Images

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.

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.

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 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.

A telephoto view of a small overflow to the 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.

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.

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.

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.

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 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.

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.