description Inferno Crater Overview
Inferno Crater is a dynamic mudpot within Wai-o-Tapu’s geothermal area near Rotorua, New Zealand. This intensely active feature displays significant boiling activity and produces substantial volumes of hot mud due to underground volcanic heat. The crater's size and intensity make it a compelling geological observation point. It is particularly interesting for geologists, volcanologists, and visitors seeking to witness powerful geothermal processes firsthand.
insights Ranking position
Inferno Crater ranks #45 of 168 in the Mudpot ranking, behind Krafla Mudpots, ahead of Artist Paint Pots.
help Inferno Crater FAQ
Where is Inferno Crater located?
Inferno Crater is located in the Waimangu Volcanic Rift Valley on New Zealand's North Island, near the town of Rotorua. The valley was created by the catastrophic eruption of Mount Tarawera in 1886, which devastated the surrounding area.
How hot is the water in Inferno Crater?
The water temperature in Inferno Crater is reported to be well above typical hot spring temperatures, often cited near or above 80°C. The crater's temperature and water level fluctuate dramatically on a roughly periodic cycle linked to the nearby Frying Pan Lake.
What makes Inferno Crater the largest known hot spring by volume?
When its water level is at its peak during its fluctuation cycle, Inferno Crater holds an enormous volume of hot water, reportedly the largest of any hot spring of its type in the world. The spring's behavior is closely monitored by geothermal scientists because of its dramatic periodic changes.
Can visitors walk to see Inferno Crater?
Yes, Inferno Crater can be viewed via walking tracks through the Waimangu Volcanic Rift Valley, which is open to the public as a tourist attraction. The walking trail also passes other geothermal features such as Frying Pan Lake and the site of the former Waimangu Geyser.
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