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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. This special place vibrates with stories of ancient and modern hawaiian culture and protects the bond between the land and its people
The park also cares for endangered species, some of which exist nowhere else East maui's long eruptive history and recent activity indicate that the volcano will erupt in the future Read about haleakala national park and how to visit.
The usgs hawaiian volcano observatory issues volcano updates for haleakalā as activity warrants.
Your complete guide to visiting haleakalā national park on maui We make an annual trip to haleakala for sunrise, sunset, hiking, and more. At 10,023 feet above sea level, this dormant volcano is the stage for a breathtaking range of landscapes—and skyscapes Haleakalā means house of the sun in hawaiian, and legend goes that the demigod maui lassoed the sun from its journey across the sky as he stood on the volcano's summit, slowing its descent to make the day last longer.
Haleakalā national park rising dramatically to a summit of 10,023 feet, haleakalā is the third largest volcano in hawaiʻi Its mass makes up approximately three quarters of maui, and its presence is dominating, playing an important role in the island's environmental, cultural, and geological makeup. The crater is not of volcanic origin, but formed as a result of the coalescence of headward erosion of the koolau and kaupo valleys Rising 10,023ft and often shrouded in clouds, this dormant volcano dominates the entire eastern horizon of maui
Capped by a crater that covers more ground than manhattan, the summit is a visual feast and the centerpiece of haleakalā national park
Ancient hawaiians worshipped near the cinder cones that dot the crater floor, and many native hawaiians today. 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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