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Lake Taupō (also spelled Taupo; Māori: Taupō-nui-a-Tia or Taupōmoana) is a large crater lake in New Zealand's North Island, located in the caldera of Taupō Volcano. The lake is the namesake of the town of Taupō , which sits on a bay in the lake's northeastern shore.
Largest lake in New Zealand; second-largest freshwater lake in Oceania: 2: Lake Te Anau: 344 km 2 (133 sq mi) Southland: Largest lake in the South Island: 3: Lake Wakatipu: 291 km 2 (112 sq mi) Otago: Longest lake in New Zealand (80 kilometres (50 mi)) 4: Lake Wānaka: 192 km 2 (74 sq mi) Otago: 5: Lake Ellesmere / Te Waihora: 180 km 2 (69 sq ...
The eruption further expanded the lake, which had formed after the much larger Oruanui eruption. Its new deposits also briefly created another large lake to the Taupō Volcano's north that extended to the Reporoa Caldera which in due course broke out into the Waikato River valley and released over a short period 2.5 km 3 (0.60 cu mi) of water.
Therefore, mean depth figures are not available for many deep lakes in remote locations. [9] The average lake on Earth has the mean depth 41.8 meters (137.14 feet) [9] The Caspian Sea ranks much further down the list on mean depth, as it has a large continental shelf (significantly larger than the oceanic basin that contains its greatest depths).
Huka Falls is a set of waterfalls on the Waikato River, which drains Lake Taupō in New Zealand.. A few hundred metres upstream from Huka Falls, the Waikato River narrows from approximately 100 metres across to a canyon only 15 metres across.
The ancestral Waikato River flowed from an ancient lake (Lake Huka) in the centre of the North Island through deep gorges of welded ignimbrite and rhyolite, northward through the Hinuera Valley and Hauraki Basin into the Thames Estuary. It is possible that the river flowed through the Waikato Basin about a million years ago before returning to ...
Lake Erie is the shallowest of the Great Lakes but bests its cousins in several other ways. Find out more about all the Great Lakes.
The reefs are at a high heat-output geothermal hot spot area within the Taupō Volcano. [3] This is related to rhyolitic lava domes extruded after explosive volcanism. [4] The explosive eruptions include the VEI 7 Hatepe eruption of 232 ± 10 CE that ejected over 120 km 3 (29 cu mi) of material (also known as Horomatangi Reef Unit Y eruption) [5] and its linear line of eruption centres, [6] as ...