Longevity of a small shield volcano revealed by crypto-tephra studies (Rangitoto volcano, New Zealand): Change in eruptive behavior of a basaltic field

•Crypto-tephra reveals a previously unrecognized record of volcanism.•Rangitoto volcano considered ‘monogenetic’ but erupted for ~ 1000 years•Dramatic change in eruption style, volume and frequency in Auckland region•Hazard modeling needs to be revisited.

The life-span of small volcanoes in terrestrial basaltic fields, commonly considered ‘monogenetic’, can be difficult to assess due to a paucity of datable materials capable of providing a 102–103-year age resolution. We have used microscopic tephra layers (crypto-tephra) in lake sediments to determine the longevity of Rangitoto volcano, a small shield that represents the most recent volcanism in the Auckland Volcanic Field (AVF), New Zealand. Previous studies suggested construction in a relatively short interval at ~ 550–500 cal yrs BP. In contrast, the tephra record shows evidence of intermittent activity from 1498 ± 140 to (at least) 504 ± 6 cal yrs BP, a longevity of ~ 1000 years. Rangitoto volcano is thought to represent about half the magma erupted in the 250-ka-history of AVF. Thus, the AVF has experienced a dramatic shift to prolonged and voluminous central-vent volcanism in its most recent history. This demonstrates the difficulty in determining time-erupted volume relationships in such fields. Previous AVF hazard-risk modeling based on isolated, short-lived (< 1 year) phenomena at sites that have not experienced activity needs to be revisited in light of the new Rangitoto chronology.