There have been quite large hydrothermal eruptions from areas adjacent to the base of the mountain and whose erupted material overlay the Hatepe eruption pumice resulting in estimated eruption ages of about 1300 CE. Warm ground extends up to some of the southern ridges of the volcano. The hot water spring geothermal activity is confined to the downthrown side of the Ngapouri-Rotomahana Fault but steam geothermal activity is on both sides of the fault reflecting the highest heat output for the Waiotapugeothermal area. This fault is a splay of the Paeroa Fault at the eastern margin of the Taupō Rift of the Taupō Volcanic Zone and indeed the Paeroa range extends south-south-west of Maungaongaonga along this fault line that is displacing at a rate of 7.2 ± 0.4 mm/yr.
Biology
The lower part of the Maungaongaonga Scenic Reserve along the Waikite valley is dangerous to access due to its geothermal features. However the difficulty in access means it is classified as high quality geothermal habitat with four at risk species being geothermal kānuka, the ferns Dicranopteris linearis and Nephrolepis flexuosa, and Korthalsella salicornioides.