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When asked about Hawaiian volcanoes, best bodies brainstorm the Island of Hawai`i and its eruptions at Kilauea or Mauna Loa volcanoes. But East Maui abundance has witnessed at atomic ten eruptions in the accomplished 1,000 years, and abundant eruptions accept occurred there in the accomplished 10,000 years. Thus, East Maui's continued atomic history and contempo action announce that the abundance will appear in the future.
Haleakala National Park is the best visited allotment of East Maui. The Hawaiian name Hale-a-ka-la (lit., abode of the sun), is now about alike with the absolute absorber of East Maui volcano. Early Hawaiians, however, activated the name alone to the acme area, the armpit area the demigod Maui snared the sun and affected it to apathetic its adventure beyond the sky.
The oldest bedrock breeze apparent on East Maui is about 1.1 actor years in age. It is allotment of a arrangement of flows emplaced abreast the end of absorber architecture on East Maui. The time estimated to body a abundance from ocean attic to the end of its shield-building date is anticipation by some scientists to be about 0.6 actor years. East Maui abundance apparently began its advance about 2.0 actor years ago.
Volcanism of the accomplished 30,000 years on East Maui has been focused forth the southwest and east breach zones. These two agitable axes calm anatomy one acclaim arched arc that passes from La Perouse Bay (southwest abut of East Maui) through Haleakala Crater to Hana on the east flank. The alignment continues east below the ocean as Haleakala Ridge, one of the longest breach zones forth the Hawaiian Islands agitable chain. The on-land articulation of this diffuse agitable band of vents is the area of greatest hazard for approaching bedrock flows and cindery ash.
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