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Comparing and combining ethnographic records with active Māori histories to provide insights on tsunami hazard

Published online by Cambridge University Press:  03 March 2020

Darren N. King*
Affiliation:
Māori Environmental Research Centre (Te Kūwaha o Taihoro Nukurangi), National Institute of Water and Atmospheric Research Ltd (NIWA), Private Bag 99940, Auckland 1149, Aotearoa-New Zealand
Maurice Manawatu
Affiliation:
Archives and Whakapapa Unit, Te Rūnanga o Ngāi Tahu, P.O. Box 13046, Christchurch 8141, Aotearoa-New Zealand
Wendy S. Shaw
Affiliation:
Paleontology, Geobiology and Earth Archives Research Centre (PANGEA), School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney2052, Australia
*
*Corresponding author e-mail address: darren.king@niwa.co.nz (D.N. King)
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Abstract

Tectonic hazards have profoundly influenced Māori relationships with, and understandings of, the environment, with oral histories and ethnographic records referencing recurring encounters with volcanic eruptions, earthquakes, and tsunamis across Aotearoa-New Zealand. This research works alongside members of the Māori kin-group Ngāti Kuri to deliberate and compare active oral histories with two ethnographic records that potentially refer to ancestral experience with past tsunami(s) in the Kaikōura region. It applies an inductive-based methodology informed by “collaborative storytelling,” with the intent to appreciate the manner in which Ngāti Kuri interpret their past and present. The research affirms past catastrophic saltwater inundations and potential tectonic disturbances in the Kaikōura region. It also affirms that ethnographic records are not necessarily full or accurate accounts of historical events. The accounts presented here contribute to the reclaiming of Ngāti Kuri histories and point to new plural learning opportunities about coseismic tsunami hazard and history across the region.

Whakarāpopototanga

<span class='italic'>WHAKARĀPOPOTOTANGA</span>

Kua pākia nuitia ngā hononga o te Māori ki tōna taiao, otirā, tōna māramatanga anō ki tōna taiao, e ngā pūmate papaneke, ka kōrerotia ki ngā kōrero tuku, ki ngā tuhinga hītori mō te Māori nā Tauiwi anō, ētahi pupūtanga auau o te pahūtanga puia, o te rū whenua, o te tai āniwhaniwha hoki huri noa i Aotearoa-New Zealand. Ko tā tēnei rangahau he mahi ngātahi ki ētahi o te hapū o Ngāti Kuri, ki te wānanga, ki te whakataurite anō i ētahi kōrero tuku e kōrerotia tonutia ana, me ētahi tuhinga hītori e rua mō te Māori nā Tauiwi, tērā tonu pea e kōrero ana mō te pākia o ngā tūpuna e (t)ētahi tai āniwhaniwha o mua i te rohe o Kaikōura. Ka whāia he pūnaha, ko tōna tūāpapa ko ngā tirohanga ki te hapori, he mea tohutohu e “te tuku kōrero ā-kāhui”, me te whai kia mātau tātou ki te āhua e whakamāramatia ai e Ngāti Kuri tōna onamata, tōna nāianei hoki. Ka whakapūmau te rangahau i ētahi parawhenua ā-tai aituā nui o mua, ā, mē ētahi raru papaneke tērā tonu pea ka pupū ake ki te rohe o Kaikōura. E whakapūmau anō ana tēnei rangahau, ehara i te mea ka kapi rawa i ngā tuhinga hītori mō te Māori nā Tauiwi, ngā kōrero katoa, otirā, ngā kōrero tika, mō ngā pupūtanga o onamata. Ko ngā kōrero e whakaaturia ana i konei e taunaki nei i te whakamanatanga o ngā kōrero tuku iho a Ngāti Kuri ake, otirā, e tohu anō ana i ētahi ara mātāpuna-tini hei whai māramatanga ki ngā pūmate tai āniwhaniwha, otirā, ki ngā kōrero tuku iho huri i te rohe.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2020
Figure 0

Figure 1: (color online) (A) Aotearoa-New Zealand's tectonic location in the South Pacific showing the Australian-Pacific plate boundary as a dashed red line. The submerged continental shelf boundary is loosely defined by the 2000 m isobaths (adapted from Carter et al. (1988)). (B) The Kaikōura coast and surrounding locations mentioned in active oral histories and ethnographical records (Photo source: Land Information New Zealand, 2004/05).