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Although the two larger volcanos have each erupted over 150 times in the last 1,000 years, Hualālai has done so but 3 times.

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Cone collapsed causing violent phreatic eruptions of tuff.

Lava flow eruption resumed building larger cone, with eruption of long ʻAʻā lava flows. On its way down, it overran a village and a valuable 3 mi (5 km) fishing pond.

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, Hualālai is still considered active, and is expected to erupt again some time within the next century.

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Here’s how to make that volunteer time really mean something to your child. The eruptions, although partially covered by flows from Hualālai and Mauna Loa, have built a distinctive structure known as the Pu (390 sq mi), the slump consists of an intricate formation of beaches and scarps 2,000 to 4,500 m (6,600 to 14,800 ft) below the waterline.This area was explored more closely in a 2001 joint Japan-United States project to explore the volcano's flanks, utilizing the Remotely operated vehicle ROV Kaikō.Data collected showed that the lava flows there originated in shallow water 500 to 1,000 m (1,600 to 3,300 ft) deep, and that unlike similar slumps at other volcanoes, the slump at Hualālai formed gradually.Haulālai is a known source for xenoliths, rock from the Earth's mantle that have been brought up in lava flows.Although it has been relatively placid in the recent past, Hualālai is still potentially active, and is expected to erupt again within the next 100 years.

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