Images

The July 19–22, 1974, Keanakākoʻi eruption was a dramatic summit event triggered by a sudden increase in seismicity and summit deflation. Lava fountains up to 180 feet high erupted from fissures north and south of Keanakākoʻi Crater and on the caldera floor, sending lava flows about 1.5 miles southward and across the caldera floor.

The May 1973 eruption near Hiʻiaka Crater was a vigorous event on Kīlauea’s upper East Rift Zone. Lasting about seven hours, it produced lava flows that traveled from just west of Hiʻiaka to Pauahi Crater, crossing what is now Chain of Craters Road in Hawaiʻi Volcanoes National Park.

As erupting fissures migrated down Kīlauea's southwest rift zone in September 1971 for the first time in 52 years, many spectators hiked into the Ka‘ū Desert for a closer view of the rare event. Hawai‘i Volcanoes National Park rangers patrolled the area on horseback to keep people a safe distance from the lava fountains. Photo courtesy of NPS.

Seaward sliding of Kīlauea's south flank over many thousands of years has resulted in large ground displacements along shallow faults that break the surface, as shown by the cliffs ("pali" in Hawaiian) seen here. Most of the movement along the faults occur during sudden slip that cause large earthquakes.

 HVO scientist measures the episode 12 lava fountain height at Mauna Ulu from Puʻu Huluhulu on Dec 30, 1969. The Mauna Ulu eruption marks its 51^st anniversary on May 24, 1969.

This lava fountain, which erupted on September 6, 1969, during the Mauna Ulu eruption, was about 540 m (1770 ft) tall. The tephra cone, eventually named Mauna Ulu, can be seen in the fallout area (right of the fountains. in middle of image). It is now a 121 m (397 ft) tall lava shield in Hawai‘i Volcanoes National Park.

The February 1969 rift eruption near Nāpau Crater was a brief but dynamic precursor to the long-lived Maunaulu eruption that began in May of that year. This week-long event featured lava fountaining from multiple fissures along a 2.5-mile stretch of Kīlauea’s upper East Rift Zone.

An aerial photo of a segment of the 1968 eruptive fissures in the middle East Rift Zone of Kīlauea. A line of lava fountains is feeding a small lava channel on October 8, 1968, during the second day of this eruption. USGS photo taken by D. Swanson.

A telephoto image of vents erupting on the floor of Halema‘uma‘u crater, at the summit of Kīlauea, in 1967. NPS photo by C. Stoughton.

An aerial overview of Halema‘uma‘u crater erupting in early December 1967. USGS image.

Earthquake report card from 1967 containing detailed information of personally observed effects from a M3.9 earthquake at the summit of Kīlauea. HVO staff distributed the report cards to local citizens between 1930 and 1989.

A fissure on the northwestern crater wall of Makaopuhi Crater on the East Rift Zone of Kīlauea sent lava cascading into the deepest portion of the crater, forming a lava lake. USGS photo taken by E. Endo on March 6, 1965, from a viewing area along the old Chain of Craters Road.     

The 1961 fissure eruption near Nāpau Crater was a short-lived but notable event on Kīlauea’s East Rift Zone, occurring in late September. Over two days, lava erupted from vents along a 13-mile stretch, producing 13 small flows and lava fountains that reached heights of up to 400 feet, with the largest flows occurring near Pāhoa.

The July 1961 eruption at Halemaʻumaʻu was the third summit eruption of that year, continuing the pattern of vigorous volcanic activity at Kīlauea. This event featured sustained lava fountaining and further infilling of the crater, building upon the changes initiated by the February and March eruptions.

The March 1961 eruption at Halemaʻumaʻu was the second of three summit eruptions at Kīlauea that year, marked by renewed lava activity within the northeast collapse pit formed in February. This phase featured vigorous lava fountaining, crater floor uplift, and the gradual infilling of the pit, reflecting continued magma supply and dynamic summit processes.

The February 1961 summit eruption of Kīlauea marked the beginning of a year of intense volcanic activity, characterized by three distinct summit eruptive phases.

View westward along the Kapoho fault scarp in the village of Kapoho following a swarm of earthquakes in the area. The ground cracking was caused by subsidence of a graben (down-dropped block) that spanned the community.

Great quantities of lava pour from the base of a 480-m-tall (1,575 ft) fountain about 65 minutes after the start of episode 16. Lava discharge at this time was about 1.3 million cubic meters per hour (1.7 million cubic yards), which sent lava over the entire lake by 4:05 a.m.

Hawaiian Volcano Observatory Scientists at the rim of Kīlauea volcano measuring variations in magnetic field strength in 1950. Photo by Ray E. Wilcox.

Fissure of lava fountains erupting from Mauna Loa's upper southwest rift zone, June 2, 1950. Plumes of volcanic gas rise high into the air. Aerial photograph taken by the Air National Guard.

The Ka‘apuna flow traveled from the Southwest Rift Zone vent (7,800 ft elevation) to the coast in just 17 hours.