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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 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 western 25% of the island is formed by another volcano, mauna kahalawai, also referred to as the west maui mountains.
Southern slope of east maui, haleakalā volcano seen from the air It is a central feature of haleakala national park The most recent eruptions occurred sometime between the years 1480 and 1600
East maui's long eruptive history and recent activity indicate that the volcano will erupt in the future
East maui's volume is about 30,000 km 3 (7,200 mi 3) with about 97% of the volume below sea level. The largest dormant volcano in the world, haleakalā, makes up a large part of maui Mount haleakalā is also called the east maui volcano Haleakalā is considered a dormant volcano because it has not erupted in a long time, but it could erupt again in the future
Haleakalā is a huge shield volcano. Haleakalā is a shield volcano that is not extinct and could erupt again Learn about its formation, features, types of lava, and history of eruptions from this web page. Read about haleakala national park and how to visit.
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