Images

Close up of Sheet 2 of "Lava inundation zone maps for Mauna Loa, Island of Hawai‘i," recently published by the U.S. Geological Survey. Colors depict lava Inundation zones for the Kaumana, Waiākea, and Volcano-Mountain View regions on Mauna Loa. Yellow indicates the volcano's Northeast Rift Zone, one area along which lava could erupt.

The lava lake within Halema‘uma‘u, a crater at the summit of Kīlauea, was about 30 m (98 ft) below the vent rim on the day of this photo (January 7, 2016).

Animated GIF of lava bubbling up from Kīlauea Volcano in Hawaiʻi Volcanoes National Park. The source of the GIF comes from footage found within the USGS video: Kīlauea Summit Eruption | Lava Returns to Halemaʻumaʻu.

The 1917 Curtis relief model of Kīlauea Volcano's summit shows many well-known geologic features, including the summit caldera (large depression), Halema‘uma‘u (crater within the caldera), Kīlauea Iki (crater at far right), and elaborate drainage patterns (foreground). Photo by Burr A. Church.

This view of Halema‘uma‘u as it appeared in the 1917 relief model by George Carroll Curtis shows fine details around the crater, including the first road for automobiles, which ended near the crater rim. The light-colored circular feature around Halema‘uma‘u is a nearly continuous escarpment along which subsidence occurred. Photo by Burr A. Church.

Aerial view of Mauna Loa erupting on the morning of March 25, 1984, the first day of the volcano's most recent eruption. The lava flow was advancing southeast, toward Kīlauea, from fissure vents at an elevation of about 11,200 feet on Mauna Loa's Northeast Rift Zone. Moku‘āweoweo, Mauna Loa's summit caldera, is visible at top left.

A USGS Hawaiian Volcano Observatory geologist monitored the advance of an ‘A‘ā lava flow on April 6 during the 1984 Mauna Loa eruption. This flow was about 4 m (13 ft) high and advancing at a rate of 50 m (55 yards) per hour. Lava reached within 6 km (4 mi) of Hilo city limits before the 22-day-long eruption ended on April 15.

Spattering is common in Kīlauea Volcano's summit lava lake, and consists of many large bursting gas bubbles. The fluid nature of the lake can be seen when lava hits the wall and flows downward like syrup. The thin, flexible nature of the crust is also shown here, as the bursting gas bubbles rip and fold the thin skin on the lake.

USGS Hawaiian Volcano Observatory field engineers begin the process of lowering a tiltmeter into a deep borehole on the west flank of Mauna Loa. The installation is guided by a custom-built apparatus that includes a 3-D printed jig. This tiltmeter will help monitor the currently elevated activity of Mauna Loa Volcano. USGS photo.

This perched lava channel, which was as much as 150 feet (45 meters) above the ground, carried lava downslope from the Pu‘u ‘Ō‘ō Fissure D vent during episode 58 of Kīlauea Volcano's ongoing East Rift Zone eruption. The channel was the main path for lava between July and November 2007. Episode 58 continued until early March 2011.

Charcoal collected from under the base of a pāhoehoe flow in a black sooty zone over orange ash.  The black sooty zone represents the region where the vegetation was converted to charcoal.  The hammer is approximately 13 inches long. USGS photo by F. Trusdell. 

A beautiful sunset over Mauna Loa (in distance at left) provided a backdrop to the lava lake within Halema‘uma‘u. HVO and Jaggar Museum are on the horizon near the center of the panorama.

Kīlauea Volcano's Kamokuna ocean entry photographed on May 23, 2017 (left) and July 13, 2017 (right) show how lava flowing from the tube has both widened and thickened the delta. Near the sea cliff, the delta appears to have doubled in thickness over the past seven weeks, creating a distinctly sloped surface from the base of the cliff to the sea.

"Geologic map of the northeast flank of Mauna Loa volcano, Island of Hawai‘i," published by the U.S. Geological Survey in May 2017, shows the distribution of lava flows and other deposits covering an area from Pu‘u‘Ula‘ula ("Red Hill") on the southwest to Hilo on the northeast.

Campaign GPS antenna on Kīlauea's south flank at Pu‘ukapukapu inside Hawai‘i Volcanoes National Park during the 2019 Kīlauea GPS campaign. View is to the southwest along the Kīlauea Volcano coastline. 

On March 6, 2011, USGS Hawaiian Volcano Observatory scientists were stationed along Kīlauea Volcano's East Rift Zone to monitor the progression of erupting fissures that had opened west of Pu‘u ‘Ō‘ō the day before. Lava spewing from this fissure (background) reached heights up to 30 m (100 ft) and produced a massive lava flow, visible behind the HVO scientist.

This spectacular lava fountain, erupting from Pu‘u ‘Ō‘ō on June 30, 1984, lasted just over 7 hours and reached a height of 318 m (1043 ft). It was one of 44 high lava fountains erupted during the first 3.5 years of Kīlauea Volcano's ongoing East Rift Zone eruption, which began in January 1983.

On the evening of June 30, 2008, littoral explosions at Kīlauea Volcano's Waikupanaha ocean entry created a fireworks-like display as incandescent fragments of lava flew through the air. When molten lava entered the sea, the water flashed to steam, triggering explosions that hurled spatter and other lava fragments up to heights of 50 m (164 ft).

This video clip shows Kīlauea Volcano's Kamokuna ocean entry, with the steam plume rising from the front of the lava delta. Recent flows have covered the surface of the delta with fresh lava.

USGS Hawaiian Volcano Observatory broadband-seismic stations located at the summit of Kīlauea have been significantly upgraded over the past three years. During the upgrades, HVO field engineers (inset) complete the wiring connections of the solar power and telemetry systems at each site, which are about 10 m (33 ft) from the seismometer.

Interferometric Synthetic Aperture Radar (InSAR) images of Kīlauea (left) and Mauna Loa (right) spanning the past several years. Concentric patterns of colored fringes indicate magma accumulation centered near the summit calderas of both volcanoes.