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[ˈhɐlɛˈjɐkəˈlaː]), or the east maui volcano, is a massive, active shield volcano that forms more than 75% of the hawaiian island of maui. Haleakala, as mentioned before, is a shield volcano (on the pacific plate). Haleakalā is a shield volcano that forms where a hotspot meets the pacific plate

Learn about its features, history, types of lava, and potential for future eruptions. The formation of volcanoes as magma rises through the plate, is what created the chain of hawaiian islands Haleakalā, is one of two volcanoes that make up the island of maui

It is in the postshield alkalic stage of hawaiian volcanism.

It is a central feature of haleakala national park Haleakala has one of the world’s largest dormant volcanic craters, which was formed mainly by erosion and measures about 20 miles (30 km) in circumference. The broad haleakalā shield volcano towers over the eastern part of the island of maui, seen here from the beach at kihei on the west flank Its summit profile is irregular because of the many scoria cones that have erupted along the sw rift zone, which extends from the coast to the summit.

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