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Haleakala Eruption Private Collection Updates #833

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The most recent eruption on haleakalā was probably between a.d [2] this volcanic activity has been along two rift zones The volcano is monitored by a continuous gps instrument and seismometer located near the southwest edge of the summit crater

Key sites on haleakalā are resurveyed using gps receivers every few years to detect any changes in the volcano's shape. Subsequently the crater has been partially filled by a. Haleakalā started forming 2 million years ago and built a massive shield volcano along 3 rift zones that was once broken by a central caldera

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. The table below lists all known eruptions (date in bold face) of haleakala volcano since around 2000 bc Updates on the most recent volcanic activity of haleakala can be found on the news page of haleakala volcano. Find out why it could erupt again and how to recognize its lava flows and cinder cones.

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. The last eruption occurred sometime between 1480 and 1600 according to scientific records The history of haleakalā and its recent activity indicate that the volcano will erupt again in the future

Although studies indicate that haleakalā will erupt again, the volcano is currently dormant.

Mauna loa eruptions typically start at the summit and, within minutes to months of eruption onset, can migrate into either the northeast or southwest rift zone, or radial vents on the northwest flank. 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

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