Where does 80m of molten rock end up?
Wherever it wants.
Apparently, if the next Auckland volcano is in the worst possible location, 500000 people might need to be evacuated. Even in a better location it will be no fun at all, with the only redeeming feature being that even Peter Thompson will have to concede that it’s not the best time to buy a house. It’s good that research and planning is underway, so the mayor’s office will have a set of contingency plans filed under “V” for when the next eruption happens, but the need for public panic awareness is perhaps less than for the Alpine Fault.
From a statistical viewpoint, there are two factors that go into how much you should do to prepare for an emergency: how likely it is, and how much the preparation will help. The earthquake wins on both of these: it’s about ten times as likely in the next 50 years, and we can do a lot more to reduce the damage. With the Alpine Fault, we need to decide how much to spend on strengthening roads, bridges, and houses, and making water and sewer systems less likely to break. Public discussion and pressure on the government are important. On the other hand, if a river of molten rock heads south from One Tree Hill, or a chunk of tuff the size of a refrigerator lands on my roof, my house isn’t going to survive no matter how good the building standards are.
In terms of things we can actually influence, we might want to worry more about which bits of Auckland will be under water in 50-100 years, not which bits will be under lava.

Recent comments on Thomas Lumley’s posts