title: What’s in a name? The sense of reference, the rigidity of designators and the history of causes when determining the names of the two main islands of Aotearoa/New Zealand

authors: Parker, Martin

subjects: New Zealand

abstract: The New Zealand Geographic Board recently revealed that the two main islands of Aotearoa/New Zealand have never been officially named. The revelation made both national and international news and led to a large number of publicly aired comments on the matter, suggesting that something so fundamental and seemingly innocuous as naming is in fact likely to generate a good deal of controversy, no more so than in a bicultural/bilingual context. This paper will examine the phenomenon of naming from a number of angles. After discussing a layperson’s idea of what is meant by the meaning of names, we shall attempt to apply a number of theoretical models from the field of Language Philosophy to the case of the main islands of Aotearoa/New Zealand: the Descriptivist approach of Frege and Russell, Kripke’s Rigid Designators, and Causal Grounding theory. We shall conclude that, in the case of applying the first two of these, there is a question mark over whether any of the current names for the two islands, both Māori and Pākehā, are in fact names at all; in terms of applying the theory of Causal Grounding, we are drawn to the conclusion that in history lies the key to the future.

text: What’s in a name? The sense of reference, the rigidity of designators and the history of causes when determining the names of the two main islands of Aotearoa/New Zealand The New Zealand Geographic Board recently revealed that the two main islands of Aotearoa/New Zealand have never been officially named. The revelation made both national and international news and led to a large number of publicly aired comments on the matter, suggesting that something so fundamental and seemingly innocuous as naming is in fact likely to generate a good deal of controversy, no more so than in a bicultural/bilingual context. This paper will examine the phenomenon of naming from a number of angles. After discussing a layperson’s idea of what is meant by the meaning of names, we shall attempt to apply a number of theoretical models from the field of Language Philosophy to the case of the main islands of Aotearoa/New Zealand: the Descriptivist approach of Frege and Russell, Kripke’s Rigid Designators, and Causal Grounding theory. We shall conclude that, in the case of applying the first two of these, there is a question mark over whether any of the current names for the two islands, both Māori and Pākehā, are in fact names at all; in terms of applying the theory of Causal Grounding, we are drawn to the conclusion that in history lies the key to the future.

year: 2010-02

title: Te Piringa

authors: Dickson, Matiu

abstract: Māori have an oral tradition, that is, the transfer of knowledge within and between generations, which was carried out orally by way of story-telling or the more formal speech-making. Ngā korero purākau are the stories and whaikōrero is formal talking on the marae or ancestral gathering places of Māori people. The value of public speaking is expressed in the saying: Ko te kōrerote kai a te Rangatira – (The chiefs thrive on talking and debating). This article looks at the transfer of knowledge to the next generation.

text: Te Piringa Māori have an oral tradition, that is, the transfer of knowledge within and between generations, which was carried out orally by way of story-telling or the more formal speech-making. Ngā korero purākau are the stories and whaikōrero is formal talking on the marae or ancestral gathering places of Māori people. The value of public speaking is expressed in the saying: Ko te kōrerote kai a te Rangatira – (The chiefs thrive on talking and debating). This article looks at the transfer of knowledge to the next generation.

year: 2010

title: Stratigraphy and chronology of a 15ka sequence of multi-sourced silicic tephras in a montane peat bog, eastern North Island, New Zealand.

authors: Lowe, David J.

subjects: tephra

abstract: We document the stratigraphy, composition, and chronology of a succession of 16 distal, silicic tephra layers interbedded with lateglacial and Holocene peats and muds up to c. 15 000 radiocarbon years (c. 18 000 calendar years) old at a montane site (Kaipo Bog) in eastern North Island, New Zealand. Aged from 665 +/- 15 to 14 700 +/- 95 14C yr BP, the tephras are derived from six volcanic centres in North Island, three of which are rhyolitic (Okataina, Taupo, Maroa), one peralkaline (Tuhua), and two andesitic (Tongariro, Egmont). Correlations are based on multiple criteria: field properties and stratigraphic interrelationships, ferromagnesian silicate mineral assemblages, glass-shard major element composition (from electron microprobe analysis), and radiocarbon dating. We extend the known distribution of tephras in eastern North Island and provide compositional data that add to their potential usefulness as isochronous markers. The chronostratigraphic framework established for the Kaipo sequence, based on both site-specific and independently derived tephra-based radiocarbon ages, provides the basis for fine-resolution paleoenvironmental studies at a climatically sensitive terrestrial site from the mid latitudes of the Southern Hemisphere. Tephras identified as especially useful paleoenvironmental markers include Rerewhakaaitu and Waiohau (lateglacial), Konini (lateglacial-early Holocene), Tuhua (middle Holocene), and Taupo and Kaharoa (late Holocene).

text: Stratigraphy and chronology of a 15ka sequence of multi-sourced silicic tephras in a montane peat bog, eastern North Island, New Zealand. We document the stratigraphy, composition, and chronology of a succession of 16 distal, silicic tephra layers interbedded with lateglacial and Holocene peats and muds up to c. 15 000 radiocarbon years (c. 18 000 calendar years) old at a montane site (Kaipo Bog) in eastern North Island, New Zealand. Aged from 665 +/- 15 to 14 700 +/- 95 14C yr BP, the tephras are derived from six volcanic centres in North Island, three of which are rhyolitic (Okataina, Taupo, Maroa), one peralkaline (Tuhua), and two andesitic (Tongariro, Egmont). Correlations are based on multiple criteria: field properties and stratigraphic interrelationships, ferromagnesian silicate mineral assemblages, glass-shard major element composition (from electron microprobe analysis), and radiocarbon dating. We extend the known distribution of tephras in eastern North Island and provide compositional data that add to their potential usefulness as isochronous markers. The chronostratigraphic framework established for the Kaipo sequence, based on both site-specific and independently derived tephra-based radiocarbon ages, provides the basis for fine-resolution paleoenvironmental studies at a climatically sensitive terrestrial site from the mid latitudes of the Southern Hemisphere. Tephras identified as especially useful paleoenvironmental markers include Rerewhakaaitu and Waiohau (lateglacial), Konini (lateglacial-early Holocene), Tuhua (middle Holocene), and Taupo and Kaharoa (late Holocene).

year: 1999-12-01