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Rotorua Caldera information


Rotorua Caldera
NASA image of the caldera. The town of Rotorua is south of the lake that fills much of the apparently circular caldera. The caldera is a more complex shape with areas of collapse and the Tikitere Graben at its outlet. Mount Tarawera is in the lower right corner south east of the caldera and it and the lakes to the east are features of the adjacent active Ōkataina Caldera. The eruption products are thickest towards the north east.
Highest point
Elevation757 m (2,484 ft)
Coordinates38°05′S 176°16′E / 38.08°S 176.27°E / -38.08; 176.27
Dimensions
Width22 kilometres (14 mi)[1]
Geography
Rotorua Caldera is located in New Zealand
Rotorua Caldera
Rotorua Caldera
North Island
Rotorua Caldera is located in North Island
Rotorua Caldera
Rotorua Caldera
Rotorua Caldera (North Island)
CountryNew Zealand
RegionBay of Plenty
Geology
Age of rockPleistocene (0.24 Ma)[2]
PreꞒ
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Pg
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Mountain typeCaldera
Volcanic arc/beltTaupō Volcanic Zone
Last eruption< 25,000 years ago[3]

The Rotorua Caldera is a large rhyolitic caldera that is filled by Lake Rotorua. It was formed by an eruption 240,000 years ago that produced extensive pyroclastic deposits. Smaller eruptions have occurred in the caldera since, the most recent less than 25,000 years ago. It is one of several large volcanoes in the Taupō Volcanic Zone on the North Island of New Zealand.

  1. ^ Milner, David M (2001). The structure and eruptive history of Rotorua Caldera, Taupo Volcanic Zone, New Zealand (Thesis).
  2. ^ Bégué, F.; Deering, C. D.; Gravley, D. M.; Kennedy, B. M.; Chambefort, I.; Gualda, G. A. R.; Bachmann, O. (2014). "Extraction, Storage and Eruption of Multiple Isolated Magma Batches in the Paired Mamaku and Ohakuri Eruption, Taupo Volcanic Zone, New Zealand". Journal of Petrology. 55 (8): 1653–1684. doi:10.1093/petrology/egu038. hdl:20.500.11850/88102.
  3. ^ "Rotorua". Global Volcanism Program. Smithsonian Institution.

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Rotorua Caldera

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The Rotorua Caldera is a large rhyolitic caldera that is filled by Lake Rotorua. It was formed by an eruption 240,000 years ago that produced extensive...

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the Rotorua Caldera, in which the town lies. The name Rotorua comes from the Māori language, where the full name for the city and lake is Te Rotorua-nui-a-Kahumatamomoe...

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of volume of water. It is located within the Rotorua Caldera in the Bay of Plenty Region. Lake Rotorua is fed with water from a number of rivers and...

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years ago that included the formation of Lake Rotorua and eruption of the Mamaku ignimbrite. The Ohakuri Caldera lies mainly to the east and north of the Ātiamuri...

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rising to 180 metres above the lake surface. It was formed after the Rotorua caldera collapsed and rhyolitic magma was pushed through the cracks. One of...

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Kapenga Caldera. The Paeroa Garben's eastern edge is defined by the Paeroa Fault. The cliffs are composed of Mamaku ignimbrite from the Rotorua Caldera eruption...

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Waikato River at Ātiamuri. At Ātiamuri the Ohakuri Caldera which had a paired eruption with the Rotorua Caldera is to its immediate north. The eastern boundary...

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rhyolite. The Omanawa Caldera is inferred by an area of gravity and magnetic anomaly that exists to the north-west of the Rotorua Caldera, and this postulated...

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Whakamaru Caldera

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The Whakamaru Caldera was created in a massive supereruption 335,000 years ago and is approximately 30 by 40 km (19 by 25 mi) in size and is located in...

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Omanawa Caldera

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Omanawa Caldera is inferred by an area of magnetic anomaly that exists to the north-west of the Rotorua Caldera. It is also located to the north west...

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Tikitere Graben

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079 in/year) and has destroyed the Rotorua Caldera rim at this point, so providing the current natural outlet for Lake Rotorua. The graben is a tectonic intra-rift...

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Lake Tikitapu

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known as Blue Lake, is the smallest of four small lakes lying between Lake Rotorua and Lake Tarawera in the Bay of Plenty Region of New Zealand's North Island...

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Mount Tarawera

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within the older but volcanically productive Ōkataina Caldera. Located 24 kilometres southeast of Rotorua, it consists of a series of rhyolitic lava domes...

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forgotten survey from 1859. Many lakes around Rotorua are calderas from rhyolitic eruptions. For example, Lake Rotorua erupted around 13,500 years ago. A line...

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the Taupō Volcanic Zone: Rotorua, Ōkataina, Maroa, Taupō, Tongariro and Mangakino. It includes Mangakino volcano, Reporoa Caldera, Mount Tarawera, Mount...

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explosive activity or a collapse during a volcanic eruption. Lakes in calderas fill large craters formed by the collapse of a volcano during an eruption...

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lies within the Ōkataina Caldera. It is the most recently formed larger natural lake in New Zealand, and the deepest in the Rotorua district. The New Zealand...

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three lakes to the northeast of Lake Rotorua in New Zealand's North Island. It is located between the city of Rotorua and town of Whakatāne. The southern...

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