Mount Ruapehu is an active stratovolcano at the southern end of the Taupō Volcanic Zone and North Island volcanic plateau in New Zealand. It is 23 km (14 mi) northeast of Ohakune and 23 km (14 mi) southwest of the southern shore of Lake Taupō, within the Tongariro National Park. The North Island's major ski resorts and only glaciers are on its slopes.
The Taupō Volcanic Zone (TVZ) is a volcanic area in the North Island of New Zealand that has been active for at least the past two million years and is still highly active. Mount Ruapehu marks its south-western end and the zone runs north-eastward through the Taupō and Rotorua areas and offshore into the Bay of Plenty. It is part of the larger Central Volcanic Region that extends further westward through the western Bay of Plenty to the eastern side of the Coromandel Peninsula and has been active for four million years. At Taupō the rift volcanic zone is widening east–west at the rate of about 8 mm per year while at Mount Ruapehu it is only 2–4 mm per year but this increases at the north eastern end at the Bay of Plenty coast to 10–15 mm per year. It is named after Lake Taupō, the flooded caldera of the largest volcano in the zone, the Taupō Volcano and contains a large central volcanic plateau as well as other landforms associated with its containing tectonic intra-arc continental Taupō Rift.
Whakaari / White Island, also known as White Island or Whakaari, is an active andesite stratovolcano situated 48 km (30 mi) from the east coast of the North Island of New Zealand, in the Bay of Plenty. The island covers an area of approximately 325 ha, which is just the peak of a much larger submarine volcano.
In New Zealand, long distance walking or hiking for at least one overnight stay is known as tramping. There are a number of walkways in New Zealand, however most of these are relatively short and can be walked in a day or less. Many are also an easy walk, with well formed footpaths. However, some tracks require an overnight stay either because of the rugged country or the length of the track.
Mount Taranaki is a dormant stratovolcano in the Taranaki region on the west coast of New Zealand's North Island. At 2,518 metres (8,261 ft), it is the second highest mountain in the North Island, after Mount Ruapehu. It has a secondary cone, Fanthams Peak, 1,966 metres (6,450 ft), on its south side.
Whakapapa skifield is a commercial skifield on the northern side of Mount Ruapehu in Tongariro National Park, New Zealand. It is one of three skifields on the mountain, the others being Turoa, which is on Ruapehu's south-western slopes and Tukino on the eastern slopes. The ski season is generally from late June to late October, depending on snow and weather conditions. The terrain at Whakapapa Skifield is divided up as 25% beginner, 50% intermediate and 25% advanced.
Mount Ngauruhoe 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. Although often regarded as a separate mountain, geologically, it is a secondary cone of Mount Tongariro.
Tongariro National Park is the oldest national park in New Zealand, located in the central North Island. It has been acknowledged by UNESCO as a World Heritage Site of mixed cultural and natural values.
Mount Tongariro 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.
The North Island Volcanic Plateau is a volcanic plateau covering much of central North Island of New Zealand with volcanoes, lava plateaus, and crater lakes. It contains the Taupō caldera complex, Ōkataina caldera complex and Tongariro Volcanic Centre resulting in it being currently the most frequently active and productive area of silicic volcanism on Earth. New Zealand is part of the Pacific Ring of Fire.
Te Onetapu, commonly known as the Rangipo Desert, is a barren desert-like environment located in New Zealand, located in the Ruapehu District on the North Island Volcanic Plateau; to the east of the three active peaks of Mount Tongariro, Mount Ngauruhoe, and Mount Ruapehu, and to the west of the Kaimanawa Range.
The Whangaehu River is a large river in central North Island of New Zealand. Its headwaters are the crater lake of Mount Ruapehu on the central plateau, and it flows into the Tasman Sea eight kilometres southeast of Whanganui. Due to the high acidity of the water coming from the crater lake, water is not diverted from the headwaters for the Tongariro Power Scheme. Instead, it bypasses the Waihianoa Aqueduct via a ford.
The New Zealand Great Walks are a set of popular tramping tracks developed and maintained by the Department of Conservation. They are New Zealand's premier tracks, through areas of some of the best scenery in the country, ranging from coastlines with beaches to dense rain forests and alpine terrain. The tracks are maintained to a high standard, making it easier for visitors to explore some of the most scenic parts of New Zealand's backcountry.
In Māori tradition, Ngātoro-i-rangi (Ngātoro) is the name of a tohunga (priest) prominent during the settling of New Zealand (Aotearoa) by the Māori people, who came from the traditional homeland Hawaiki on the Arawa canoe. He is the ancestor of Ngāti Tūwharetoa and his travels around Lake Taupō and up onto the Volcanic Plateau are the basis of Ngāti Tūwharetoa's claim to those regions.
The Tongariro Northern Circuit, one of the New Zealand Great Walks, is a three- to four-day tramp in Tongariro National Park, New Zealand. The hike includes the Tongariro Alpine Crossing, a day's march that incorporates the Northern Circuit's most stunning scenery. The complete trail forms a 50-kilometre (31 mi) long loop trail that circumnavigates Mount Ngauruhoe. Approximately 7,000 trampers complete the walk each year. This compares to the approximately 25,000 who walk only the Tongariro Crossing section.
The volcanism of New Zealand has been responsible for many of the country's geographical features, especially in the North Island and the country's outlying islands.
The geology of New Zealand is noted for its volcanic activity, earthquakes and geothermal areas because of its position on the boundary of the Australian Plate and Pacific Plates. New Zealand is part of Zealandia, a microcontinent nearly half the size of Australia that broke away from the Gondwanan supercontinent about 83 million years ago. New Zealand's early separation from other landmasses and subsequent evolution have created a unique fossil record and modern ecology.
Hauhungatahi is an eroded volcano at the southern end of the Taupo Volcanic Zone in New Zealand, located about 11 kilometres (7 mi) WNW of Mount Ruapehu. Although relatively little-known, at 1,521 metres (4,990 ft) Hauhungatahi is one of the highest volcanoes in New Zealand, exceeded in elevation by only Ruapehu, Taranaki/Egmont, and the Tongariro massif. The volcano is constructed atop an upfaulted block of Mesozoic marine sediments. The age of the erupted andesite lava is about 900,000 years, making Hauhungatahi more than three times as old as the neighboring Ruapehu.
Whangaehu is a settlement in the Rangitikei District and Manawatū-Whanganui region of New Zealand's North Island.
Horace Arthur Holl was a New Zealand mathematician, mountaineer and rock climber. He climbed extensively in the Southern Alps, including two summits of Mount Cook within a fortnight, first via the Linda Glacier and then via Earl's Route. In the final decade of his life, he made frequent visits to Tongariro National Park and it is estimated that he ascended Mount Ruapehu about 50 times.
