Images

The western fissure at Kīlauea's summit continues to send lava into Halemʻaumaʻu crater through an open channel into the lava lake. Around sunset on the evening of January 19, field crews observed a minor collapse event of the spatter rampart on its northern rim and the channel margins at 5:46 p.m. HST.

This photo, taken at just after 6 p.m. HST on January 19, shows that the western fissure continues to send lava into Halemʻaumaʻu crater through an open channel into the lava lake. The western side of the lava lake has an incandescent surface, while the eastern portion is more crusted over.

A close up of the vent area at the western fissure within Halema‘uma‘u at Kīlauea's summit. The two main vents were exhibiting low fountaining while a small vent in the middle had sporadic, weak spattering. USGS photo by M. Patrick.

A close up of the southwest portion of the lava lake within Halema‘uma‘u, just south of the west fissure. The lava lake at Kīlauea's summit is perched, and is contained by a steep levee 2-3 meters (yards) high. USGS photo by M. Patrick.

On the evening of January 17, the vent on the north side of the western fissure in Halema‘uma‘u at Kīlauea's summit activated and seemed to become the dominant vent overnight. This vent is the one on the right in this photo. The vent on the left, which was the dominant vent over the past week, seemed less energetic today. USGS photo by M. Patrick.

Sunlight interacts with volcanic gas from Kīlauea's summit lava lake and western fissure in this late afternoon view. The western fissure has built a spatter cone on the steep walls of Halema‘uma‘u, with lava spilling into the active lake, which forms the lower right portion of the photo.

A closer view of the low fountaining at the western fissure in  Halema‘uma‘u at Kīlauea's summit. The rim of the cone is built from accumulated deposits of spatter, and large chunks of the cone rim were observed to collapse from time to time. USGS photo by M. Patrick

Photos from a Scanning Electron Microscope (SEM) showing reacted rhyolite fragments at the end of the laboratory experiments. (a) Image magnified by 500 times showing the rhyolite after it reacted with water at 250 degrees Celsius (482 F). The reacted rhyolite fragments show very little change compared with the unreacted fragments.

Low fountaining continues at the western fissure, supplying lava to the lava lake in Halema‘uma‘u crater, at the summit of Kīlauea. The vent has formed a spatter cone around the fountaining, with lava spilling into an open channel that plunges into the lake.

Steam vents along the Yellowstone River near Mud Volcano thermal area, Yellowstone National Park.

Mudpot located in the Mud Volcano thermal area of Yellowstone National Park.  This type of thermal feature indicates an acid-sulfate system.

The west vent in Halemaʻumaʻu erupting and building a spatter cone complex, with lava cascades feeding a growing lava lake at Kīlauea summit. USGS photograph from January 11, 2021, by B. Carr.

A close up view of the spatter cone over the west vent, in Halema‘uma‘u crater at the summit of Kīlauea. This photo was taken on January 10, 2022, from within the closed area of Hawai‘i Volcanoes National Park. Hawaiian Volcano Observatory geologists monitor the eruption from within the closed area with NPS permission. USGS photo by M. Patrick.

The arrival of nightfall at Halema‘uma‘u on January 9, 2021, provided a clearer view of ongoing eruptive activity for USGS scientists monitoring the eruption this Saturday evening.

Looking southwest from the Steens Mountain summit area into the Alvord desert of eastern Oregon.  This fault-block escarpment reveals the oldest lava flows of the Columbia River Flood Basalts, which erupted about 17 million years ago.  Three or four vertical dikes that feed these flows are evident in the midground ridge where they stand as rock walls cutti

Around sunset on Saturday (January 9, 2021), a break in the rain allowed HVO scientists to visit and monitor the ongoing eruption in Halema‘uma‘u. The west vent is still actively effusing lava, but outflow into the lava lake is increasingly sluggish, as evidenced by slow-moving crustal plates near the once-vigorous vent outlet.

Kīlauea’s summit lava lake, in Halema‘uma‘u, just after sunset on January 8, 2021. This view is to the north, from the south rim of the crater.  HVO scientists continue to monitor the eruption within an area of Hawai‘i Volcanoes National Park that remains closed to the public for safety reasons. USGS image by N. Deligne. 

This photo, taken during an overflight of Kīlauea's summit this morning (January 7, 2021), shows the southeast margin of Halemaʻumaʻu's growing lava lake. The photo shows the boundary between the active portion of the lava lake (left) and the subtle levee around the lake perimeter that allows the lake to be slightly perched.

This thermal image, looking northwest, shows the distribution of activity on the lava lake at Kīlauea's summit. The lake is slightly perched and surrounded along its perimeter by a lower ledge of cooler lava. The western fissure, in the wall of Halema‘uma‘u crater, is visible in the upper left portion of the image, just above the lake.

During an overflight of Kīlauea summit today (January 7, 2021) at approximately 10:30 a.m. HST, HVO geologists captured this image of the growing lava lake within Halemaʻumaʻu. Sunny weather allowed for clear views of Mauna Loa, to the west. USGS photo by M. Patrick. 

Aerial image of the active west vent area and the largest island in Halemaʻumaʻu's growing lava lake. During the overflight of Kīlauea's summit today (January 7, 2021) at approximately 10:30 a.m. HST, HVO geologists noted that the dome fountain, which had been persistent near the base of the west vent area, had subsided and was no longer present. USGS photo by K.