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The paleotsunami record of the Auckland region and implications for understanding tsunami hazards
Published in New Zealand Journal of Geology and Geophysics, 2022
Kate Clark, Regine Morgenstern
The NZPD has an entry for Okiwi, a site located ∼2 km south of the Whangapoua Bay gravel deposit. This site has a poor validity ranking and the NZPD entry describes the evidence as a ‘modified soil’ with additional notes saying there is a ‘much disturbed midden’ and hummocky topography (‘or tsunami geomorphology’) was observed. We could not find descriptions matching a ‘much disturbed midden’ in the primary reference material of Prince and Clough (2001) and evidence for paleotsunami at Okiwi seems highly subjective.