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Tholeiitic basalt, indicative of the submarine subphase of the volcano's construction, has been found in wells driven into the volcano at a depth of 75 ft (23 m).

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Haulālai is a known source for xenoliths, rock from the Earth's mantle that have been brought up in lava flows.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.i, following Kīlauea and the much larger Mauna Loa.Its peak stands 8,271 feet (2,521 m) above sea level.

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