Hualālai
Hualalai
Shield volcano · United States · 2523m

- Type
- Shield volcano
- Country
- United States
- Region
- Eastern Pacific Volcanic Regions / Hawaiian-Emperor Hotspot Volcano Group
- Elevation
- 2523m
- Coordinates
- 19.692, -155.870
- Last eruption
- 1801
- Tectonic setting
- Intraplate / Oceanic crust (< 15 km)
- Landform
- Shield
- Major rock type
- Basalt / Picro-Basalt
Geological summary
The basaltic Hualalai, at the western end of the island, is the third youngest shield volcano on Hawaii. Three rift zones, with numerous cinder cones and spatter cones, trend N, NW, and SE, and converge about 5 km E of the summit. Detailed mapping has shown that 95% of the surface area is of Holocene age, more than half is less than 3,000 years old, and a quarter is less than 1,000 years old. Eruptions at the end of the 18th century and in 1801 produced lava flows from vents on the NW rift zone that reached the sea and buried villages; the 1801 Huehue lava flow underlies part of the airport at Kona. The earlier of the two flows, the Kaupulehu lava flow, is notable for its large quantities of lava-encrusted mafic and ultramafic nodular xenoliths.
From Wikipedia
Hualālai is an active shield volcano on the island of Hawaiʻi in the Hawaiian Islands. It is the westernmost, third-youngest and the third-most active of the five volcanoes that form the island of Hawaiʻi, following Kīlauea and the much larger Mauna Loa. Its peak stands 8,271 feet (2,521 m) above sea level. Hualālai is estimated to have risen above sea level about 300,000 years ago. Despite maintaining a very low level of activity since its last eruption in 1801, and being unusually inactive for the last 2,000 years, Hualālai is still considered active, and is expected to erupt again sometime in the next 100 years. The relative unpreparedness of the residents in the area caused by the lull in activity would worsen an eruption's consequences.
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Eruption history
Detailed timeline
- 1800VEI 0Observed1800 – 1801NW rift zone (520 m)
- 1784 (±7 yrs)VEI 0Observed1784 – OngoingNW rift zone (1400-1900 m)
- 1650 (±50 yrs)VEI 1Geological estimate1650 – OngoingNW rift zone (Luamakami)
- 1240 (±150 yrs)VEI 2Geological estimate1240 – OngoingSSE rift zone (Waha Pele)
- 1150VEI 0Geological estimate1150 – OngoingNW rift zone (Puu Alauawa, Nahaha)
- 1050 (±100 yrs)VEI 1Geological estimate1050 – OngoingSSE rift zone (3 km NE of Waha Pele)
- 920 (±50 yrs)VEI 0Geological estimate920 – OngoingNW rift zone (2 km NW of Luamakami)
- 770 (±200 yrs)VEI 1Geological estimate770 – OngoingSSE rift zone (4.5 km NW of Waha Pele
- 80 BCE (±75 yrs)VEI 0Geological estimateBCE 80 – OngoingNorth rift zone (1130-1830 m)
- 350 BCE (±75 yrs)VEI 0Geological estimateBCE 350 – OngoingSE flank (1 km west of Waha Pehe)
- 400 BCE (±75 yrs)VEI 0Geological estimateBCE 400 – OngoingNW rift zone (Luamakami)
- 440 BCE (±50 yrs)VEI 0Geological estimateBCE 440 – OngoingNorth rift zone (3 km NE of Hainoa)
- 720 BCE (±75 yrs)VEI 0Geological estimateBCE 720 – OngoingNorth rift zone (700 m ENE of Hainoa)
- 1080 BCE (±200 yrs)VEI 0Geological estimateBCE 1080 – Ongoing
- 1150 BCE (±75 yrs)VEI 0Geological estimateBCE 1150 – OngoingNW rift zone (0.7 km NW of Luamakami)
- 1650 BCE (±200 yrs)VEI 0Geological estimateBCE 1650 – Ongoing
- 2040 BCE (±75 yrs)VEI 0Geological estimateBCE 2040 – OngoingNW rift zone (0.3 km NW of Hainoa)
- 2440 BCE (±75 yrs)VEI 0Geological estimateBCE 2440 – OngoingNW rift zone (1 km W of Hainoa Crater)
- 2770 BCE (±75 yrs)VEI 0Geological estimateBCE 2770 – Ongoing
- 4410 BCE (±100 yrs)VEI 0Geological estimateBCE 4410 – OngoingSE rift zone (1.6 km SE of Hainoa)
- 6820 BCE (±200 yrs)VEI 0Geological estimateBCE 6820 – OngoingCone 60 m north of Hainoa Crater
- 7540 BCE (±200 yrs)VEI 0Geological estimateBCE 7540 – Ongoing
External links
⚠ For reference only. Not for emergency response.