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The volcano erupted on 9 December 2019 at 2:11 pm local time (01:11 UTC). [3] The ash plume rose 3.7 kilometres (12,000 ft) into the air. [26]It was initially believed that there were about 100 tourists on or near the island when the eruption took place; later, this figure was revised to 47 people who were on the island at the time. [27]
The island is New Zealand's most active cone volcano, and has been built up by continuous volcanic activity over the past 150,000 years. [4] The nearest mainland towns are Whakatāne and Tauranga . The island has been in a nearly continuous stage of releasing volcanic gas at least since it was sighted by James Cook in 1769.
The Kermadec Islands are an active volcanic island arc stretching north-northeast from New Zealand's North Island towards Tonga. While only a few volcanoes in the arc are tall enough to form islands, it includes about 30 sizeable submarine volcanoes with many in the South Kermadec Ridge Seamounts at the New Zealand end of the chain.
Whakaari is New Zealand's most active cone volcano, and has been built up by continuous volcanic activity over the past 150,000 years. [3] The nearest mainland towns are Whakatāne and Tauranga. The island has been in a nearly continuous stage of releasing volcanic gas at least since it was sighted by James Cook in 1769.
The following table lists the largest islands of New Zealand proper by area. [Note 2] River delta islands such as Rakaia Island (25.7 km 2 (9.9 sq mi)), [8] Fereday Island, Rangitata Island, and Inch Clutha (approximately 15 km 2 (5.8 sq mi), 30 square kilometres (12 square miles), and 35 km 2 (14 sq mi) respectively) are omitted, as are temporary islands in braided river channels and tidal ...
Motukorea or Browns Island is a small New Zealand island, in the Hauraki Gulf north of Musick Point, one of the best preserved volcanoes in the Auckland volcanic field.The age of eruption is about 25,000 years ago, when the Tāmaki Estuary and the Waitemata Harbour were forested river valleys. [1]
Puketutu Island, also known as Te Motu a Hiaroa, is a volcanic island in the Manukau Harbour, New Zealand, and is part of the Auckland volcanic field. European settlers called it Weekes' Island, but this was eventually abandoned in favour of the historical Māori name. The island is joined to the mainland via a causeway known as Te Ara Tāhuna.
Much of the volcanic activity in the northern portions of the North Island of New Zealand is recent in geological terms and has taken place over the last 30 million years. . This is primarily due to the North Island's position on the boundary between the Indo-Australian and Pacific plates, a part of the Pacific Ring of Fire, and particularly the subduction of the Pacific plate under the Indo ...
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