Taranaki wharf in Wellington

Wellington is the capital of New Zealand, located on the southern tip of the North Island, and is a windy city, the southern-most capital city in the world and the only in the Roaring Forties. In climate it is closer to its neighbour, the South Island than to the mild major city of the north, Auckland. Yet despite, or perhaps because of this, Wellington is the undisputed cultural capital of New Zealand, with much contem porary art, design music and media coming from this town that has an absurd amount of hip bars and cafes for a population this size: 164,000 approximately. The conjunction in Lord of the Rings of incredible nature and amazing production seems to characterise the rich culture/nature hybrid that Wellington distils, the microcosm of the things that make New Zealand such an incredible place.

Controls on mid-Holocene fringing reef growth and termination in a high latitude, estuarine setting, Wellington Point, Southeast Queensland

Several fringing coral reefs in Moreton Bay, Southeast Queensland, some 300 km south of the Great Barrier Reef (GBR), are set in a relatively high latitude, estuarine environment that is considered marginal for coral growth. Previous work indicated that these marginal reefs, as with many fringing reefs of the inner GBR, ceased accreting in the mid-Holocene. This research presents for the first time data from the subsurface profile of the mid-Holocene fossil reef at Wellington Point comprising U/Th dates of in situ and framework corals, and trace element analysis from the age constrained carbonate fragments. Based on trace element proxies the palaeo-water quality during reef accretion was reconstructed. Results demonstrate that the reef initiated more than 7,000 yr BP during the post glacial transgression, and the initiation progressed to the west as sea level rose. In situ micro-atolls indicate that sea level was at least 1 m above present mean sea level by 6,680 years ago. The reef remained in "catch-up" mode, with a seaward sloping upper surface, until it stopped aggrading abruptly at ca 6,000 yr BP; no lateral progradation occurred. Changes in sediment composition encountered in the cores suggest that after the laterite substrate was covered by the reef, most of the sediment was produced by the carbonate factory with minimal terrigenous influence. Rare earth element, Y and Ba proxies indicate that water quality during reef accretion was similar to oceanic waters, considered suitable for coral growth. A slight decline in water quality on the basis of increased Ba in the later stages of growth may be related to increased riverine input and partial closing up of the bay due to either tidal delta progradation, climatic change and/or slight sea level fall. The age data suggest that termination of reef growth coincided with a slight lowering of sea level, activation of ENSO and consequent increase in seasonality, lowering of temperatures and the constrictions to oceanic flushing. At the cessation of reef accretion the environmental conditions in the western Moreton Bay were changing from open marine to estuarine. The living coral community appears to be similar to the fossil community, but without the branching Acropora spp. that were more common in the fossil reef. In this marginal setting coral growth periods do not always correspond to periods of reef accretion due to insufficient coral abundance. Due to several environmental constraints modern coral growth is insufficient for reef growth. Based on these findings Moreton Bay may be unsuitable as a long term coral refuge for most species currently living in the GBR.

Assessing the property market impact of stigma removal : high voltage overhead transmission lines removal in Wellington, NZ

This thesis advances the understanding of the impact of stigma on property values. A case study in Wellington, New Zealand, enabled hedonic modelling and an empirical analysis to determine the impact of the stigma from the high voltage transmission line structure and how long the stigma remained after removal. The results reveal a substantial difference between the discount applied to individual properties while the structure is in place, as compared to the overall increase in neighbourhood value once the structure, which created the stigma, is removed.

A formação de professores no curso Pré-vestibular Comunitário Prof. Wellington Ricardo

Essa pesquisa trata da investigação da formação na docência no curso Pré-Vestibular Comunitário Prof. Wellington Ricardo, com sede na periferia da cidade do Rio de Janeiro, e busca avaliar como os docentes deste curso, imbuídos da construção de um ensino popular, articulam e desenvolvem diferentes saberes e práticas que passam a se constituir como características importantes de sua constituição como professor. O estudo tem como objetivos conhecer o pensamento dos docentes deste curso a respeito do que é ser professor e o seu papel na sociedade, e também verificar de que maneiras esses docentes aprimoram sua formação e a sua prática como professores atuando no WR. Para tanto, alguns elementos foram considerados, como: a história escolar dos professores do curso, sua formação inicial, bem como os fatores de contexto relacionados a diferentes vivências junto à equipe do WR que influenciam nessa aprendizagem. Os pressupostos metodológicos utilizados neste estudo se coadunam com aqueles desenvolvidos pela chamada crítica imanente e investem na possibilidade da construção de uma teoria dialética da formação de professores, visando contribuir para a constituição não-metafísica do sujeito. Este trabalho endossa a perspectiva que a comunicação inconsciente influencia, de modo muito mais efetivo e prático, do que a comunicação verbal (racionalizada pelos indivíduos), o entendimento sobre o processo de formação do magistério. A vivência proveniente da inserção desses docentes numa comunidade não-totalizante e sem hierarquias permite que competências e habilidades que dificilmente seriam possíveis num curso de formação ou numa estrutura formal de ensino fossem edificadas e difundidas com sucesso. Desse modo, pode-se constatar na pesquisa, o incremento de uma nova forma de pensar e atuar politicamente, inventada pelos docentes WR. Assim, os docentes do curso reconstroem em seu dia-a-dia uma nova maneira de fazer e viver a política. Essa reconstrução passa necessariamente pelo investimento que fazem no estabelecimento de relações de amizade e de vínculos sólidos entre seus participantes. Uma nova forma que investe na participação horizontal e valorização da solidariedade e da autonomia, que passa, por isso, a produzir uma espécie de cultura pedagógica, que serve como apoio para a formação política e também profissional dos próprios docentes.

Quaternary geology of the Campbellford, Trenton, Consecon, Tweed, Belleville, Wellington, Sydenham, Bath, and Yorkshire Island map-areas, Ontario /

Sediment relationships observed during geological mapping in southeastern Ontario indicate a relatively simple deglaciation history for the area during late Wisconsin time. The ice from the north (part of the Lake Simcoe lobe) and the Lake Ontario ice lobe, which were coalesced during most of late Wisconsin time, initially separated along the crest of the Oak Ridges Moraine. Available data indicate that the Oak Ridges Moraine is composed primarily of sediments pre-late Wisconsin in age capped by late Wisconsin till and interlobate deposits. Retreat of the northern ice was relatively steady and resulted in the deposition of the Dummer Moraines, a facies of the drumlinized till to the south. Retreat of the Lake Ontario ice lobe into the Lake Ontario basin was interrupted by a re-advance which covered the southeastern half of the map area. The northern ice had already retreated from the area by this time. The Lake Ontario lobe was fed through the St. Lawrence Valley, indicating that the Ottawa Valley was ice filled at this time. High level glacial lakes fronted the ice during deglaciation. These waters quickly fell to low levels as the ice retreated from the St. Lawrence Valley, opening lower outlets.

Flit, fylleri och förbundsstatspotential : En undersökning av den nyzeeländska Sverigebilden i samband med skandinaviska emigranters ankomst till Wellington år 1871

This Bachelor’s thesis elucidates the subject of Swedish migration to New Zealand in 1871. Drawing on the work of Anthony Grigg, who has assessed the public opinions regarding the arrival of Scandinavians in 1871-1876, this study aims to highlight the image of Sweden and Swedes conveyed in New Zealand at this time. Through a hermeneutic engagement with newspapers of the day, it is concluded that Swedes in general were being portrayed as industrious, thrifty and well suited for the forestry labour expected of them. It is also shown, however, that Swedes and Sweden to a limited extent were being associated with notorious drinking habits and inferior intellectual abilities. Furthermore, the study highlights what appears to have been a medial difficulty to differentiate between Swedes and Norwegians.