title: Book Review: Nonproliferation Norms: Why states choose nuclear restraint

authors: Smith, Ron C.

subjects: Nonproliferation Norms: Why states choose nuclear restraint

abstract: The article reviews the book "Nonproliferation Norms: Why States Choose Nuclear Restraint," by Maria Rost Rublee.

text: Book Review: Nonproliferation Norms: Why states choose nuclear restraint The article reviews the book "Nonproliferation Norms: Why States Choose Nuclear Restraint," by Maria Rost Rublee.

year: 2009

title: Stratigraphy and chronology of the Stent tephra, a c. 4000 year old distal silicic tephra from Taupo Volcanic Centre, New Zealand.

authors: Alloway, Brent V.

subjects: Stratigraphy

abstract: Tephrostratigraphic and chronologic studies in two areas of the North Island have identified a previously unrecorded, thin, distal silicic tephra derived from the Taupo Volcanic Centre. In Taranaki, three radiocarbon ages of the uncorrelated tephra are consistent with the independent radiocarbon chronology obtained from enveloping Egmontsourced tephras. In western Bay of Plenty, where the uncorrelated tephra is also directly dated, it is overlain by Whakaipo Tephra (c. 2.7 ka) and underlain by Hinemaiaia Tephra (c. 4.5 ka). From these sites in Taranaki and western Bay of Plenty, seven radiocarbon dates obtained on the uncorrelated silicic tephra yield an error-weighted mean age of 3970 Â±31 conventional radiocarbon years B.P. The ages on the uncorrelated tephra (informally referred to as Stent tephra) from both areas are statistically identical but significantly different from those on both Waimihia and Hinemaiaia Tephras. occurrence of Stent tephra in Taranaki, c. 160 km upwind from the postulated source area, and in western Bay of Plenty, suggests that it represents the product of a moderately large plinian eruption. Until recently, its validity as a discrete eruptive event had been problematical, because a near-source equivalent deposit between Waimihia and Hinemaiaia Tephras was not recognised in the Taupo area. However, a revised stratigraphy proposed by C. J. N. Wilson in 1993 for eastern sectors of the Taupo area shows that multiple tephra layers were erupted from Taupo volcano between c. 3.9 and 5.2 ka. Of these newly recognised layers, unit-g--the product of a moderately large eruption (>0.15 km3) at c. 4.0 ka--is tentatively correlated with Stent tephra. Other eruptive units recognised by Wilson are either too old or too small in volume to be considered as likely correlatives.

text: Stratigraphy and chronology of the Stent tephra, a c. 4000 year old distal silicic tephra from Taupo Volcanic Centre, New Zealand. Tephrostratigraphic and chronologic studies in two areas of the North Island have identified a previously unrecorded, thin, distal silicic tephra derived from the Taupo Volcanic Centre. In Taranaki, three radiocarbon ages of the uncorrelated tephra are consistent with the independent radiocarbon chronology obtained from enveloping Egmontsourced tephras. In western Bay of Plenty, where the uncorrelated tephra is also directly dated, it is overlain by Whakaipo Tephra (c. 2.7 ka) and underlain by Hinemaiaia Tephra (c. 4.5 ka). From these sites in Taranaki and western Bay of Plenty, seven radiocarbon dates obtained on the uncorrelated silicic tephra yield an error-weighted mean age of 3970 Â±31 conventional radiocarbon years B.P. The ages on the uncorrelated tephra (informally referred to as Stent tephra) from both areas are statistically identical but significantly different from those on both Waimihia and Hinemaiaia Tephras. occurrence of Stent tephra in Taranaki, c. 160 km upwind from the postulated source area, and in western Bay of Plenty, suggests that it represents the product of a moderately large plinian eruption. Until recently, its validity as a discrete eruptive event had been problematical, because a near-source equivalent deposit between Waimihia and Hinemaiaia Tephras was not recognised in the Taupo area. However, a revised stratigraphy proposed by C. J. N. Wilson in 1993 for eastern sectors of the Taupo area shows that multiple tephra layers were erupted from Taupo volcano between c. 3.9 and 5.2 ka. Of these newly recognised layers, unit-g--the product of a moderately large eruption (>0.15 km3) at c. 4.0 ka--is tentatively correlated with Stent tephra. Other eruptive units recognised by Wilson are either too old or too small in volume to be considered as likely correlatives.

year: 1994-03-01

title: An external evaluation of Phat Pak process and structure: Volume 1: Evaluation report

authors: Masters-Awatere, Bridgette

subjects: psychology

abstract: An evaluation was conducted by the 510 Evaluation Research Group 2007 after receiving a request from the Phat Pak Governance Group (PPGG). The evaluation focused on four areas identified in the Phat Pak service specification plan attached to it’s Ministry of Health contract (Youth participation, Communication Strategies, Decision making Processes and Skills Development). Our intention of evaluating the Phat Pak Programme has been to, through feedback from a range of participants, gauge the extent that the programme objectives (such as those highlighted in the contract are being met. More specifically, the function of the evaluation has been to help identify specific areas that are working well and those areas that need further development. It is our intention that the evaluation will provide both short and long-term direction with added insight towards increasing participation and enhancing health outcomes for youth and the wider community of the Waikato region.

text: An external evaluation of Phat Pak process and structure: Volume 1: Evaluation report An evaluation was conducted by the 510 Evaluation Research Group 2007 after receiving a request from the Phat Pak Governance Group (PPGG). The evaluation focused on four areas identified in the Phat Pak service specification plan attached to it’s Ministry of Health contract (Youth participation, Communication Strategies, Decision making Processes and Skills Development). Our intention of evaluating the Phat Pak Programme has been to, through feedback from a range of participants, gauge the extent that the programme objectives (such as those highlighted in the contract are being met. More specifically, the function of the evaluation has been to help identify specific areas that are working well and those areas that need further development. It is our intention that the evaluation will provide both short and long-term direction with added insight towards increasing participation and enhancing health outcomes for youth and the wider community of the Waikato region.

year: 2007-12