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New Zealand's most fragile and threatened geological process systems are our geothermal fields and their surface features. The activity of Pohutu Geyser at Whakarewarewa had been waning for many years before picking up significantly since the government-imposed bore closures. Photo: Lloyd Homer

This article text was automatically generated and may include errors. View the full page to see article in its original form.I whakaputaina aunoatia ēnei kuputuhi tuhinga, e kitea ai pea ētahi hapa i roto. Tirohia te whārangi katoa kia kitea te āhuatanga taketake o te tuhinga.
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Hononga pūmau ki tēnei tūemi

https://paperspast.natlib.govt.nz/periodicals/FORBI19890801.2.27.1

Bibliographic details
Ngā taipitopito pukapuka

Forest and Bird, Volume 20, Issue 3, 1 August 1989, Page 28

Word count
Tapeke kupu
42

New Zealand's most fragile and threatened geological process systems are our geothermal fields and their surface features. The activity of Pohutu Geyser at Whakarewarewa had been waning for many years before picking up significantly since the government-imposed bore closures. Photo: Lloyd Homer Forest and Bird, Volume 20, Issue 3, 1 August 1989, Page 28

New Zealand's most fragile and threatened geological process systems are our geothermal fields and their surface features. The activity of Pohutu Geyser at Whakarewarewa had been waning for many years before picking up significantly since the government-imposed bore closures. Photo: Lloyd Homer Forest and Bird, Volume 20, Issue 3, 1 August 1989, Page 28

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