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Level 4, 66 Wyndham Street
Auckland, New Zealand
The Northwest Territories’ Smoking Hills show a natural phenomenon which has probably been active for thousands of years. The hills close to the Beaufort Sea were seen by John Franklin in 1826 during his second Canadian expedition looking for indications of a Northwest Passage. Franklin observed that the rocks and soil around Cape Bathurst seemed to be on fire and produced acrid white smoke. They were therefor named “Smoking Hills”. The reason behind this phenomenon is neither human-induced burning nor volcanic activity, but the subsurface exothermic reaction between the bituminous shale, the sulfur and the iron pyrite of the area. The heat being released through the oxidation of pyrites in the Cretaceous mudstones along the sea cliffs leads not only to high ground temperatures, but also to hot sulfurous gas being driven off and the possibility of spontaneous combustion. The fumes that are seen contain sulfur dioxide and sulfuric acid and are noxious.