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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 East maui's volume is about 30,000 km 3 (7,200 mi 3) with about 97% of the volume below sea level. The western 25% of the island is formed by another volcano, mauna kahalawai, also referred to as the west maui mountains.
The usgs hawaiian volcano observatory issues volcano updates for haleakalā as activity warrants. East maui's long eruptive history and recent activity indicate that the volcano will erupt in the future 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.
Haleakala is one of the world's largest dormant volcanoes, but it still has one eruption left in it Learn how it was formed by a hot spot and how it shaped the island of maui and the hawaiian archipelago. 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
In several places the rim of the crater rises more than 2,500 feet (760 meters) above the crater floor
Read about haleakala national park and how to visit. The summit contains a dramatic 3.5 x 9.5 km summit crater that is widely breached on the n and se sides The 'crater' is not of volcanic origin, but formed as a result of the coalescence of headward erosion of the koolau and kaupo valleys Subsequently the crater has been partially filled by a.
Southern slope of east maui, haleakalā volcano seen from the air The most recent eruptions occurred sometime between the years 1480 and 1600
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