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The plateau is approximately 60 km (37 mi) east–west and the north–south distance is about 125 km (78 mi). [1]Extensive ignimbrite sheets spread east and west from the Central Taupō Volcanic Zone, centred on the huge active supervolcanic caldera of Lake Taupō, now the largest lake in New Zealand.
The large ignimbrite sheets of the North Island Volcanic Plateau extend, under later sedimentary and volcanic deposits, from Hawkes Bay all the way to Auckland. This is as the Kidnappers eruption of a million years ago (1 Ma) produced 1,200 km 3 (287.9 cu mi) of ignimbrite deposits, the most widespread on Earth, being over 45,000 km 2 (17,000 ...
Mount Tongariro (/ ˈ t ɒ ŋ ɡ ə r ɪr oʊ /; Māori: [tɔŋaɾiɾɔ]) is a compound volcano in the Taupō Volcanic Zone of the North Island of New Zealand. It is located 20 km (12 mi) to the southwest of Lake Taupō, and is the northernmost of the three active volcanoes that dominate the landscape of the central North Island.
Satellite image of the Big Raven Plateau in British Columbia, Canada Rangipo Desert of the North Island Volcanic Plateau. Numerous tephra layers are visible. The Pajarito Plateau in New Mexico, United States is an example of a volcanic plateau. A volcanic plateau is a plateau produced by volcanic activity. There are two main types: lava ...
Pihanga is a 1,326 metres (4,350 ft) [2] andesitic volcanic peak in the North Island Volcanic Plateau, located to the north of Mount Tongariro, between Tongariro and Lake Taupō. The nearest town to Pihanga is Tūrangi .
In turn it uses data from the source pages that it is used in as a map overlay. These source pages are above. It is a map of approximate selected surface volcanic features in Northern North Island of New Zealand within the last 25 million years odd of formation when the Alpine Fault tectonics of Zealandia that started when most of this ...
The North Island Volcanic Plateau occupies the center of the island. Lake Taupō , New Zealand's largest lake, sits in a volcanic caldera formed during a violent eruption 2000 years ago. The volcanic peaks of Mount Tongariro (1,978 m), Mount Ngauruhoe (2,291 m), and Mount Ruapehu (2,797 m) lie south of Lake Taupō.
Mount Ngauruhoe (Māori: Ngāuruhoe) is a volcanic cone in New Zealand. It is the youngest vent in the Tongariro stratovolcano complex on the Central Plateau of the North Island and first erupted about 2,500 years ago. [3] Although often regarded as a separate mountain, geologically, it is a secondary cone of Mount Tongariro.