Images

View of the west vent cone and outlet channel in Halema‘uma‘u crater, at the summit of Kīlauea. On the lower left is an overflow (orange), where lava breached a levee and started flowing into a lower area to the west. Photo taken at 1:40 p.m. HST on Nov. 12, 2021, from the western rim. USGS photo by J.M. Chang.

A telephoto view of the overflow north of the west vent in Halema‘uma‘u crater, at the summit of Kīlauea. The flow direction is from east (top) to west (bottom) in the photo, and the height of the overflow is approximately 1 meter (3.3 feet). Black chunks of cooled crust can be seen entrained in the flow. Photo taken at 1:18 p.m. HST on Nov.

A telephoto view of spatter erupting from the west vent in Halema‘uma‘u crater, at the summit of Kīlauea. Photo taken at 2:42 p.m. HST on Nov. 12, 2021, from the western rim. USGS photo by J.M. Chang.

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.

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.

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.

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 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 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.

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).

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).

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.

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.

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.

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.

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 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.

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. 

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.

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.

A telephoto image of the west vent in Halema‘uma‘u, taken from the northwest rim on November 3. Low roiling lava continues to erupt from the west vent, with occasional larger bursts of spatter. The spatter cone that has built up since the eruption began on September 29, contains ponded lava that supplies the lava lake through the tubed-over spillway.