The natural geothermal heat flow at Wairakei during 1958 was approximately the same as during 1951–52, namely 100,000 kcal/sec relative to 12°C, despite the fact that the draw‐off from bores increased from 10,000 kcal/sec in 1951 to 160,000 kcal/sec in 1958.
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Rachel Fisher (1964) studied this question.
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