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Rotorua (Māori: [ˌɾɔtɔˈɾʉa] [5]) is a city in the Bay of Plenty Region of New Zealand 's North Island. It is sited on the southern shores of Lake Rotorua, from which it takes its name. It is the seat of the Rotorua Lakes District, a territorial authority encompassing Rotorua and several other nearby towns.
Lake Rotorua (Māori: Te Rotorua nui ā Kahumatamomoe) is the second largest lake in the North Island of New Zealand by surface area, and covers 79.8 km 2. [ 1 ] With a mean depth of only 10 metres it is considerably smaller than nearby Lake Tarawera in terms of volume of water. It is located within the Rotorua Caldera in the Bay of Plenty Region.
Champagne Pool is a prominent geothermal feature within the Waiotapu geothermal area in the North Island of New Zealand. The terrestrial hot spring is located about 30 km (20 mi) southeast of Rotorua and about 50 km (30 mi) northeast of Taupō. The name Champagne Pool is derived from the abundant efflux of carbon dioxide (CO 2), similar to a ...
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 ...
The Rotorua Museum Te Whare Taonga o Te Arawa is a local museum and art gallery in the Government Gardens near the centre of Rotorua, New Zealand. The museum is housed in the former Bath House building which was opened in 1908 and is noted as the first major investment in the New Zealand tourism industry by the government. [1]
Waiotapu (Māori for "sacred waters") is an active geothermal area at the southern end of the Okataina Volcanic Centre, just north of the Reporoa caldera, in New Zealand 's Taupo Volcanic Zone. It is 27 kilometres south of Rotorua. [1] Due to dramatic geothermal conditions beneath the earth, the area has many hot springs noted for their ...