Images

An aerial view of Halema‘uma‘u crater from the northeast during a helicopter overflight of the Kīlauea summit eruption on February 1. The dull black color on the eastern (lower left) portion of the lava lake is the inactive surface.

A closer view of the lava lake in Halema‘uma‘u crater from the helicopter. Most of the lake surface in the foreground (east) is solidified on the surface, with active lava limited to the western end of the lake, in the distance. Rockfall debris can be seen on the southern margin of the lake (left side of photo). USGS photo by M. Patrick.

Rockfalls have been a frequent occurrence in Halema‘uma‘u crater, both before and during the current eruption. Debris from a recent rockfall can be seen sitting on the solidified lava lake crust (center). The crust on the southern edge of the lava lake is thick enough to support the weight of the boulders that have fallen. USGS photo taken by B.

Eruptive activity continues in Halema‘uma‘u crater, at the summit of Kīlauea. The active surface lava remains largely confined to the western (left) portion of the lava lake. As of the afternoon of January 31 lava had filled about 212 m (695 ft) of Halemaʻumaʻu in the active western portion of the lava lake. USGS photo by M. Patrick.

A close-up view of the main island near the center of the lava lake in Halema‘uma‘u. All the islands have been stationary since approximately January 10. USGS photo by M. Patrick.

A close-up view of the western fissure, which is supplying lava to the lava lake in Halema‘uma‘u crater. A slow-moving lava stream marked the inlet where lava entered the lake. Several incandescent openings remain over the vent region. USGS photo by M. Patrick.

A close-up view of the leading edge of the active lobe of surface lava slowly moving south in the central part of the Halema‘uma‘u lava lake. USGS photo by M. Patrick.

A view of the central region of the lava lake in Halema‘uma‘u. On the left is the main island. In the center, a lobe of surface lava is moving south (towards the bottom of the photo) as surface crust founders along its leading edge.

Hawaiian Volcano Observatory geologists collect tephra from the December 2020 deposit, found in the Southwest Rift Zone of Kīlauea Volcano on January 29, 2021.

View of the active west vent from the south rim of the Halemaʻumaʻu crater on January 29, 2021. The west vent is almost completely crusted over and the effusion is slow from the base of the spatter cone. This photograph was taken from an area of Hawai‘i Volcanoes National Park that remains closed to the public for safety reasons.

HVO scientists observed the Halema‘uma‘u lava lake from the southern crater rim in the late afternoon on Tuesday. In this view, the active western fissure at Kīlauea's summit is visible to the left. The circulating western portion (left) of the lava lake has a more silvery color than the stagnant eastern portion (right).

This close-up view of the active western fissure in Halema‘uma‘u at Kīlauea's summit was captured through the lens of a laser ranging device used by HVO scientists to measure distances to features within the crater.

This map of Halema‘uma‘u at the summit of Kīlauea shows 20 m (66 ft) contour lines (dark gray) that mark locations of equal elevation above sea level (asl).

Cycles in Kīlauea's summit eruptive vigor were present on January 22 and 23, with the lava channel at Halema‘uma‘u's western fissure alternating between high and low flow rates over periods of 5-6 minutes. USGS photos by M. Patrick.

Active lava reached as far as the central lake in Halema‘uma‘u at Kīlauea's summit, on the east side of the main island, where crustal foundering was occasionally happening. USGS photo by M. Patrick.

Active lava was again limited to the western half of the lava lake in Halema‘uma‘u at Kīlauea Volcano's summit. The western vent remained active with cycles of eruptive vigor in the open channel lasting 5-6 minutes. USGS photo by M. Patrick.

Activity at the west vent within Halemaʻumaʻu crater on January 22 included frequent spattering from multiple locations and an open lava channel which drops 20 meters (65 feet) from its source to the lava lake surface.

Between overcast and rainy weather, HVO field crews took this photo at 3:34 p.m. HST on January 21, 2021, from the south side of Kīlauea's summit caldera. The photo shows Halema‘uma‘u's active west vent, which overflowed its tubed-over lower half at 2:51 p.m.

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.