Images

Subtle steaming was visible at Pu‘u ‘Ō‘ō during HVO's overflight of Kīlauea on March 4, 2021. Steam is normally visible as the vent—which was active for more than 35 years—continues to cool, following the 2018 Pu‘u ‘Ō‘ō collapse.

Data from a Kīlauea summit helicopter overflight on March 4th allowed for the calculation of the depth of the lava in Halema‘uma‘u crater. The deepest parts of the lake (darkest reds) exceed 200 meters (650 feet). Different-colored lines in Halema‘uma‘u show the perimeter of the lava lake and the vents over the course of the eruption.

During a routine overflight of the Kīlauea East Rift Zone on March 4, HVO scientists visited the Pu‘u ‘Ō‘ō area to check for any significant changes in recent months. Their most notable observation was further accumulation of talus—rock collapse debris—in the crater that formed on April 30, 2018, as seen in this wide-angle photo.

The lava lake in Halema‘uma‘u crater remains active. This view looking to the northwest on Wednesday, March 4, 2021, focuses on the active portion of the lake; the eastern stagnant portion is out of view to the right. Lava enters the lake at the base of the western vent spatter cone (left).

Steam was also visible in other portions of the 2018 eruption flow field, close to Kīlauea's East Rift Zone (bottom portion of image). As lava was flowing south towards the ocean in 2018, lava channels formed; these channels are visible as dark grey meandering lines in the image. Like water, lava flows along the path of least resistance downslope. USGS image by K.

View of the Kīlauea summit lava lake taken from the west rim of Halema‘uma‘u at 12:21 p.m. HST on March 3, 2021. The western portion of the lava lake is active with lava being fed from the west vent. The eastern surface of the lava lake remains crusted over. SO₂ emission rates are elevated at approximately 1000 t/d, as measured on March 3, 2021.

The lava lake in Halema‘uma‘u crater, at the summit of Kīlauea, remains active. Lava is entering the lake at a small inlet along the western lake margin, at the site of the western fissure. Active surface lava remains limited to the western portion of the lake. Scattered crustal foundering and small overflows were present on Tuesday, March 2, 2021. USGS photo by M.

The western fissure in Halema‘uma‘u remains active, with incandescence visible in two small vent openings. The northeastern incandescent vent opening (right) has a narrow, drained lava channel extending down the flank of the cone. USGS photo taken by M. Patrick on March 2, 2021.

The eastern portion of the lava lake in Halema‘uma‘u remains solidified at the surface. Numerous islands, previously drifting in the lake currents, are now locked in place. The remnants of a section of Crater Rim Drive, from the 2018 summit collapse, is visible in the lower right corner of the photo. USGS photo taken by M. Patrick on March 2, 2021.

Another close-up view of the western fissure in Halema‘uma‘u, showing the incandescent lava upwelling at the inlet zone along the western lake margin. This photo was taken on March 2, 2021, in an area of Hawai‘i Volcanoes National Park that remains closed to the public due to safety reasons. USGS photo by M. Patrick.

On the afternoon of Friday February 26, 2021, the active west side of the lava lake at Halema‘uma‘u, Kīlauea Volcano, Hawaii, had numerous surface breakouts and foundering crust amid vigorous steaming due to the heavy rainfall. This view is looking to the east from the west side of 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). The map shows that the lava lake has filled 218 m (715 ft) of the crater, to an elevation of 735 m (2411 ft) asl since the eruption began at approximately 9:30 p.m. HST on December 20, 2020.

Heavy rains at the summit of Kīlauea Volcano (Hawaii) cleared on the afternoon of Friday, February 26, 2021, to show the steaming surface of the lava lake at Halema‘uma‘u viewed from the west.

 A telephoto image of the western fissure within Halema‘uma‘u crater, at the summit of Kīlauea Volcano. On Wednesday, February 24, 2021, the northern-most vent of the fissure was producing occasional weak bursts of spatter (center).

On Wednesday, February 24, HVO scientists observed the Kīlauea summit eruption in Halema‘uma‘u from the west rim of the crater. In this photo, the active western fissure is marked by an incandescent skylight on the near side of the lava lake.

A telephoto image of the small lava flow from the western fissure within Halema‘uma‘u, at the summit of Kīlauea. Occasional incandescence was visible (center) from the weakly active flow on the northwestern lava lake levee. A portion of the active lava lake is visible in the lower-right.

In the morning of Tuesday, February 23, a new source of spatter appeared on flank of the active western fissure within Halema‘uma‘u at the summit of Kīlauea. It started to feed a short lava flow down the spatter cone and onto the crusted northwest margin of the lava lake.

The lava lake in Halema‘uma‘u crater, at the summit of Kīlauea, remains active. Active surface lava remains limited to the western portion of the lake, shown here as seen from the south rim of the crater and looking towards the northwest. The western fissure cone is in the center of the photo.

This photo shows a view of the western fissure, feeding the lava lake in Halema‘uma‘u at the summit of Kīlauea. The inlet zone, where lava is entering the lake, is visible at the bottom of the photo. Near the center of the photo, an area of lava driblets can be seen running down the flank of the western fissure's cone. USGS photo by M. Patrick.

This photo shows the main island, just west of the lake center, in Halema‘uma‘u lava lake at the summit of Kīlauea. The recent drop in lake level, associated with ongoing summit deflation, is shown by the raised edge around much of the perimeter of the island. USGS photo by M. Patrick.

The lava lake in Halema‘uma‘u crater, at the summit of Kīlauea, remains active. Active surface lava remains limited to the western portion of the lake, shown here. Ongoing summit deflation has been associated with a slight drop in the lake level, now a few meters below the rim of the levee.