Вайотапу является активным геотермальным районом в вулканической зоне Таво. Вулканическая зона Вайотапу в Новой Зеландии располагает геотермальным ландшафтом с живыми залежами оранжевых и коричневых минералов. Выдающееся белое минеральное образование выделяется на фоне текстурированной поверхности пузырьков, окруженной восходящим паром, что свидетельствует о высокой геотермальной активности. Этот район является частью вулканического центра Окатаина, расположенного к северу от кальдеры Репороа, и известен своими уникальными геотермальными свойствами и красочными геотермальными бассейнами.

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