Silica residue is the main product of the alteration of a rhyolitic, tuff-rich, volcanic substrate by acid sulfate condensate formed, in a major steam field at Tikitere, near Rotorua. Here steam and accompanying H2S discharge in an area characterized by large standing pools of acid water and mud pots. As in silica sinters, that precipitate from hot, near-neutral, alkali chloride waters, the fir...