This thesis provides a critical review of the Transition movement, a grassroots response to peak oil and climate change, co-founded by this author. It focuses on two key aspects of the Transition approach, resilience and economic relocalisation, with the aim of analysing whether and how they can be implemented in a locality based on the Transition approach, and assessing what socio-economic and community-related structures would be necessary to implement such a process. The focus of the research is Totnes, Devon, which because of its status as the UK’s first Transition initiative and the longer history of various initiatives to promote local resilience, offers a valuable case study of attempts to practically implement resilience and localisation. A variety of research methods were employed, including surveys, focus groups, oral history and in-depth interviews, as well less conventional public participation methods such as Open Space and World Café. The first major finding was that Transition Town Totnes (TTT) has become a significant organisation in the town, with a high level of popular support. It was also found that the obstacles to resilience and relocalisation lie not, as was hypothesised, in a lack of skills or an absence of community cohesion, but in issues of governance and the need for increased social entrepreneurship. It was found that what researchers call the ‘Value Action Gap’ (i.e. the gap between people’s declared sympathies and intentions and their actions) exists in Totnes as much as anywhere else, but that some of TTT’s projects, such as ‘Transition Together’, are working imaginatively to overcome this and to reduce emissions. From this evidence is it concluded that Transition’s approach towards relocalisation and reducing carbon emissions can be argued to be effective in, generating engagement and initiating new enterprises. Like other ‘green’ initiatives, it struggles to engage those from more disadvantaged backgrounds, but some of its initiatives are showing promise for overcoming this. Its primary contribution is in suggesting a redefining of resilience, not as a state of preparedness for disaster, but as a desired characteristic of a sustainable society. A more resilient community, it is argued, would be one more in control of its food and energy production, as well as being one that enables inward financial investment. It also argues that the government focus on ‘localism’, the devolving of political power to the local level, ought to be expanded to include ‘localisation’, the strengthening of local production to meet local needs, a shift which would financially benefit local communities. It argues that the key challenge for Transition initiatives such as TTT is going to be scaling up from being ‘niche’ organisations to become economically viable organisations with a broad appeal and engagement, and also articulates the need for ‘Resilience Indicators’ which would allow communities to measure the degree to which their levels of resilience are increasing.

This thesis innovates on existing literature on the Transition movement by relinquishing stock academic definitions of its ends and means, which purportedly spell out what Transition 'is'. In its stead, it approaches Transition as phenomenon, namely as an evolving socio-material formation that proliferates a cultural repertoire to sustain a growing range of concerted everyday activities. This is the difference between an instrumental focus, whereby Transition is reduced to a strategy which is oriented towards an unchanging programmatic definition, and an orientational one; the latter attuned to the contingent process by which a movement expresses form and orientation in emergent fashion. The monograph and the introductory chapter contribute to this task in different ways. Everything Gardens and Other Stories undertakes a rich description of various practical realms of Transition and, to capture the coming into being of a phenomenon, it pays particular attention to its developmental trajectory. This entails focusing on the generative movement of the culture of Transition, as it emerges from the attempt to address embodied disquiets originally elicited by information about peak oil and climate change. That initial focus, however, forms merely a station along a path in which new sources of anxiety find validation and prompt further cultural production. The monograph also describes the tensions arising in the process, as a growing body of discursive and material resources have to negotiate an accommodation, in order to become reciprocally recognisable as participant parts enfolded in a common cultural milieu. The introductory chapter supports this account by fleshing out a methodological paradigm that helps direct attention to the unfolding of a socio-material phenomenon in its dilemmatic moments and continual negotiations. For this purpose, starting from canonical sources in phenomenology, it goes on to situate the 'unfolding' of a phenomenon in the proliferation of entanglements between actors, human and nonhuman. In the 'mattering' of a phenomenon so understood, dilemmatic moments call forth an ethical questioning and an ontological politics immanent to the very process of cultural production. This, it is submitted, is precisely how an orientational focus allows to access Transition as phenomenon, beyond the bounds of academic definitions.

In the summer of 1611, Sir George Carew, the Irish Elizabethan military commander and former president of Munster, was commissioned by the king and his royal council in London to conduct an enquiry into all aspects of the Castle administration. Included in that wide mandate was an investigation into the existing practices and procedures of the Irish exchequer and judiciary, the two most important divisions of the Dublin government. This thesis is concerned with these two aspects of the commission of Sir George Carew. Since it is requisite for an understanding of the terms of reference handed to Sir George Carew in 1611, the study includes an analysis of the exchequer and judiciary between 1603 and 1611. In addition, there is an examination of the fiscal and judicial reforms that the king and his councillors commanded Irish officials to implement between 1613 and 1616. As is shown, these reformist measures were a direct outgrowth of recommendations submitted by Sir George Carew to the English privy council following the conclusion of his commission in 1611.

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During the Geological Survey of Canada’s Cumberland Peninsula Integrated Geoscience project a ~150km long NE-SW trending volcanic belt, now termed the North Touak-Cape Dyer volcanic belt, was mapped. The volcanic rocks that comprise the belt are dominantly green weathering komatiitic rocks with some black weathering tholeiitic occurrences. Given the similar stratigraphic position, textures, mineralogy, and geochemical characteristics of the volcanic rocks throughout the belt they have been termed the Totnes Road formation, after the locality from which they were first described. The komatiitic rocks possess numerous unusual characteristics for ultramafic volcanic rocks including: fragmental textures, lack of spinifex texture, young eruption age (Paleoproterozoic), eruption through ancient continental crust, and enrichment in the HFSEs including the REEs. This places them in the uncommon and poorly understood sub-type of komatiites termed Karasjok-type komatiites. Given the ultramafic nature of the rocks and their within-plate geochemical signatures, a mantle plume is the most likely source of these rocks, with the komatiites being sourced from the hot plume axis and the tholeiites from the cooler plume head. Incorporation and melting of mantle enriched by the addition of subduction zone recycled, garnet-bearing eclogitic material, beneath thick lithosphere could cause the rocks geochemical enrichment. Stratigraphically overlying the Totnes Road formation is a variety of chemical sedimentary rocks including chert, sulphide and silicate facies iron formation, and sulphide-rich boulders. Given their consistent stratigraphic position and parallel REE patterns, these rocks have been interpreted as a co-genetic suite and are grouped under the Clephane Bay formation, after a locality that exposes a spectacular section of the chemical rocks. The variety of lithologies is believed to be due to mixing of hydrothermal and detrital inputs during deposition within an anoxic basin. Regional correlations in the area are tentative due to the lack of available geochronological and geochemical data. Mafic-ultramafic volcanic occurrences to both the north and the south of the Cumberland Peninsula show remarkably similar geochemical characteristics to the Totnes Road formation. Thus it is possible that one plume was the source for numerous volcanic occurrences within in the region but more detailed study is required to prove or disprove this possibility.