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This special place vibrates with stories of ancient and modern hawaiian culture and protects the bond between the land and its people The shape of haleakalā means that only the very top — only about 5% — is above sea level. The park also cares for endangered species, some of which exist nowhere else
[ˈhɐlɛˈjɐkəˈlaː]), or the east maui volcano, is a massive, active shield volcano that forms more than 75% of the hawaiian island of maui About 12% of the volcanoes on earth are shield volcanoes The western 25% of the island is formed by another volcano, mauna kahalawai, also referred to as the west maui mountains.
Read about haleakala national park and how to visit.
Southern slope of east maui, haleakalā volcano seen from the air 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.
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 One of maui's most popular attractions is haleakala national park
Learn more about outdoor adventures and experiences on the mountain and plan your perfect vacation to the hawaiian islands.
Explore maui's haleakala national park for the day, sunrise or sunset Go camping, explore the hiking trails too Learn about life zones and more on tour. Often referred to as the backside of haleakalā, the kīpahulu district shows off a different side of the volcano, where its lava flows have met the sea, creating waterfalls and other lush environments, such as the pools at ʻoheʻo
If you like the road less traveled, exploring the 'backside' of haleakala is an adventure worth taking. 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.
Shield volcano all hawaiian volcanoes are called shield volcanoes because the gradual buildup of many thin layers of lava erupting from the hot spot creates a shape like a warrior's shield —long, broad, and gently curved
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