Lake Waikare, situated within the Huntly coalfield in North Waikato, is host to a small island (Punikanae Island) where a silica sinter-depositing spring is located. This is the only sinter depositing spring known outside the Taupo Volcanic Zone. The chemical analysis from the two spring samples complimented by geological information gathered during a short field visit and other technical data available in the literature are the sets of information used in this study. Based on the Cl-SO 4 -HCO 3 ternary plot that was used to classify the geothermal waters with respect to major anion composition and the Na-K-Mg ternary plot to classify fluids according to the state of equilibrium at given temperatures, the origin of the geothermal system that feeds the spring is thought to be mature neutral chloride waters that probably originate from an up-flow zone beneath Punikanae Island with the Maungaroa Fault as its main conduit. Up-flow zones are generally characterized by silica sinter depos...
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