Volcano Hazards Program Office

Scanning electron microscopy (SEM) images of the Colloidal Pool colloids (images are a combination of backscatter and secondary electrons). The colloids are a mixture of clay particles, hydrated silica, alunite, and diatoms. (a) Image shows how hydrated silica (the whispy, lighter colored precipitate) uses larger particles, such as dust, clay, or things like pine needles

Sherrod, D.R., Sinton, J.M., Watkins, S.E., and Brunt, K.M., 2021, Geologic map of the State of Hawaiʻi: U.S. Geological Survey Scientific Investigations Map 3143, pamphlet 72 p., 5 sheets, scales 1:100,000 and 1:250,000, https://doi.org/10.3133/sim3143.

View from the south looking at the active west vent in Halema‘uma‘u at Kīlauea summit. The vent is mostly obscured by a plume of steam and sulfur dioxide, with a little spatter visible. A lava flow is slowly entering the lava lake from the base of the scoria cone that has been constructed around the west vent. USGS photo by D. Downs.

View from the south looking at the western, active part of the lava lake in Halema‘uma‘u crater at the summit of Kīlauea. Effusion into the lava lake is slow and steady with a few red-orange incandescent patches of lava visible within the flat black part of the lava lake. The perched margin of the active lava lake is visible around its perimeter. USGS photo by D. Downs.

Lava continues to erupt from a perched lava pond within the west vent of Halema‘uma‘u crater at the summit of Kīlauea. This photo shows spatter bursts through the pond and a roiling and sloshing pond surface, as well as a white-trailed tropicbird (koa‘e kea).. These birds make their homes in the walls of Halema‘uma‘u crater and are frequently seen flying around the crater

Lava continues to erupt from a perched lava pond within the west vent of Halema‘uma‘u crater at the summit of Kīlauea. This video shows nearly continuous spatter bursts through the pond and a roiling and sloshing pond surface. At about 43 seconds into the video, a white-trailed tropicbird (koa‘e kea) flies through the frame. These birds make their homes in the walls of

Lava continues to eruption from a vent on the western wall of Halema‘uma‘u crater and flow into the lava lake. The active area of the lava lake remains similar in size to the previous week. In the foreground, a down-dropped block containing a segment of the old Crater Rim Drive can be seen. The southeast flank of Mauna Loa is in the background. USGS photo taken by B. Carr

Lava erupts through a perched lava pond in the active western vent of Halema‘uma‘u crater, and supplies lava to the lava lake. Spatter bursts like the one seen here disrupt the pond surface nearly continuously and occasionally throw lava outside the vent, building up the cone. This burst is approximately 5 meters (16 feet) tall. USGS photo taken by B. Carr on November 23,

This reference map depicts the ongoing Kīlauea summit eruption on November 19, 2021. One eruptive vent is active within Halema‘uma‘u at this time, along the western edge of the rising lava lake. Similar to the last eruption—from December 2020 until May 2021—the eastern end of the lava lake has stagnated and solidified, and sits several yards (meters) lower than the

A telephoto photograph of the roiling 4-7 meter (13-23 ft) lava fountains of the western vent in Halema‘uma‘u crater at the summit of Kīlauea. The spatter cone is nearly circular, with only one outlet letting lava cascade east into the lake. Concentric lava crust rings form around where lava enters the lake from a single source with persistent flux. USGS image by C.

This thermal image is looking west and shows the lava lake in Halema‘uma‘u, at the summit of Kīlauea. The active lava on the surface is limited to the west side of the lake, near the west vent. The eastern portion is solidified at the surface, with small ooze-outs often active along the lake perimeter. One of these ooze-outs has recently flowed a short distance onto the