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The coast west of Hualālai in particular had several royal complexes.The volcano is also important ecologically, is home to many rare species and several nature reserves near the summit, and is a popular hiking attraction.There are over 100 cinder and spatter cones arranged along these rift zones.Hualālai has no summit caldera, although there is a collapse crater about 0.3 mi (0.48 km) across atop a small lava shield.

The recurrence of activity at the volcano seems to be every 200 to 300 years.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.Hualālai is a known source for xenoliths, rock from the Earth's mantle that have been brought up in lava flows.

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