title: The effectiveness of delineation treatments

authors: Charlton, Samuel G.

subjects: delineation

abstract: A literature review undertaken for Transit NZ has found that delineation has a significant effect on driver behaviour with, for example, shoulder rumble strips reducing run-off-theroad crashes by between 22% and 80% (average of 32% for all crashes and 44% for fatal run-of-the-road crashes). The concern that enhancing roadway delineation may sometimes be accompanied by an unwanted increase in drivers’ speeds (known as behavioural adaptation) is not borne out by the research and appears to be a phenomenon associated with a few restricted situations (e.g. where a centre line is added to an otherwise unmarked road).
The preponderance of the evidence supports the conclusion that profiled edge lines and centre lines provide drivers with positive guidance and produce significant reductions in crashes as a result of improving drivers’ lateral position. Further, unlike other safety measures that show decreased effectiveness over time due to a novelty effect, profiled lane delineation continues to work regardless of driver familiarity. There is no published research to suggest that profiled edge lines will decrease the effectiveness of a profiled centre line or will result in an increase in crash rates or an increase in the severity of crashes. However it has also been noted that local conditions have a major influence on the level of benefits that can be achieved through improved delineation.

text: The effectiveness of delineation treatments A literature review undertaken for Transit NZ has found that delineation has a significant effect on driver behaviour with, for example, shoulder rumble strips reducing run-off-theroad crashes by between 22% and 80% (average of 32% for all crashes and 44% for fatal run-of-the-road crashes). The concern that enhancing roadway delineation may sometimes be accompanied by an unwanted increase in drivers’ speeds (known as behavioural adaptation) is not borne out by the research and appears to be a phenomenon associated with a few restricted situations (e.g. where a centre line is added to an otherwise unmarked road).
The preponderance of the evidence supports the conclusion that profiled edge lines and centre lines provide drivers with positive guidance and produce significant reductions in crashes as a result of improving drivers’ lateral position. Further, unlike other safety measures that show decreased effectiveness over time due to a novelty effect, profiled lane delineation continues to work regardless of driver familiarity. There is no published research to suggest that profiled edge lines will decrease the effectiveness of a profiled centre line or will result in an increase in crash rates or an increase in the severity of crashes. However it has also been noted that local conditions have a major influence on the level of benefits that can be achieved through improved delineation.

year: 2005

title: Petrologic, geochemical and isotopic evolution of rhyolite lavas from the Okataina, Rotorua and Kapenga Volcanic Centres, Taupo Volcanic Zone, New Zealand

authors: Bowyer, Deborah Ann

abstract: The Okataina Volcanic Centre (OVC) is a highly active modern silicic magmatic system at the northeastern end of the central Taupo Volcanic Zone, North Island, New Zealand. This study presents a set of petrographic, mineralogical, geochemical and isotopic data that focuses on the rhyolite lavas erupted from the OVC. These data have been combined with existing geochronological data and knowledge of vent positions to identify magma types, and hence provide a model for the spatial and temporal evolution of the silicic magmatic system. Representative samples of OVC rhyolite lavas were analysed for whole rock major and trace elements by XRF (90 samples), trace and rare earth elements by LA-ICPMS (32), and Sr (25), Nd (8) and Pb (4) isotopes by TIMS. Major element compositions of phenocrysts in 24 representative lavas were determined by EPMA. Rhyolite lavas of the OVC contain phenocrysts (5 - 35 %) of plagioclase, quartz, Fe-Ti oxides ± orthopyroxene ± calcic amphibole ± cummingtonite ± biotite. Apatite and zircon are accessory. Temperatures determined from Fe-Ti oxide geothermometry range from ∼ 650 - 830°C. The lavas are dominantly peraluminous, medium-K, calc-alkaline rhyolites, with SiO₂ ≈ 72.5 - 77.5 wt. %,  ⁸⁷Sr/⁸⁶Sr ≈ 0.70516 - 0.70583, εNd ≈ 0.02 - 1.70, ²⁰⁶Pb/²⁰⁴Pb ≈ 18.75 - 18.84, ²⁰⁷Pb/²⁰⁴Pb ≈ 15.55 - 15.64 and ²⁰⁸Pb/²⁰⁴Pb ≈ 38.42 - 38.74. The volcanic history of the OVC can be subdivided into three periods, (i) > 220 ± 10 ka, (ii) 220 ± 10 - c. 65 ka, and (iii) < c. 65 ka. The two earlier periods involved eruption of caldera-forming ignimbrites and rhyolite lavas. The most recent period of activity involved eruption of the caldera-modifying Mangaone Pyroclastics Subgroup (c. 43 000 - 31 400 years B.P.), and the caldera-infilling rhyolite lavas and pyroclastics comprising the Haroharo, Okareka and Tarawera volcanic complexes (c. 25 000 years B.P. - present). In each period, a number of rhyolitic magma types or batches have been identified and distinguished based on their mineralogical, geochemical and isotopic characteristics. At least nine magma batches may have been erupted in the last 25 000 years, with estimated maximum generation times from c. 3 800 - 15 500 years, minimum generation rates from 3.1 x 10⁻⁴ - 3.2 x 10⁻³ km³/year, residence times from c. 4 000 - 31 000 years and erupted volumes generally < 15 km³. The Haroharo Volcanic Complex was built up in four rhyolitic eruptive episodes beginning c. 25 000 years B.P. The lavas and pyroclastics erupted in the Te Rere episode were derived from a single, genetically discrete, relatively volumetrically small magma batch. The lavas and pyroclastics erupted in the Rotoma, Mamaku and Whakatane episodes record the evolution of a relatively larger single magma batch over c. 4 000 years by closed-system fractional crystallisation processes. The Okareka Volcanic Complex was built up in two rhyolitic eruptive episodes at c. 25 000 and 15 800 years B.P., and a genetic relationship is suggested between the magma erupted in these episodes. The Tarawera Volcanic Complex was built up in four rhyolitic eruptive episodes beginning c. 22 500 years B.P. Multiple magma batches were erupted during the Okareka and Rerewhakaaitu episodes. The lavas and pyroclastics erupted in each of the two youngest episodes (Waiohau and Kaharoa) were derived from single, genetically discrete magma batches. The eruption of multiple, relatively small volume, genetically discrete magmas in the last c. 25 000 years precludes the coalescence of a large magma body beneath the OVC, and has implications for volcanic hazard assessment and eruption prediction. Future eruptions may involve either residual silicic magmas revived by basaltic intrusion, or basaltic magmas that have reached the surface without interacting with residual silicic magmas because they have crystallised, or new genetically discrete silicic magma. Mineralogical, geochemical and isotopic data obtained for rhyolite lavas erupted from the adjacent Rotorua and Kapenga volcanic centres reveal that their evolution has also involved eruption of multiple magma batches, but lack of geochemical, isotopic and age data preclude the development of any spatial and temporal models for these centres.

text: Petrologic, geochemical and isotopic evolution of rhyolite lavas from the Okataina, Rotorua and Kapenga Volcanic Centres, Taupo Volcanic Zone, New Zealand The Okataina Volcanic Centre (OVC) is a highly active modern silicic magmatic system at the northeastern end of the central Taupo Volcanic Zone, North Island, New Zealand. This study presents a set of petrographic, mineralogical, geochemical and isotopic data that focuses on the rhyolite lavas erupted from the OVC. These data have been combined with existing geochronological data and knowledge of vent positions to identify magma types, and hence provide a model for the spatial and temporal evolution of the silicic magmatic system. Representative samples of OVC rhyolite lavas were analysed for whole rock major and trace elements by XRF (90 samples), trace and rare earth elements by LA-ICPMS (32), and Sr (25), Nd (8) and Pb (4) isotopes by TIMS. Major element compositions of phenocrysts in 24 representative lavas were determined by EPMA. Rhyolite lavas of the OVC contain phenocrysts (5 - 35 %) of plagioclase, quartz, Fe-Ti oxides ± orthopyroxene ± calcic amphibole ± cummingtonite ± biotite. Apatite and zircon are accessory. Temperatures determined from Fe-Ti oxide geothermometry range from ∼ 650 - 830°C. The lavas are dominantly peraluminous, medium-K, calc-alkaline rhyolites, with SiO₂ ≈ 72.5 - 77.5 wt. %,  ⁸⁷Sr/⁸⁶Sr ≈ 0.70516 - 0.70583, εNd ≈ 0.02 - 1.70, ²⁰⁶Pb/²⁰⁴Pb ≈ 18.75 - 18.84, ²⁰⁷Pb/²⁰⁴Pb ≈ 15.55 - 15.64 and ²⁰⁸Pb/²⁰⁴Pb ≈ 38.42 - 38.74. The volcanic history of the OVC can be subdivided into three periods, (i) > 220 ± 10 ka, (ii) 220 ± 10 - c. 65 ka, and (iii) < c. 65 ka. The two earlier periods involved eruption of caldera-forming ignimbrites and rhyolite lavas. The most recent period of activity involved eruption of the caldera-modifying Mangaone Pyroclastics Subgroup (c. 43 000 - 31 400 years B.P.), and the caldera-infilling rhyolite lavas and pyroclastics comprising the Haroharo, Okareka and Tarawera volcanic complexes (c. 25 000 years B.P. - present). In each period, a number of rhyolitic magma types or batches have been identified and distinguished based on their mineralogical, geochemical and isotopic characteristics. At least nine magma batches may have been erupted in the last 25 000 years, with estimated maximum generation times from c. 3 800 - 15 500 years, minimum generation rates from 3.1 x 10⁻⁴ - 3.2 x 10⁻³ km³/year, residence times from c. 4 000 - 31 000 years and erupted volumes generally < 15 km³. The Haroharo Volcanic Complex was built up in four rhyolitic eruptive episodes beginning c. 25 000 years B.P. The lavas and pyroclastics erupted in the Te Rere episode were derived from a single, genetically discrete, relatively volumetrically small magma batch. The lavas and pyroclastics erupted in the Rotoma, Mamaku and Whakatane episodes record the evolution of a relatively larger single magma batch over c. 4 000 years by closed-system fractional crystallisation processes. The Okareka Volcanic Complex was built up in two rhyolitic eruptive episodes at c. 25 000 and 15 800 years B.P., and a genetic relationship is suggested between the magma erupted in these episodes. The Tarawera Volcanic Complex was built up in four rhyolitic eruptive episodes beginning c. 22 500 years B.P. Multiple magma batches were erupted during the Okareka and Rerewhakaaitu episodes. The lavas and pyroclastics erupted in each of the two youngest episodes (Waiohau and Kaharoa) were derived from single, genetically discrete magma batches. The eruption of multiple, relatively small volume, genetically discrete magmas in the last c. 25 000 years precludes the coalescence of a large magma body beneath the OVC, and has implications for volcanic hazard assessment and eruption prediction. Future eruptions may involve either residual silicic magmas revived by basaltic intrusion, or basaltic magmas that have reached the surface without interacting with residual silicic magmas because they have crystallised, or new genetically discrete silicic magma. Mineralogical, geochemical and isotopic data obtained for rhyolite lavas erupted from the adjacent Rotorua and Kapenga volcanic centres reveal that their evolution has also involved eruption of multiple magma batches, but lack of geochemical, isotopic and age data preclude the development of any spatial and temporal models for these centres.

year: 2001

title: Te manemanerau a te kāwanatanga: A history of the confiscation of Tūhoe lands in the Bay of Plenty

authors: Melbourne, Sydney

subjects: Ngāi Tūhoe

abstract: This thesis endeavours to show that Tūhoe lands should never have been confiscated and that Tūhoe efforts to gain compensation have been totally unsuccessful to date. When certain lands within the confiscated district of the Bay of Plenty were returned to the tribes there, Tūhoe were not granted any. Furthermore, lands which actually belonged to Tūhoe were granted to other tribes.
Although the major focus is on issues specific to Tūhoe, these are viewed within the wider context of nineteenth century land acquisition in New Zealand. This study looks at Tūhoe historical claims to disputed lands included in the confiscation district of the Bay of Plenty. Chapter One traces the extent of Tūhoe territories within the confiscation district and describes how Tūhoe came to occupy them and the duration of their occupation. Information about these claims came from tribal oral sources and original manuscripts, as well as from more generally accessible sources.
The development of colonial expansion patterns is discussed in Chapter Two. The contention is that they were based on materialistic considerations and legal pretexts to justify the acquisition of Māori lands. Hostilities between Māori and Government in the Bay of Plenty are dealt with in Chapter Three. Particular attention is paid to the causes of the hostilities and the complex racial and political misunderstandings which contributed to the inevitability of war. As a result of these encounters, the New Zealand Settlements Act was imposed.
Chapter Four covers the implementation of its provisions through the Compensation Court. The failings of this Court and its commissioners and field officials are exposed.
Chapter Five examines the settlement of Tūhoe lands in Ōpouriao and Waimana, as well as the changing fortunes of some of the settlers who took advantage of the settlement scheme. After placing the experiences of Tūhoe people within the wider context of what had taken place in New Zealand, Chapter Six focuses on Tūhoe attempts to bring the wrongs they had suffered to the attention of Government. In retrospect these early Tūhoe attempts at redress show that much has to be learnt about presenting substantial submissions. It was obvious that much of what was known by the elders then, though recorded, was never used in evidence to support their petitions. Nonetheless, without the existence of these manuscripts, present attempts would not be possible.
Chapter Seven gives a basis for a proposed just settlement for the confiscation of Tūhoe lands. In order to provide a guide for monetary compensation, details of values of Tūhoe confiscated land have been sought from official records. Compensation for the denial of justice, the loss of human life, land and property, remain open for negotiation.
Finally, while certain conclusions can be and are drawn from these investigations, the end of the story remains unwritten. It will depend on the outcome of new Tūhoe attempts to gain redress from the appropriate statutory body.

text: Te manemanerau a te kāwanatanga: A history of the confiscation of Tūhoe lands in the Bay of Plenty This thesis endeavours to show that Tūhoe lands should never have been confiscated and that Tūhoe efforts to gain compensation have been totally unsuccessful to date. When certain lands within the confiscated district of the Bay of Plenty were returned to the tribes there, Tūhoe were not granted any. Furthermore, lands which actually belonged to Tūhoe were granted to other tribes.
Although the major focus is on issues specific to Tūhoe, these are viewed within the wider context of nineteenth century land acquisition in New Zealand. This study looks at Tūhoe historical claims to disputed lands included in the confiscation district of the Bay of Plenty. Chapter One traces the extent of Tūhoe territories within the confiscation district and describes how Tūhoe came to occupy them and the duration of their occupation. Information about these claims came from tribal oral sources and original manuscripts, as well as from more generally accessible sources.
The development of colonial expansion patterns is discussed in Chapter Two. The contention is that they were based on materialistic considerations and legal pretexts to justify the acquisition of Māori lands. Hostilities between Māori and Government in the Bay of Plenty are dealt with in Chapter Three. Particular attention is paid to the causes of the hostilities and the complex racial and political misunderstandings which contributed to the inevitability of war. As a result of these encounters, the New Zealand Settlements Act was imposed.
Chapter Four covers the implementation of its provisions through the Compensation Court. The failings of this Court and its commissioners and field officials are exposed.
Chapter Five examines the settlement of Tūhoe lands in Ōpouriao and Waimana, as well as the changing fortunes of some of the settlers who took advantage of the settlement scheme. After placing the experiences of Tūhoe people within the wider context of what had taken place in New Zealand, Chapter Six focuses on Tūhoe attempts to bring the wrongs they had suffered to the attention of Government. In retrospect these early Tūhoe attempts at redress show that much has to be learnt about presenting substantial submissions. It was obvious that much of what was known by the elders then, though recorded, was never used in evidence to support their petitions. Nonetheless, without the existence of these manuscripts, present attempts would not be possible.
Chapter Seven gives a basis for a proposed just settlement for the confiscation of Tūhoe lands. In order to provide a guide for monetary compensation, details of values of Tūhoe confiscated land have been sought from official records. Compensation for the denial of justice, the loss of human life, land and property, remain open for negotiation.
Finally, while certain conclusions can be and are drawn from these investigations, the end of the story remains unwritten. It will depend on the outcome of new Tūhoe attempts to gain redress from the appropriate statutory body.

year: 1987