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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. Unlike other national parks, haleakala's eruptions are less intense and shapes the features of a classic hawaiian volcano. Haleakalā is a shield volcano that forms where a hotspot meets the pacific plate

Haleakala Crater | Haleakala National Park - Maui's volcano

Learn about its features, history, types of lava, and potential for future eruptions. Haleakala is located above a hotspot, an area where molten rock from deep within the earth rises toward the surface, which creates active volcanism East maui volcano, known more widely as haleakalā, is one of two volcanoes that make up the island of maui

East maui began its growth about 2 million years ago, but its early history of volcanism is buried beneath innumerable lava flows thousands of.

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 massive haleakala shield volcano forms the eastern portion of the island of maui The summit is at the nw end of a volcanic ridge and at the head of a large scarp that opens to the ene, interrupting the ridge which continues 7 km across the valley, formed as a result of the coalescence of headward erosion of the koolau and kaupo valleys

Subsequently the valley has been partially filled by.