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Taupo Volcanic Zone facts for kids

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The Taupo Volcanic Zone (often called TVZ) is a very active area in the North Island of New Zealand. It has been active for the last two million years and still has many active volcanoes. This zone stretches from Mount Ruapehu in the southwest, goes through the Taupo and Rotorua areas, and even extends out into the Bay of Plenty sea.

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Mount Ngauruhoe
Lake taupo landsat
Satellite photo of the Lake Taupo caldera
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Volcano and lake locations in the Taupo Volcanic Zone. White Island is not shown.
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Whakaari/White Island

The Taupo Volcanic Zone is slowly getting wider, moving about 8 millimeters (about the width of a pencil) each year. It gets its name from Lake Taupo, which is a huge lake filling the crater of the biggest volcano in the zone, the Taupo Volcano.

Volcanic Activity in the TVZ

The Taupo Volcanic Zone has many volcanoes and areas with hot springs and geysers (called geothermal fields). Some of the most active volcanoes are Mount Ruapehu, Mount Ngauruhoe, and White Island. They erupt quite often.

The biggest eruption since people from Europe arrived in New Zealand was from Mount Tarawera in 1886. This powerful eruption caused many deaths and changed the landscape. Even earlier, around 1300 AD, a much larger eruption from Tarawera, called the Kaharoa eruption, would have affected the early Māori.

Past Major Eruptions

The last huge eruption from the Taupo Volcano (which now holds Lake Taupo) was the Hatepe eruption in 232 AD. It was so powerful that it's thought to have emptied the lake first! Then, a super-hot cloud of gas and ash, called a pyroclastic flow, covered a massive area of about 20,000 square kilometers (that's a huge amount of land) with volcanic ash. Scientists believe about 120 cubic kilometers of material was blasted out, and over 30 cubic kilometers of that came out in just a few minutes!

Even bigger was the Oruanui eruption from Taupo about 26,500 years ago. This eruption blasted out an estimated 1170 cubic kilometers of material. It was the most recent eruption on Earth to reach VEI-8, which is the highest level on the Volcanic Explosivity Index. This means it was incredibly powerful.

The Rotorua Caldera has been quiet for a longer time. Its main eruption happened about 240,000 years ago, though some lava has slowly oozed out in the last 25,000 years.

How Big is the Taupo Volcanic Zone?

The Taupo Volcanic Zone is about 350 kilometers (217 miles) long and 50 kilometers (31 miles) wide. It starts at Mount Ruapehu in the south and goes all the way to the underwater Whakatane volcano, which is about 85 kilometers (53 miles) past White Island in the northeast.

This zone is part of a larger area where the Earth's plates are moving. It sits behind the Kermadec-Tonga Subduction Zone, where one of Earth's huge plates is sliding under another. This movement causes the volcanic activity you see in the TVZ.

Studying the TVZ

Scientists have been studying the Taupo Volcanic Zone closely. They've found that the Earth's crust (its outer layer) under the TVZ might be as thin as 16 kilometers (10 miles). They also believe there's a huge layer of hot, melted rock (called magma) about 50 kilometers (30 miles) wide and 160 kilometers (100 miles) long, sitting just 10 kilometers (6 miles) below the surface.

The history of the volcanoes here shows that while they don't erupt often, when they do, their eruptions are very large, violent, and destructive.

Volcanoes, Lakes, and Hot Spots

The Taupo Volcanic Zone is home to several important volcanic areas, each with its own volcanoes, lakes, and geothermal fields.

Whakatane Area – Bay of Plenty

This area includes volcanoes that are partly or fully underwater, like the Submarine Whakatane volcano.

Rotorua Volcanic Center

This area is famous for its geothermal activity and beautiful lakes.

  • Rotorua Caldera: A large volcanic crater, about 22 km wide, now mostly filled by Lake Rotorua.
  • Ngongotaha (volcano)
  • Lakes:

* Lake Rotorua: A large lake with Mokoia Island in its center.

  • Geothermal fields:

* Tikitere/Hell's Gate * Whakarewarewa: Home to the famous Pohutu Geyser.

Inside the Tarawera rift
In 1886, Mount Tarawera produced New Zealand's largest historic eruption.

Okataina Volcanic Center

This center is known for its complex volcanic structures and many lakes.

  • Okataina Caldera: A large caldera, roughly 27 x 20 km.
  • Mount Tarawera: Famous for its 1886 eruption.
  • Lakes:

* Lake Okataina * Lake Tarawera * Lake Rotokakahi (Green Lake) * Lake Tikitapu (Blue Lake) * Lake Okareka * Lake Rotomahana * Lake Rotoiti * Lake Rotoma * Lake Rotoehu

  • Geothermal fields:

* Waimangu Volcanic Rift Valley: Home to Frying Pan Lake, one of the largest hot springs in the world.

Lady Knox Geyser
Lady Knox Geyser, Waiotapu geothermal area
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Craters of the Moon geothermal area

Maroa Volcanic Center

This area includes several large calderas and active geothermal sites.

  • Maroa Caldera: About 16 x 25 km.
  • Reporoa Caldera: About 10 x 15 km.
  • Whakamaru Caldera: A very large caldera, 30 x 40 km.
  • Geothermal fields:

* Waiotapu: Famous for its colorful hot springs and geysers like Lady Knox Geyser. * Wairakei: A major geothermal power station area, including Craters of the Moon. * Orakei Korako: Another beautiful geothermal park. * Ngatamariki * Ohaaki Power Station

Taupo Volcanic Center

This is the heart of the TVZ, home to New Zealand's largest lake.

* Lake Taupo: The largest lake in New Zealand.

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Composite satellite image of Mount Ruapehu
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Satellite view of the Lake Rotorua Caldera. Mount Tarawera is in the lower right corner.
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Southwest side of Mount Tarawera, Mount Edgecumbe in the background.

Tongariro Volcanic Center

This area includes some of New Zealand's most iconic volcanoes, often seen in movies!

* Mount Ngauruhoe: A cone-shaped volcano that is a main vent of Tongariro. * Tama crater lakes: Volcanic lakes within craters.

  • Mount Ruapehu: The highest mountain in the North Island and an active volcano.
  • Lakes:

* Lake Rotoaira * Lake Rotopounamu

  • Geothermal fields:

* Ketetahi Springs

Mangakino Volcanic Center

This is the westernmost and oldest volcanic caldera in the Taupo Volcanic Zone. The Waikato River flows through this area.

Other important features in the TVZ include areas where the ground has dropped down, forming valleys called grabens, such as Whakatane, Ngakuru, and Ruapehu grabens.

Images for kids

See also

Kids robot.svg In Spanish: Zona volcánica de Taupo para niños

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