Images

Kīlauea eruption in Halema‘uma‘u on Jan. 1, 2021. The channel-like feature remains visible on the lava lake surface within Halemaʻumaʻu crater at Kīlauea Volcano's summit. This feature originates from the influx of lava from the western fissure. USGS photo by M. Patrick. 

Kīlauea's summit lava lake in Halemaʻumaʻu is continually re-surfacing. Like the 2008-2018 lava lake, the current lava lake is exhibiting crustal foundering, when fragments of solidified lava crust on the surface break and sink back into the liquid portion.  USGS photo by M. Patrick. 

The margins of the lava lake in Halema‘uma‘u are showing a subtle levee around the perimeter. The levees grow from repeated small overflows, and the rafting and piling of pieces of surface crust that fuse together into a barrier that impounds the lake.

Another telephoto view of the west vent area in Halema‘uma‘u, Kīlauea Volcano. The west vents are in the northwestern wall of Halema‘uma‘u crater; intermittent spattering at the vents has constructed a perched pointed cone on the crater wall. USGS photo by M. Patrick. 

On January 1, 2021, with permission from Hawai‘i Volcanoes National Park, HVO researchers set up temporary seismic instruments around Halema‘uma‘u crater to collect data that will help them learn more about how magma travels in the shallow magmatic plumbing system beneath Kīlauea Volcano.

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).

Kīlauea's summit lava lake in Halemaʻumaʻu is continually re-surfacing. HVO geologists monitoring the activity in the field have observed crustal foundering, in which pieces of solidified lava crust on the surface of the lava lake break and sink back into the liquid portion. USGS photo by M. Patrick on 12/31/2020. 

The western fissure in Halemaʻumaʻu wall remains active. Glowing vents and a prominent spatter cone are visible in this photo. This view looks steeply down from Kīlauea's west caldera rim, and the lava lake surface is visible in the background. USGS photo by M. Patrick on 12/31/2020. 

View of the northern portion of the lava lake within Halemaʻumaʻu crater at Kīlauea Volcano's summit. Smaller islands present in the northeastern portion of the lava lake are visible. USGS photo by M. Patrick on 12/31/2020. USGS photo by M. Patrick on 12/31/2020. 

Left: magnified view of erupted material, including Pele’s hair and tears, as seen under a microscope (USGS Photo by K. Lynn on 12/26/2020). Middle: Zoomed in electron image of the tephra, where greyscale indicates the relative abundance of iron (Fe).

The figure shows changes in the propagation speed of ocean noise signals (red filled circles) through Kīlauea volcano from September 2020–February 2021. Positive values indicate a speedup in the propagation speed of ocean noise while negative values indicate a velocity slowdown.

Kīlauea's summit lava lake in Halemaʻumaʻu is continually re-surfacing. HVO geologists monitoring the activity in the field have observed crustal foundering, in which pieces of solidified lava crust on the surface of the lava lake break and sink back into the liquid portion. USGS photo by M. Patrick on 12/31/2020. 

The view from Kīlauea Volcano's western caldera rim shows the eastern portion of the lava lake in Halemaʻumaʻu crater. The main island is visible in the bottom of the photograph, and smaller islands can be seen above it (to the east). USGS photo by M. Patrick on 12/31/2020. 

A channel-like feature is visible on the lava lake surface within Halemaʻumaʻu crater at Kīlauea Volcano's summit. This feature originates from the influx of lava from the western fissure, just out of view on the bottom of the photograph. USGS photo by M. Patrick on 12/31/2020. 

View of the northern portion of the lava lake within Halemaʻumaʻu crater at Kīlauea Volcano's summit. Smaller islands present in the northeastern portion of the lava lake are visible. USGS photo by M. Patrick on 12/31/2020. 

The western fissure in Halemaʻumaʻu wall remains active. Glowing vents and a prominent spatter cone are visible in this photo, which shows some spattering at the vent. This view looks steeply down from Kīlauea's west caldera rim, and the lava lake surface is visible in the background. USGS photo by B. Carr on 12/31/2020. 

Annotated eruption photograph taken at 5 p.m. HST on December 30, 2020, from the south rim of Halemaʻumaʻu, Kīlauea Volcano summit. USGS photo by K. Lynn. 

HVO field crews observed activity within Halema‘uma‘u, at Kīlauea Volcano's summit, overnight from within a closed area of Hawai‘i Volcanoes National Park. The area remains closed to the public for safety reasons and HVO field crews are equipped with a range of specialized safety gear and personal protective equipment.

HVO scientists monitor the ongoing Kīlauea summit eruption from within an area of Hawai‘i Volcanoes National Park that remains closed to the public for safety reasons. They are equipped with a range of specialized safety gear and personal protective equipment such as gas masks, helmets, gloves, and eye protection.

This photo, taken at approximately 5:30 a.m. December 29, 2020, shows Kīlauea's ongoing summit eruption. The western vent in the wall of Halema‘uma‘u continued to erupt overnight, and the northern/eastern vent remained inactive. At approximately 3:45 a.m. HST today (Dec.

HVO field crews observed the continuing eruption in Halema‘uma‘u at Kīlauea's summit early this morning. Overnight, the western vent in the wall of Halema‘uma‘u continued to erupt, and the northern/eastern vent remained inactive. At approximately 4:30 a.m. HST today (Dec. 28), HVO field crews measured the lava lake as 179 m (586 ft) deep.