description Lake Rotorua Overview
Lake Rotorua is a large volcanic caldera lake located in the Bay of Plenty region on New Zealand's North Island. It was formed approximately 140,000 years ago following a massive volcanic eruption, resulting in a shallow lake floor with an average depth of only 10 meters. The lake and its immediate surrounding area are renowned for ongoing geothermal activity, including sulfur vents and geysers, and serve as a significant cultural center for the Te Arawa Māori iwi.
insights Ranking position
Lake Rotorua ranks #103 of 214 in the Lake ranking, behind Lake Bosumtwi, ahead of Cayuga Lake.
help Lake Rotorua FAQ
How was Lake Rotorua formed?
Lake Rotorua is a large volcanic caldera lake located in the Bay of Plenty region on New Zealand's North Island. It was formed approximately 140,000 years ago following a massive volcanic eruption that caused the ground to collapse.
How deep is Lake Rotorua?
The lake is notably shallow, with an average depth of only 10 meters. Its shallow floor sits over an active geothermal vent, which contributes to the lake's unique mineral composition and sulfuric smell.
Why does Lake Rotorua smell like sulfur?
The high level of geothermal activity in the Rotorua region causes sulfur and other minerals to be constantly released into the water and the surrounding air. This results in the famous "rotten egg" smell that is characteristic of the area's hot springs and mud pools.
What is the mythical creature of Lake Rotorua?
In Māori legend, a monstrous, lizard-like creature called a *taniwha* named Kāhua is said to inhabit the depths of Lake Rotorua. This mythical creature is an important figure in the local indigenous folklore.
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