10. Frying Pan Lake
Frying Pan Lake is the largest hot spring in the world. It is located in Waimangu Volcanic Rift Valley, New Zealand. Waimangu Volcanic Rift Valley is the hydrothermal system created on 10 June 1886 by the volcanic eruption of Mount Tarawera, on the North Island of New Zealand. It encompasses Lake Rotomahana, the former site of the Pink and White Terraces. It was the location of the Waimangu Geyser, which was active from 1901 to 1904.
The Moeraki Boulders are unusually large and spherical boulders lying along a stretch of Koekohe Beach on the wave cut Otago coast of New Zealand between Moeraki and Hampden. They occur scattered either as isolated or clusters of boulders within a stretch of beach where they have been protected in a scientific reserve. The erosion by wave action of mudstone, comprising local bedrock and landslides, frequently exposes embedded isolated boulders.
8. Nugget Point
Nugget Point is one of the most iconic landforms on the Otago coast. Located at the northern end of the Catlins coast down the road from Kaka Point, this steep headland has a lighthouse at its tip, surrounded by rocky islets (The Nuggets). The point is home to many seabirds, including penguins, gannets and spoonbills, and a large breeding colony of fur seals.
Mount Tarawera is the volcano responsible for one of New Zealand's largest historic eruptions. Located 24 km southeast of Rotorua in the North Island, it consists of a series of rhyolitic lava domes that were fissured down the middle by an explosive basaltic eruption in 1886. These fissures run for about 17 km northeast-southwest. The volcano's component domes include Ruawahia Dome (the highest at 1111 m), Tarawera Dome and Wahanga Dome.
Mount Ngauruhoe is an active stratovolcano or composite cone in New Zealand, made from layers of lava and tephra. It is the youngest vent in the Tongariro volcanic complex on the Central Plateau of the North Island, and first erupted about 2,500 years ago. Although seen by most as a volcano in its own right, it is technically a secondary cone of Mount Tongariro.
Mitre Peak is an iconic mountain in the South Island of New Zealand. It is one of the most photographed peaks in the country. The distinctive shape of the peak in southern New Zealand gives the mountain its name, after the mitre headwear of Christian bishops. It was named by a survey crew from the HMS Acheron.
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 southeast of Rotorua and about 50 km northeast of Taupo. The name Champagne Pool is derived from the abundant efflux of carbon dioxide (CO2), similar to a glass of bubbling champagne.
2. Lake Rotoehu
Lake Rotoehu is the smallest in a chain of three lakes to the northeast of Lake Rotorua in North Island, New Zealand. It is located between the city of Rotorua and town of Whakatane. The southern end of the lake occupies part of the Okataina caldera. It is fed (underground seepage) by Lake Rotoma to the east, and flows westward joining Lake Rotoiti.
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The cliff was formed during the ice age, about approximately 10,000 years ago, when the edges of the glacier reached the cliff.
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