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Island of Lana‘i Formed of a single shield volcano, Palawa caldera on the Maui Nui The Lana‘i volcano reached the subaerial sheild stage, has a single volcanic rock member Lana‘i Member , tholeiitic basalt, 1.46 to 0.78 Ma pahoehoe and a‘ā, and and spatter cones on the rift zones
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Island of Lana‘i • Formed of a single shield volcano, Palawa caldera on the Maui Nui • The Lana‘i volcano reached the subaerial sheild stage, has a single volcanic rock member • Lana‘i Member, tholeiitic basalt, 1.46 to 0.78 Ma • pahoehoe and a‘ā, and and spatter cones on the rift zones • caldera partly filled by lava, but is still visible • three rift zones • grabens along rift zones • This volcano also has has marine deposits, evidence for higher stands of the sea
Pacific Ocean Lanai Volcano Palawa caldera Rift zones
Reef coral and basalt boulders deposits resting ~conformably on basalt flows, ~100 m above sea level, south coast of Lana‘i -
Lanai slumped into sea on southwest: sea cliff exposing faults
Island of Kaho‘olawe • Formed of a single shield volcano • Shield Stage, Lower Member (age unknown) • caldera is present but filled in, ~5 km diameter • typical shield lavas, tholeiitic basalt • later shield-stage lavas have high silica (similar to Ko‘olau) • source rock for adzes found all over Hawai‘i • Postshield Stage, Upper Member, ~1.0 Ma • small extent, include top part of caldera filling lavas • hawaiite • Rejuvenation Stage Vents? • Youngest vents cut alluvium, but are tholeiitic (!); found at top of sea cliff • Water problems--shallow wells yield brackish water • in rain shadow of Maui; also a low island • little vegetation--overgrazed (had been used as a ranch) • soil erosion by wind • Eastern part of volcano is missing--landslide? • No debris, but eruptions from SW rift of East Maui may bury deposits
Kaholawee Volcano Caldera and rift zones Pacific Ocean