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As urban areas continue to expand into rural areas the world is experiencing a loss of productive agricultural land and diminishing natural habitats and associated ecosystems. The space where urban meets rural is known as the rural-urban fringe and what happens in these areas ultimately determines urban development patterns. Despite being such an important area, the rural-urban fringe is poorly understood and is often described as a “blurry” space – blurry in land patterns because it is where multiple uses collide and in how individuals interact in this space (since actors with often diverse opinions on how land should be used coexist there). Furthermore, there is no single body of scholarly literature that explains why and how decisions get made in rural-urban fringe areas. This thesis contributes to filling this gap in literature by helping to (i) understand and explain decision-making processes at the rural-urban fringe; (ii) create an analytical framework for understanding decision-making dynamics at the rural-urban fringe within two UNESCO Biosphere Reserves: the Cape Winelands Biosphere Reserve, South Africa and the Niagara Escarpment Biosphere Reserve, Canada; and (iii) construct a theory of decision-making for better outcomes at the rural-urban fringe. The analytical framework is divided into two parts with components drawn from problem-solving (including governance and management) and critical (critical political economy and resilience) theories. The premise is that each part contributes to a holistic understanding that they cannot accomplish on their own. The analytical framework is used as the analytical platform for consideration of the research data and is the basis on which the thesis’ theoretical contribution is built. Specifically, each case study is first examined within the context of existing governance and management processes. This reveals the character of key issues and dynamics and the resulting policy responses. The cases are then located within the broader analytical contexts of critical political economy and resilience. This reveals the historical and structural dynamics often overlooked or neglected in problem-solving approaches. The thesis reveals that in both case studies, government policy notwithstanding, decision-making within the rural-urban fringe is primarily determined by neoliberal ideologies of economic development and ‘return on investment’. What emerges from the application of the analytical framework to the two case studies is a theory of decision-making for better outcomes at the rural-urban fringe wherein "better" means a process for achieving outcomes in line with the stated goals of policies and plans, generally framed by the idea of sustainable development. The theory asserts that effective decision-making for environmentally sustainable and socially equitable outcomes at the rural-urban fringe requires six conditions to be in place: (1) sufficient economic resources; (2) adequate knowledge; (3) forgiving time scale; (4) capable state; (5) robust legal structure; (6) favorable global context. All six are important though at this stage it cannot be said with absolute certainty whether better-for-all decisions may emerge in the absence of one or more of these conditions. This theory makes a meaningful contribution to the scholarship on the rural-urban fringe and advances knowledge by articulating a new integrated approach to better decision-making that addresses the explanatory weaknesses identified by this thesis for each of the five bodies of literature considered.

Thesis (Ph.D.)--York University, 2005. Graduate Programme in Environmental Studies. / Typescript. Includes bibliographical references (leaves 242-265). Also available on the Internet. MODE OF ACCESS via web browser by entering the following URL: http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:NR19834

Thesis (D.W.S.)--Institute for Worship Studies, 2006. / Includes bibliographical references.

Presents information on the capture of Fort Niagara on Dec. 18, 1813 during the War of 1812. Includes links to features on the War of 1812, the city of Niagara, and Niagara Falls. Also presents information on the opening of the Williamsburg Bridge on December 19, 1903. Provides links to information on the bridge, including films by James Blair Smith and Blair Blitzer on the opening of the bridge, and features on New York City. / Title from HTML header (viewed Nov. 12, 2002; last updated Dec. 2001). Illustrated by digitized items from the American Memory historic collections compiled by the National Digital Library Program of the Library of Congress.

Thesis (D.W.S.)--Institute for Worship Studies, 2006. / Abstract. Includes bibliographical references (leaves 297-304).

O Estado de São Paulo é o principal produtor de uvas de mesa do país, sendo a Niágara Rosada (Vitis Labrusca) a cultivar predominante. Para se oferecer produtos de qualidade ao mercado, os produtores necessitam determinar, periodicamente, o estado de maturação das uvas, sendo o teor de sólidos solúveis (tss), a principal variável avaliada. Para essa determinação, utilizase a amostragem dos frutos na área cultivada. O presente trabalho discute, assim, os métodos de amostragem estratificado e aleatório, e o tamanho adequado da amostra de baga individual, para avaliar o estado de maturação da uva Niágara Rosada, com base no teor de sólidos solúveis. O tamanho adequado da amostra de baga individual foi encontrado para os dois métodos de amostragem, separadamente, utilizando-se os métodos Máxima Curvatura, Máxima Curvatura Modificado e Curva da Variancia. Os métodos de amostragem foram comparados utilizando-se uma análise univariada para dados com medidas repetidas, através dos procedimentos GLM e MIXED do SAS. Foram utilizados dois procedimentos, para que se produzisse resultados confiáveis. Os tamanhos mínimos de amostra de baga individual requeridos, para os métodos estratificado e aleatório foram aproximadamente 30 e 27 bagas por área, respectivamente. Os métodos de amostragem estudados apresentaram diferença significativa, e o método aleatório apresentou grande variação máxima e mínima por planta, devendo assim, ser evitado para esse tipo de estudo. / Sao Paulo state is the main table grape producer in Brazil, being the Niágara Rosada (Vitis Labrusca) the predominant cultivar. To offer quality products to the market, the producers need to determine, periodically, the grapes maturation state, being the content of soluble solids the main variable measured. To determine this content, a sample of fruits in an area is collected. This work approaches the random and the stratified sampling methods and the appropriate sample size of individual berry to evaluate the maturation state of the Niágara Rosada based on the content of soluble solids. The appropriate sample size for individual berry was obtained for two sampling methods, separately, using the Maximum Curvature, Modified Maximum Curvature and Variance Curve methods. The sampling methods were compared using a univariate analysis for repeated measures data using the SAS GLM and MIXED procedures. Two different procedures were used to attain reliable results. The minimum berry sample size required for stratified and random methods were approximately 30 and 27 berries by area, respectively. The sampling methods investigated present significantly different results, and the random method presented high maximum and minimum variation by plant and should be avoided for this kind of study.

<p> The Paleozoic bedrock surface of southern Ontario is dissected by an interconnected system of buried bedrock valleys that are infilled with thick successions of glacial, interglacial and fluvial sediments. These valleys can be several kilometers wide, reach depths of up to 250m and the coarse-grained units are known to host significant local and regional groundwater aquifers.</p> <p> Two buried bedrock valleys located near the Niagara Escarpment in the Region of Halton were under investigation in the fall of 1999 for their potential to host additional municipal groundwater aquifers to supply drinking water to the towns of Milton and Georgetown. Detailed logging of sediment recovered from eleven continuously-cored boreholes, drilled within the Georgetown and Milton bedrock valleys, forms the basis for this study. Four distinct facies types were identified within the borehole cores including sand, gravel, fine-grained sediment and diamict (sand-rich, mud-rich and clast-rich). These four facies types were used to subdivide the cores into six stratigraphic units based on textural characteristics and stratigraphic position. These six units form a stacked succession of aquifers and aquitards within the valley infill with two stratigraphic units being identified as potential municipal aquifers.</p> <p> The Georgetown buried bedrock valley contains narrow bedrock channel interpreted to have been fluvially incised, lying within a broader flat-bottom valley likely formed by glacial scouring of the bedrock. It is feasible that regional bedrock jointing created a zone of weakness that was later exploited by a drainage network. The valley infill sediments record the approach of the Laurentide Ice Sheet into southern Ontario during the Early to Mid-Wisconsin, and the subsequent overriding of the area during the Late Wisconsin period.</p> / Thesis / Master of Science (MSc)

The past few decades have seen rapid improvement in technologies related to remote sensing, specifically in digital photogrammetry and the use of unmanned aerial vehicles (UAVs). This has presented new opportunities to collect imagery at both a high temporal and spatial resolution to create detailed digital elevation models (DEMs) and investigate small-scale geomorphological features and their development over time. The high-resolution capacity of this methodology is well-suited to the study of a variety of terrains in which many critical geomorphological features are low relief and difficult or impossible to delineate using traditional remote sensing datasets. This study utilizes UAV-based imagery collection and data analysis, in conjunction with sedimentological analysis, of two study sites in Iceland and southern Ontario. The primary objective of this work is to explore the utility of integrating high-resolution spatial surveys with more traditional field techniques to identify geomorphological features, interpret their depositional origin, and quantify temporal changes in their form. The first study was completed on the forefields of Öldufellsjökull and western Sléttjökull, two surge-type outlet glaciers of the Mýrdalsjökull Ice Cap in southeast Iceland. Glacial deposits are important sources of paleoclimatic information but not all deposits are formed by processes that reflect the overall climatic conditions of a region; surge-type (fast-flowing) glaciers undergo periodic episodes of rapid ice movement, often unrelated to ambient climatic conditions. Remotely sensed data and field investigations were combined to complete a landsystem analysis of the forefields at each of Öldufellsjökull and western Sléttjökull, and an unmanned aerial vehicle (UAV) was used to collect high-resolution imagery of areas of particular interest. The forefields of Öldufellsjökull and western Sléttjökull, lack many of the characteristics typical of surge-type landsystems and instead are more similar to the active temperate landsystem common in Iceland. The identification of landforms considered to be diagnostic of surge-type glacier behaviour was only possible through a targeted high-resolution UAV survey suggesting that small-scale diagnostic landforms may be overlooked in many investigations. The second study area focused on the Niagara Escarpment in Hamilton, Ontario, a major landform resulting from extensive glacial and fluvial erosion of Paleozoic sedimentary rocks during the late Quaternary. In Hamilton, the Niagara Escarpment is a steep faced cuesta composed of Ordovician and Silurian sedimentary rocks. Recent rockfalls onto roads crossing the escarpment have raised serious concerns about its stability. To address these concerns, and to provide more information on erosional processes active along the escarpment in Hamilton, a comprehensive study of the Niagara Escarpment was completed including the collection of multi-temporal photogrammetric surveys of select rock faces, and detailed sedimentological and fracture analysis. A comprehensive lithological investigation was completed of all accessible rock outcrops in Hamilton to identify areas most likely to experience erosion based on site characteristics. A second component of this investigation was to evaluate the utility of using high-resolution imagery combined with Structure from Motion (SfM) software to detect temporal changes on the escarpment face. A staged erosion study was conducted in which lithological blocks of a known size were removed from the escarpment face at a selected site, to determine the lower limits of detection of erosion using this methodology. The study found that the location of block removal (erosion) was consistently identified, but the calculated volume of blocks removed was less accurately determined, differing by an average of 175% from the known volume of the block. A further study using this same methodology tested its ability to identify areas of natural loss (erosion) from the escarpment face. Based on multiple surveys taken 14 months apart at a selected study site, approximately one third of the area of interest experienced either loss (erosion) or gain (deposition) of material. There appear to be clear connections between lithology, density of fracturing, and the location of material loss (erosion); areas of the outcrop characterised by interbedded shales, and those areas exposing densely fractured sandstone or dolostone, were most likely to erode. The lithological characteristics of the Niagara Escarpment, including the strength of individual stratigraphic units, their vertical arrangement, and their density of fracturing, as well as climatic and hydrological factors (e.g., groundwater flow, location of surficial water features, mean annual temperature, mean annual precipitation etc.), all contribute to the amount and types of erosion active on the exposed rock face. The studies reported in this thesis have integrated high-resolution, close-range imagery with traditional field techniques to explore the characteristics and development of geomorphological forms in different terrain types. In each of the studies, the importance of collecting high-resolution imagery (<10 cm) to map geomorphological features of various scales is highlighted. / Dissertation / Doctor of Science (PhD)

<p>This study explores the history of Niagara settlement and settlers through the changing patterns of burial and commemoration visible in historical family cemeteries established following Euro-American settlement in the 1790s. Data collected from a combination of site survey and archival research demonstrate three clear phases of: 1) early cemetery creation and use 2) the transition to burial in public cemeteries throughout the late 1800s; and 3) the closure of family cemeteries by the early 1900s followed by periods of neglect and renewal characterized by inactive cemeteries being repurposed by descendants as sites of heritage display.</p> <p>There is incredible variation in burial data and the overall patterns speak to changing identity relating to family, land, community, memory, and history. More specifically, the results of this study demonstrate a shift from an identity created through the experience of family place and burial to a community-based identity that emphasizes the nuclear family and their history within their wider social network. More recent heritage displays have explicitly introduced a narrative of settlement, Loyalist identity, and land ownership that was inherent when cemeteries were in use.</p> <p>This cemetery-based history approach demonstrates the potential of mortuary material culture to address questions of social change within the historical context in which it was created and used. It also highlights the value of variability in cemetery data and the consideration of the circumstances of cemetery creation, use, neglect, and renewal to inform the range of personal and collective histories that are visible over generations.</p> / Doctor of Philosophy (PhD)