the Kīlauea summit caldera, taken during a helicopter overflight of the Kīlauea summit on the morning of November 16, 2021. The current lava lake in Halema‘uma‘u is visible in bottom left, and scarps associated with 2018 Kīlauea summit collapse are prominent in the center of the photo.

During a helicopter overflight of Kīlauea summit on the morning of November 16, 2021, this aerial view (looking southwest) of the lava flow erupted in September 1982 was captured. The September 1982 lava flow exited Kīlauea summit caldera through a narrow gap, visible near the center of the photo.

A view of the active west vent within Halema‘uma‘u crater, at the summit of Kīlauea, on November 15, 2021. A new flow has developed on the south side of the west vent cone (right side of photo), with lava moving from a source near the base of the cone toward the lava lake. Photo taken at 12:55 p.m. HST from the western rim of the crater. USGS photo by J.M.

A telephoto view of the flow on the south side of the west vent cone within Halema‘uma‘u crater, at the summit of Kīlauea. The direction of flow is from the west (bottom) to the east (top). Entrained pieces of solidified crust (black) can be seen in the flow and can be used to determine the direction of flow.

Lava continues to erupt from the west vent in Halema‘uma‘u, and supply the lava lake through a spillway in the spatter cone. On November 12, a small overflow of the perched lava lake levee was visible from the western crater rim. Overflows are an important process for building up perched levees, as they help add height and stability.