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Weird Magnetic "Anomaly" Identified On New Maps Of Lake Rotorua For the First Time

The famous lake was created by volcanic activity 200,000 years ago, but it is still the site of hydrothermal activity today.

Russell is a Science Writer with IFLScience and has a PhD in the History of Science, Medicine and Technology

Dr. Russell Moul

Russell is a Science Writer with IFLScience and has a PhD in the History of Science, Medicine and Technology.

Science Writer

Edited by Holly Large
Holly Large - Editorial Assistant

Holly Large

Jr Copy Editor & Staff Writer

Holly is a graduate medical biochemist with an enthusiasm for making science interesting, fun and accessible.

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A poster showing three maps of Lake Rotorua in a column to the side of a large map. The large map shows a detailed view of the lake floor bathymetry with a bright red rim and gradual colours fading into yellow, green, and then blue as the crater becomes deeper. There is a white mass near the centre where Makoia island is.

The large map shows a detailed view of the lake floor bathymetry in Lake Rotorua at a scale of 1:17,500. Three smaller maps in the image detail free air gravity, total magnetic intensity, and conductive heat flow over the lake.

Image credit: Institute of Geological and Nuclear Sciences Limited (GNS Science)

Scientists have now fully mapped a legendary lake in New Zealand that was once an important setting for a famous Māori love story. Their analysis reveals never-before-seen details about the deep hydrothermal systems that are concealed below its disarmingly peaceful surface. 

Peaceful water and violent histories 

Lake Rotorua (Te Rotorua nui ā Kahumatamomoe in Māori) is a special place. It is the second-largest lake on New Zealand’s North Island and was formed by the violent explosions of a now dormant ancient volcano. Around 200,000 years ago, that volcano experienced a massive eruption, which caused its underlying magma chamber to collapse, creating a large 9.94 mile (16 kilometers) wide caldera. Then, around 65,000 years ago, the crater filled with water to form Lake Rotorua, which has been at its current level for the last 22,000 years.

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Despite its beauty, Lake Rotorua is still home to hydrothermal activity that reminds us of the violent volcanic processes that created it. In fact, some have described how its waters sometimes have clouds of steam drifting across them and that the lake’s heavy sulfur content gives it a “magical green-blue” appearance.

Now, researchers at GNS Science, a New Zealand-based institute, have mapped Lake Rotorua’s floor and revealed new details about its ancient base. According to their work, the lake hides thousands of “pockmarks” – essentially, smaller caters – some of which were 50 meters (164 feet) in diameter. These pockmarks mark where gas bubbles have disturbed the sediment on the lake’s floor.

The map also shows evidence of an ancient river that predates the lake. The river can be seen meandering off the shore of Sulphur Point and then winding west of Mokoia Island before curving northeast. The island, which was formed by a rhyolite dome created by slowly flowing lava, is now a lush green environment that serves as a sanctuary for many of New Zealand’s endangered wildlife and rare birds. 

It is also steeped in cultural significance for the Te Arawa people, who see it as a sacred space. Importantly, Mokoia Island is the setting for one of the most famous legends in New Zealand, the love story of Hinemoa and Tūtānekai.

Bright sun beams lake Rotorua, North Island - New Zealand
The maps reveal the hidden history behind this serene scene.
Image credit: Troy Wegman/Shutterstock.com


Magnetic anomalies

In total, the maps cover around 21 square miles (55 square kilometers) and account for about 68 percent of the lake’s floor. The mapping process was achieved through various techniques, some of which were performed by the New Zealand Navy; they used multibeam sonar to map the lake’s physical features and also conducted magnetic surveys of the lake floor. This latter technique revealed interesting magnetic anomalies towards the center of the lake.

Under normal conditions, volcanic rocks contain magnetite, a mineral (not to be mistaken for the similarly named Pokémon) that is highly magnetic and aligns itself to Earth’s magnetic field. However, in places like Lake Rotorua, hot water can pass through the rock and transform magnetite into pyrite (fool’s gold), which has pretty much no magnetic signal.

“Normally with volcanic rocks, when you run a magnetometer over the top of them, you get very positive anomalies, but in this case we're getting negative anomalies, likely due to very low magnetic susceptibilities,” Dr Cornel de Ronde, a principal scientist at GNS, told Live Science.

This anomaly seems to coincide with a “subtle heat flow anomaly”, researchers explained in a statement, which hints at a "possible igneous intrusion and another hydrothermal system nearby—exciting clues as to the hydrothermal processes at play beneath the lake floor.”

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This could explain why there is a negative anomaly in that part of the lake.

“We are excited not only for how these new maps broaden our collective knowledge of region,” said the researchers, “but also celebrate the iconic landscape and will contribute to further study in the future.”


ARTICLE POSTED IN

natureNaturenatureplanet earth
  • tag
  • eruption,

  • volcanic activity,

  • New Zealand,

  • mapping,

  • planet earth,

  • hydrothermal,

  • Lake Rotorua

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