title: Just take a second to breathe: Empowering youth through mindfulness at Atawhai 2019

authors: McAllister, Suzanne Maree

subjects: Mindfulness

abstract: This research was an evaluation of The Kindness Institute’s 2019 Atawhai programme. It examined the effects that exposure to mindfulness-based skills, Māori cultural practices, mentoring, and the creative arts had on a cohort of marginalised youth. Specifically, the research aimed to determine (1) if learning mindfulness-based skills helped the youth to positively deal with challenges, (2) what effect learning mindfulness-based skills has on their positive and negative emotions and (3) were youth empowered to share the skills they learned within their homes, families and communities to enable a wider benefit from the mindfulness-based skills. Participants included 12 youth who attended the Atawhai programme during 2019. They all completed shortened versions of the Five Facet Mindfulness Questionnaire (FFMQ), Adolescent Self-Regulatory Inventory (ASRI), The Oxford Happiness Questionnaire (OHQ), Revised Children’s Anxiety and Depression Scale (RCADS) and Self-Compassion Scale (SCS) at seven stages over a nine-month period from March 2019 to December 2019. Self-report debrief questionnaires and researcher observations were recorded during the October 2019 residential intensive of 5 days. Inferential statistics (repeated measures ANOVA and post-hoc paired t-tests) indicated a statistically significant increase in positive emotions (p<0.01) with a large effect 1.07 over the duration of the evaluation period from March 2019 to December 2019; the October 2019 intensive, p<0.01, d=1.37; and the April 2019 intensive, p<0.01, d=1.89. Statistically significant decreases in anxiety (p<0.01) with a large effect d=1.99 were indicated over the duration of the evaluation period from March 2019 to December 2019; the October 2019 intensive, p=0.07, d=0.57; and the April 2019 intensive, p≤0.01, d=1.19. Self-report measures indicated the youth; found the mindfulness-based skills beneficial, preferred a particular skill over others, and found their mentors supportive in helping them incorporate the skills into their daily lives. Youth reported they had continued their mindfulness-based practice outside Atawhai and were regularly sharing the skills within their homes, families and communities including their schools. These findings suggest the Atawhai programme has a profound and significant positive effect on the wellbeing of the young people it serves.

text: Just take a second to breathe: Empowering youth through mindfulness at Atawhai 2019 This research was an evaluation of The Kindness Institute’s 2019 Atawhai programme. It examined the effects that exposure to mindfulness-based skills, Māori cultural practices, mentoring, and the creative arts had on a cohort of marginalised youth. Specifically, the research aimed to determine (1) if learning mindfulness-based skills helped the youth to positively deal with challenges, (2) what effect learning mindfulness-based skills has on their positive and negative emotions and (3) were youth empowered to share the skills they learned within their homes, families and communities to enable a wider benefit from the mindfulness-based skills. Participants included 12 youth who attended the Atawhai programme during 2019. They all completed shortened versions of the Five Facet Mindfulness Questionnaire (FFMQ), Adolescent Self-Regulatory Inventory (ASRI), The Oxford Happiness Questionnaire (OHQ), Revised Children’s Anxiety and Depression Scale (RCADS) and Self-Compassion Scale (SCS) at seven stages over a nine-month period from March 2019 to December 2019. Self-report debrief questionnaires and researcher observations were recorded during the October 2019 residential intensive of 5 days. Inferential statistics (repeated measures ANOVA and post-hoc paired t-tests) indicated a statistically significant increase in positive emotions (p<0.01) with a large effect 1.07 over the duration of the evaluation period from March 2019 to December 2019; the October 2019 intensive, p<0.01, d=1.37; and the April 2019 intensive, p<0.01, d=1.89. Statistically significant decreases in anxiety (p<0.01) with a large effect d=1.99 were indicated over the duration of the evaluation period from March 2019 to December 2019; the October 2019 intensive, p=0.07, d=0.57; and the April 2019 intensive, p≤0.01, d=1.19. Self-report measures indicated the youth; found the mindfulness-based skills beneficial, preferred a particular skill over others, and found their mentors supportive in helping them incorporate the skills into their daily lives. Youth reported they had continued their mindfulness-based practice outside Atawhai and were regularly sharing the skills within their homes, families and communities including their schools. These findings suggest the Atawhai programme has a profound and significant positive effect on the wellbeing of the young people it serves.

year: 2020

title: Māori child rearing and infant sleep practices

authors: Jones, Horiana Majorie

abstract: Sleep is important to a healthy lifestyle for parents and children, and having effective ways of putting a child to sleep contributes significantly to mental and physical wellbeing. Cultural groups around the world have developed a variety of approaches to this task, for example, rocking, co-sleeping, bed-sharing, breastfeeding to sleep, and encouraging infants to self soothe through various methods of infant sleep training. In New Zealand the continuation of traditional Māori approaches to infant sleep, e.g. co-sleeping, bed-sharing, responsivity to infant cues have been over-shadowed by its negative association with sudden infant death syndrome (SIDS) and dependence on parent interaction when initiating infant sleep. In this study, we were interested in the approaches Māori parents used to put their pēpi (child, 2 months-2 years of age) to sleep and the various factors that have influenced these approaches. Data were collected through online surveys (n =58) and face-to-face interviews (n =10) with Māori parents. Survey results indicated that being held and breast or bottle fed to sleep were the most practiced techniques by Māori parents. Parent assisted approaches, e.g., rocking, feeding, lying with baby until they go to sleep, were the most practiced. Many parents planned for their babies to sleep separately but very few actually persisted with self-soothing approaches due to a number of factors, such as discomfort with listening to their babies cry, culture, whānau (extended families) influences safety, and convenience. The majority of participants expressed a desire for separate sleep; however, few within the interview group actually successfully practiced separate sleep regularly.

text: Māori child rearing and infant sleep practices Sleep is important to a healthy lifestyle for parents and children, and having effective ways of putting a child to sleep contributes significantly to mental and physical wellbeing. Cultural groups around the world have developed a variety of approaches to this task, for example, rocking, co-sleeping, bed-sharing, breastfeeding to sleep, and encouraging infants to self soothe through various methods of infant sleep training. In New Zealand the continuation of traditional Māori approaches to infant sleep, e.g. co-sleeping, bed-sharing, responsivity to infant cues have been over-shadowed by its negative association with sudden infant death syndrome (SIDS) and dependence on parent interaction when initiating infant sleep. In this study, we were interested in the approaches Māori parents used to put their pēpi (child, 2 months-2 years of age) to sleep and the various factors that have influenced these approaches. Data were collected through online surveys (n =58) and face-to-face interviews (n =10) with Māori parents. Survey results indicated that being held and breast or bottle fed to sleep were the most practiced techniques by Māori parents. Parent assisted approaches, e.g., rocking, feeding, lying with baby until they go to sleep, were the most practiced. Many parents planned for their babies to sleep separately but very few actually persisted with self-soothing approaches due to a number of factors, such as discomfort with listening to their babies cry, culture, whānau (extended families) influences safety, and convenience. The majority of participants expressed a desire for separate sleep; however, few within the interview group actually successfully practiced separate sleep regularly.

year: 2017

title: Ngauruhoe inner crater volcanic processes of the 1954-1955 and 1974-1975 eruptions

authors: Krippner, Janine Barbara

subjects: volcano

abstract: Ngauruhoe is an active basaltic andesite to andesite composite cone volcano at the southern end of the Tongariro volcanic complex, and most recently erupted in 1954-55 and 1974-75. These eruptions constructed the inner crater of Ngauruhoe, largely composed of 1954-55 deposits, which are the basis of this study. The inner crater stratigraphy, exposed on the southern wall, is divided into seven lithostratigraphic units (A to G), while the northern stratigraphy is obscured by the inward collapse of the crater rim. The units are, from oldest to youngest: Unit A, (17.5 m thick), a densely agglutinated spatter deposit with sharp clast outlines; Unit B, (11.2 m) a thick scoria lapilli deposit with local agglutination and scattered spatter bombs up to 1 m in length; Unit C, (6.4 m thick) a clastogenic lava deposit with lateral variations in agglutination; and Unit D, (10 m thick) a scoria lapilli with varying local agglutination. The overlying Unit E (15 cm thick) is a fine ash fallout bed that represents the final vulcanian phase of the 1954-55 eruption. Unit F is a series of six lapilli and ash beds that represent the early vulcanian episode of the 1974-75 eruption. The uppermost Unit G (averaging 10 m thick) is a densely agglutinated spatter deposit that represents the later strombolian phase of the 1974-75 eruption. Units A-D juvenile clasts are porphyritic, with phenocrysts of plagioclase, orthopyroxene, clinopyroxene, minor olivine, within a microlitic glassy groundmass. Quartzose and greywacke xenoliths are common in most units, and are derived from the underlying basement. The 1954-55 and 1974-75 eruptions are a product of a short-lived, continental arc medium-K calc-alkaline magma. The magma originated from the mantle, then filtered through the crust, undergoing assimilation and fractionation, and evolving to basaltic andesite and andesite compositions. The magma body stagnated in shallow reservoirs where it underwent further crustal assimilation and fractionation of plagioclase and olivine, and homogenisation through magma mixing. Prior to the 1954-55 eruption a more primitive magma body was incorporated into the melt. The melt homogenised and fed both the 1954-55 and 1974-75 eruptions, with a residence time of at least 20 years. The 1954-55 eruption produced alternating basaltic andesite and andesite strombolian activity and more intense fire fountaining, erupting scoria and spatter that built up the bulk of the inner crater. A period of relative quiescence allowed the formation of a cooled, solid cap rock that resulted in the accumulation of pressure due to volatile exsolution and bubble coalescence. The fracturing of the cap rock then resulted in a vulcanian eruption, depositing a thin layer of fine ash and ballistic blocks. The 1974-75 eruption commenced with the rupturing of the near-solid cap rock from the 1954-55 eruption in an explosive vulcanian blast, the result of decompressional volatile exsolution and bubble coalescence, and possible magma-water interaction. The eruption later changed to strombolian style, producing a clastogenic lava that partially flowed back into the crater.

text: Ngauruhoe inner crater volcanic processes of the 1954-1955 and 1974-1975 eruptions Ngauruhoe is an active basaltic andesite to andesite composite cone volcano at the southern end of the Tongariro volcanic complex, and most recently erupted in 1954-55 and 1974-75. These eruptions constructed the inner crater of Ngauruhoe, largely composed of 1954-55 deposits, which are the basis of this study. The inner crater stratigraphy, exposed on the southern wall, is divided into seven lithostratigraphic units (A to G), while the northern stratigraphy is obscured by the inward collapse of the crater rim. The units are, from oldest to youngest: Unit A, (17.5 m thick), a densely agglutinated spatter deposit with sharp clast outlines; Unit B, (11.2 m) a thick scoria lapilli deposit with local agglutination and scattered spatter bombs up to 1 m in length; Unit C, (6.4 m thick) a clastogenic lava deposit with lateral variations in agglutination; and Unit D, (10 m thick) a scoria lapilli with varying local agglutination. The overlying Unit E (15 cm thick) is a fine ash fallout bed that represents the final vulcanian phase of the 1954-55 eruption. Unit F is a series of six lapilli and ash beds that represent the early vulcanian episode of the 1974-75 eruption. The uppermost Unit G (averaging 10 m thick) is a densely agglutinated spatter deposit that represents the later strombolian phase of the 1974-75 eruption. Units A-D juvenile clasts are porphyritic, with phenocrysts of plagioclase, orthopyroxene, clinopyroxene, minor olivine, within a microlitic glassy groundmass. Quartzose and greywacke xenoliths are common in most units, and are derived from the underlying basement. The 1954-55 and 1974-75 eruptions are a product of a short-lived, continental arc medium-K calc-alkaline magma. The magma originated from the mantle, then filtered through the crust, undergoing assimilation and fractionation, and evolving to basaltic andesite and andesite compositions. The magma body stagnated in shallow reservoirs where it underwent further crustal assimilation and fractionation of plagioclase and olivine, and homogenisation through magma mixing. Prior to the 1954-55 eruption a more primitive magma body was incorporated into the melt. The melt homogenised and fed both the 1954-55 and 1974-75 eruptions, with a residence time of at least 20 years. The 1954-55 eruption produced alternating basaltic andesite and andesite strombolian activity and more intense fire fountaining, erupting scoria and spatter that built up the bulk of the inner crater. A period of relative quiescence allowed the formation of a cooled, solid cap rock that resulted in the accumulation of pressure due to volatile exsolution and bubble coalescence. The fracturing of the cap rock then resulted in a vulcanian eruption, depositing a thin layer of fine ash and ballistic blocks. The 1974-75 eruption commenced with the rupturing of the near-solid cap rock from the 1954-55 eruption in an explosive vulcanian blast, the result of decompressional volatile exsolution and bubble coalescence, and possible magma-water interaction. The eruption later changed to strombolian style, producing a clastogenic lava that partially flowed back into the crater.

year: 2009