Timing of the most recent surface rupture event on the Ohariu Fault near Paraparaumu, New Zealand

N. Litchfield; R. Van Dissen; Rob Langridge; D. Heron; C. Prentice

doi:10.1080/00288306.2004.9515041

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Timing of the most recent surface rupture event on the Ohariu Fault near Paraparaumu, New Zealand

N. Litchfield·R. Van Dissen·Rob Langridge·D. Heron·C. Prentice

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Abstract

Thirteen radiocarbon ages from three trenches across the Ohariu Fault tightly constrain the timing of the most recent surface rupture event at Muaupoko Stream valley, c. 2 km east of Paraparaumu, to between 930 and 1050 cal. yr BP. This age overlaps with previously published ages of the most recent event on the Ohariu Fault and together they further constrain the event to 1000-1050 cal. yr BP. Two trenches provide loose constraints on the maximum recurrence interval at 3-7000 yr. Tephra, most probably the Kawakawa Tephra, was found within alluvial fan deposits in two of the trenches. ?? The Royal Society of New Zealand 2004.

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N. Litchfield, R. Van Dissen, Rob Langridge, D. Heron, C. Prentice. 2004. Timing of the most recent surface rupture event on the Ohariu Fault near Paraparaumu, New Zealand. https://doi.org/10.1080/00288306.2004.9515041

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