Lake Pupuke
Pupuke-moana
The Auckland Volcanic Field is comprised of monogenetic volcanoes which means it is unlikely that Pupuke or any of the existing volcanoes will erupt again. The next eruption will probably occur in a new location.
Formation
On the western flanks of the volcano, a small scoria mound was formed from minor fire-fountaining of frothy lava. After the volcanic activity ended, the crater filled with fresh water to form Lake Pupuke.
Along the coast, many tree moulds (stumps and logs) are exposed in the lava. This ancient fossil forest can be seen at the northern end of Takapuna beach.
Other examples of explosion craters in Auckland are Panmure Basin and Orakei Basin. Find out more about the difference between the way explosion craters and scoria cones formed.
Use and value
Key facts
Maori name: Pupuke, shortened form of Pupukemoana, 'over flowing lake'.
Location: North Shore City, map reference NZMS 260: R11/680896
Depth: 64m
Age: Formed 140,000-150,000 years ago
Volume lava: approximately 26 million cubic metres (equivalent to 5,200 Olympic sized swimming pools)
Volume tuff/ash/pyroclastics: approximately 34 million cubic metres (equivalent to 6,800 Olympic sized swimming pools)





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