Page:Picturesque New Zealand, 1913.djvu/165

Rh In this district sulphur deposits are extensive, and a short distance from the main attractions is an old sulphur mine. Years ago sulphur blocks were to be seen stacked like wood, but at last the percentage of pure sulphur has become too low to insure a profit, and the workings have been abandoned. The principal sulphur mine in Tikitere's vicinity now is the steaming crater of Ruahine. Sulphur is believed to be responsible for much of the thermal activity in New Zealand. Dr. A. S. Wohlmann, Government balneologist at Rotorua, informed me that he had little doubt that "the chemical action of sulphuric acid on water is one of the causes of heat in the acid waters."

It is refreshing, after being steamed in Whaka and Tikitere, to make a tour of the Cold Lakes. These lakes are pretty, but years ago, when forests completely surrounded them, they were more attractive still. Around neither are there high mountains, the most imposing heights being Matawhaura, an ancient cliff-spurred and wooded Maori burial-place, at the eastern end of Lake Rotoiti. On the south side of this lake is the suicide cliff of Motutawa, over which many Maoris hurled themselves long ago. A noteworthy fact about Rotoiti is its phenomenal, unaccountable rise and fall. Its fall, sometimes amounting to two feet, Maori tradition attributes to a subterranean outlet, but none has been discovered.