Images

The western fissure remains active, supplying lava to the lava lake in Halema‘uma‘u Crater, at the summit of Kīlauea. This photo shows a close-up of the inlet where lava enters the lake. The motion of the lava stream has been slow but continuous. USGS photo by M. Patrick.

This photo shows a close-up of the inlet where lava enters the lake in Halema‘uma‘u Crater, at the summit of Kīlauea. A lava crust forms around the source of the lava stream, and occasionally fractures and is carried away by the current. Here, this sequence is beginning with a crack developing in the crust. USGS photo by M. Patrick.

The lava lake remains active in Halema‘uma‘u Crater, at the summit of Kīlauea. The surface area of the active lava lake has slowly decreased over the past several months, with the active surface lava now limited to a portion of the west side of lake. The lake remains perched several meters (yards) above its surroundings, bound by a steep levee on most sides.

The lava lake in Halema‘uma‘u crater, at the summit of Kīlauea, remains active. The active surface lava lake, shown in this photo, is limited to the western portion of the lake between the western fissure complex (center left) and the main island (right).

A close up of the inlet where lava from the western fissure feeds into the lava lake in Halema‘uma‘u, at the summit of Kīlauea. The lava stream was sluggish, with the movement barely perceptible with the naked eye. USGS photo by M. Patrick.

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 224 m (735 ft) of the crater, to an elevation of 741 m (2431 ft) asl since the eruption began on December 20, 2020.

Morning light illuminates the active west vent spatter cones from the ongoing Halema‘uma‘u eruption at Kīlauea Volcano's summit on Friday, March 26, 2021. Several of the cones were actively degassing but no spatter or lava flows were observed. USGS Photo by K. Lynn.

A close-up aerial view of the southern active lava lake margin within Halema‘uma‘u crater, at Kīlauea summit. The formation of the levee containing the “perched” active lava lake (center to upper-right) is partially due to crustal plates from the active lake surface being pushed onto the rim of the lava lake.

A helicopter overflight on March 26, 2021, at approximately 8 a.m. HST allowed for aerial visual and thermal imagery to be collected of the eruption within Halema‘uma‘u crater at the summit of Kīlauea Volcano.

This figure shows a comparison of ongoing activity in Halema‘uma‘u, at the summit of Kīlauea, with a 2007 lava channel on Kīlauea's East Rift Zone. On the left, a photo shows the levee that is containing the active perched lava lake in Halema‘uma‘u.

A telephoto view of the west vent within Halema‘uma‘u crater taken during a Hawaiian Volcano Observatory helicopter overflight of Kīlauea summit. The west vent continues to supply lava into the active western portion of the lava lake from two adjacent inlets at its base (center-left).

During today’s HVO helicopter overflight of the Kīlauea summit eruption, no major changes were observed. As the west vent continues to erupt lava into the active lava lake, volcanic gas emissions remain elevated, with a visible plume rising from the western vent (upper-right).

An aerial view of the western portion of the lava lake within Halema‘uma‘u crater at the summit of Kīlauea. The west vent (upper-right) continues to erupt lava into the perched active portion of the lava lake. The main island, which remains trapped in place by the solidified lava crust surrounding it, is visible at the bottom of the photo. USGS photo taken by L.

A wide view of the lava lake within Halema‘uma‘u crater at Kīlauea summit, taken on March 24, 2021 at 12:48 p.m. HST. A gas plume rises from the west vent (center-left), which continues to erupt lava into the active western portion of the lava lake (light gray in color). The center and eastern lava lake surface is covered by a darker, stagnant crust.

The lava lake in Halema‘uma‘u crater, at the summit of Kīlauea, remains active. Active surface lava is limited to the western (bottom) portion of the lake between the main island and the western fissure complex. In this view looking east, a 4 meter (13 feet) diameter skylight is visible at the top of the northeastern-most spatter cone (left). USGS photo by N.

The lava lake in Halema‘uma‘u crater, at the summit of Kīlauea, remains active. Active surface lava is limited to the western portion of the lake, and is impounded by steep, well-defined levees. USGS photo by M. Patrick on March 22, 2021.

A close up of the inlet where lava from the western fissure feeds into the lake in Halema‘uma‘u, at the summit of Kīlauea. The inlet is formed from two adjacent lava streams. USGS photo by M. Patrick.

This photo shows the levee that bounds the southern margin of the active lake in Halema‘uma‘u. The levee is formed, in part, by numerous small crustal plates pushed over the rim. USGS photo by M. Patrick on March 22, 2021.

This photo shows the northern portion of the active lava lake in Halema‘uma‘u, at the summit of Kīlauea. Like the southern portion of the lake, this northern zone is also contained by steep, well-defined levees. USGS photo by M. Patrick on March 22, 2021.

Crustal foundering—less-dense liquid lava overriding and sinking thin surface crust—is common in the lava lake within Halema‘uma‘u, at the summit of Kīlauea. Here, large sections of the crust are foundering, resurfacing the lake. USGS photo by M. Patrick on March 22, 2021.

This photo shows one of the islands near the inlet in the lava lake in Halema‘uma‘u, at the summit of Kīlauea. Over the past two weeks, the island has tilted 90 degrees, producing the vertical layering visible here. USGS photo by M. Patrick on March 22, 2021.