title: Education outside the classroom in Aotearoa New Zealand - A comprehensive national study: Final Report

authors: Hill, Allen

abstract: Education outside the Classroom (EOTC) has a long and rich history in Aotearoa New Zealand schools (Lynch, 2006), contributing positively to the lives of many young New Zealanders. The purpose of this study was to gain a contemporary and comprehensive understanding of what EOTC is currently occurring in schools across, the value that schools see in/ascribe to EOTC, and the various challenges and factors that influence the provision of EOTC.  
Data for the EOTC Comprehensive National Study was gathered from late 2017 throughout 2018 utilising a multiphase mixed methods research design. Data collection involved a national EOTC questionnaire (NEOTCQ) completed by school leaders and EOTC coordinators’ (n=523), specific EOTC inventories from a small sample of schools (n=23), and individual and focus group interviews with school leaders and teachers (n=28), students (n=140) and LEOTC providers (n=9).
This executive summary provides a succinct overview of the key findings from the comprehensive final report. The summary comprises four key sections addressing: what schools are doing with EOTC, teacher and student perspectives on the value of EOTC, how school leaders and teachers view challenges associated with EOTC provision, and enablers of flourishing EOTC in schools.

text: Education outside the classroom in Aotearoa New Zealand - A comprehensive national study: Final Report Education outside the Classroom (EOTC) has a long and rich history in Aotearoa New Zealand schools (Lynch, 2006), contributing positively to the lives of many young New Zealanders. The purpose of this study was to gain a contemporary and comprehensive understanding of what EOTC is currently occurring in schools across, the value that schools see in/ascribe to EOTC, and the various challenges and factors that influence the provision of EOTC.  
Data for the EOTC Comprehensive National Study was gathered from late 2017 throughout 2018 utilising a multiphase mixed methods research design. Data collection involved a national EOTC questionnaire (NEOTCQ) completed by school leaders and EOTC coordinators’ (n=523), specific EOTC inventories from a small sample of schools (n=23), and individual and focus group interviews with school leaders and teachers (n=28), students (n=140) and LEOTC providers (n=9).
This executive summary provides a succinct overview of the key findings from the comprehensive final report. The summary comprises four key sections addressing: what schools are doing with EOTC, teacher and student perspectives on the value of EOTC, how school leaders and teachers view challenges associated with EOTC provision, and enablers of flourishing EOTC in schools.

year: 2020

title: Monitoring the landslide at Bramley Drive, Tauranga, NZ

authors: Moon, Vicki G.

subjects: landslide monitoring

abstract: Omokoroa Peninsula, Tauranga Harbour, is prone to landslides in sensitive pyroclastic soils, especially in coastal bluffs. The largest is the landslide at Bramley Drive that first occurred in 1979, and was reactivated in 2011 and 2012. Since 2012 the landslide has been monitored with laser scans, vibro-and static-CPT, pore water logging at 3 depths, and a borehole inclinometer. Laser scan results track degradation of the scarp and allow development of a preliminary magnitude-frequency curve for failure events on the scarp. To date the borehole inclinometer has shown no obvious shear surface development. However, deformations in phase with the solid earth tides are evident in the cumulative displacement plots. Layers of weak soils separated by sharp boundaries are believed to exaggerate the deformations of the solid earth tides to the extent that they are measurable with a simple inclinometer. Residual deformation after subtraction of the earth tide effects indicate some movement over winter of 2014 associated with sensitive soils at or near the failure surface. The depth of this movement corresponds with a zone of high induced pore water pressures under vibratory CPTu. Pore water pressures indicate two discrete aquifers: an upper aquifer in tephra layers high in the upper part of the sequence that responds to atmospheric pressures; and a second aquifer in the underlying ignimbrites. Pressures in the bottom aquifer are lower than in the overlying aquifer in summer and higher in winter. Large spikes in pore water pressure have been observed during winter of 2014; these coincide with the time of deformation noted in the inclinometer traces.

text: Monitoring the landslide at Bramley Drive, Tauranga, NZ Omokoroa Peninsula, Tauranga Harbour, is prone to landslides in sensitive pyroclastic soils, especially in coastal bluffs. The largest is the landslide at Bramley Drive that first occurred in 1979, and was reactivated in 2011 and 2012. Since 2012 the landslide has been monitored with laser scans, vibro-and static-CPT, pore water logging at 3 depths, and a borehole inclinometer. Laser scan results track degradation of the scarp and allow development of a preliminary magnitude-frequency curve for failure events on the scarp. To date the borehole inclinometer has shown no obvious shear surface development. However, deformations in phase with the solid earth tides are evident in the cumulative displacement plots. Layers of weak soils separated by sharp boundaries are believed to exaggerate the deformations of the solid earth tides to the extent that they are measurable with a simple inclinometer. Residual deformation after subtraction of the earth tide effects indicate some movement over winter of 2014 associated with sensitive soils at or near the failure surface. The depth of this movement corresponds with a zone of high induced pore water pressures under vibratory CPTu. Pore water pressures indicate two discrete aquifers: an upper aquifer in tephra layers high in the upper part of the sequence that responds to atmospheric pressures; and a second aquifer in the underlying ignimbrites. Pressures in the bottom aquifer are lower than in the overlying aquifer in summer and higher in winter. Large spikes in pore water pressure have been observed during winter of 2014; these coincide with the time of deformation noted in the inclinometer traces.

year: 2015

title: The Waikato River settlement: Exploring a model for co-management and protection of natural and cultural resources

authors: Te Aho, Linda

abstract: This presentation explores co-management regimes in Aotearoa, including the framework established under the Waikato River Settlement, which mandates the protection and restoration of the river’s health and well being for present and future generations.

text: The Waikato River settlement: Exploring a model for co-management and protection of natural and cultural resources This presentation explores co-management regimes in Aotearoa, including the framework established under the Waikato River Settlement, which mandates the protection and restoration of the river’s health and well being for present and future generations.

year: 2015