Images

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.

This reference map depicts the ongoing Kīlauea summit eruption on November 11, 2021. One eruptive vent is active within Halema‘uma‘u at this time, along the western edge of the rising lava lake.

HVO geologists conducted a helicopter overflight of Halema‘uma‘u, at the summit of Kīlauea, on the morning of November 9. A gas plume can be seen rising from the west vent along the crater wall (center left). Mauna Loa is visible in the background. USGS photo by B. Carr.

Following a brief—about one day—decrease in activity from November 7–8, the effusion rate within Halema‘uma‘u crater increased again on November 9. The active lava lake surface, which significantly shrunk during the lower-level of activity, has since grown back to it's previous size.

A helicopter overflight on November 9, 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 telephoto view of the western lava lake in Halema‘uma‘u, at the summit of Kīlauea. Around 10:00 a.m. on November 9, geologists in the field witnessed lava from the western part of the active lava lake (right) flowing onto an area of cooled solidified crust (left).

An aerial telephoto view of the western vent in Halema‘uma‘u crater on the morning of November 9. Spattering at the west vent occasionally reached above the level of the cone rim. The ponded lava within the cone was supplying lava to the lake from a tubed over spillway that is slightly elevated above the lava lake surface. USGS photo taken by B. Carr.

During a helicopter overflight of Halema‘uma‘u crater on November 9, HVO geologists observed spattering within the west vent cone and lava entering the lake via a spillway that is now tubed-over. Sulfur dioxide (SO₂) emission rates remain elevated with the largest volcanic gas plume coming from the west vent. USGS photo by B. Carr.

A telephoto view of the west vent along the western wall of Halema‘uma‘u crater at the summit of Kīlauea. On November 9, spatter bursts in the west vent cone triggered sloshing on the surface of the ponded lava. Spatter was thrown about 6–9 m (20–30 ft) above the pond surface and occasionally deposited onto the rim of the cone. USGS photo by J. Schmith.

This compilation of recent thermal maps shows the evolution of the lava lake in Halema‘uma‘u 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 telephoto view of the west vent along the western wall of Halema‘uma‘u crater at the summit of Kīlauea. On November 9, spatter bursts in the west vent cone triggered sloshing on the surface of the ponded lava. Spatter was thrown about 6–9 m (20–30 ft) above the pond surface and occasionally deposited onto the rim of the cone.

A wide view of the lava lake in Halema‘uma‘u taken during a helicopter overflight on the morning of November 9, 2021. Lava is once again visible in the spillway of the west vent after a brief drop in activity on Monday, November 8.

A helicopter overflight on November 9, 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 view of the Halema‘uma‘u lava lake taken during a helicopter overflight on the morning of November 9, 2021. Lava is visible in the spillway and in the west vent on the far side of the lava lake (center). There are also several small perched overflows in the northwest quadrant of the lake (near center between the vent and main island). USGS photo by L. Gallant.

A telephoto view in the same area of the western lava lake surface within Halema‘uma‘u. Lava continued to flow from the active western lake surface (right) onto the lower area of cooled solidified crust just north of it (left).

On the morning of November 9, a wispy volcanic gas plume (lower left) was visible over Halema‘uma‘u crater, at Kīlauea summit. As the hot plume rose to meet the cool morning air, water vapor formed a cloud above the crater. USGS photo by J. Schmith.

The extent of the active lava lake surface (lower right) within Halema‘uma‘u crater, at the summit of Kīlauea, had decreased substantially over the previous day and (at the time of this photo) was limited to the area around the west vent. This photo was taken at 5:48 p.m. HST on November 8, 2021, from the western rim of the crater. USGS photo by J.M. Chang.

Despite the temporary decrease in activity at Halema‘uma‘u crater, at the summit of Kīlauea, spattering was still visible within the west vent cone. This telephoto image was taken from the western rim of the crater during a lower level of eruptive activity on November 8, 2021. USGS photo by J.M. Chang.

This reference map depicts the ongoing Kīlauea summit eruption on November 4, 2021. One eruptive vent is active within Halema‘uma‘u at this time, along the western edge of the rising lava lake.

A photo of the west vent and active western portion of the lava lake within Halema‘uma‘u, at Kīlauea summit. The eastern side of the lava lake (out of view to the right), has a stagnant solidified crust on the surface. USGS photo taken by L. DeSmither on November 3, 2021.

The vent in the western wall of Halema‘uma‘u continues to erupt at the summit of Kīlauea. Volcanic gas emissions, primarily from the west vent (right), remain elevated. Sulfur dioxide (SO₂) emission rates were measured at around 3,600 tonnes per day on October 28, 2021. USGS photo taken on November 3, 2021, by L. DeSmither.