An investigation of permafrost (permanently frozen soil) was conducted in Canada’s subarctic region of Northern Ontario. Environmental baseline conditions and permafrost states were estimated using seasonal freezing and thawing energies based on observed climate data and the Stefan equation. Field studies provided measurements of the active layer depths and validated the permafrost states; laboratory studies of the soil samples provided characterization for organic materials that have high affinity for soil moisture. Palsas (unique dome-like formations) were observed to have enhanced permafrost cores beneath a thermal insulating organic layer. With climate change, results suggest the possibility of shifts from the classification of continuous to discontinuous permafrost states in areas lacking the presence of organic materials that can have environmental and ecological impacts. Northern infrastructures may become destabilized with the degradation of permafrost while palsas may become lone permafrost refuges for biodiversity that depend on cooler ecosystems, such as polar bears.

In the James Bay Lowlands of northern Ontario, kimberlite pipes are concealed by peat, thick layers of till, and Tyrell sea sediments. Studies have shown that buried ore bodies produce geochemical signatures in surface media. This thesis explores the geochemistry of near-surface groundwater above concealed kimberlite pipes using factor analysis to determine whether (1) a factor analysis can reveal an underlying structure (factors) in a multivariate groundwater geochemical dataset, and whether (2) those factors are related to the presence of concealed kimberlite. Factor analysis was performed on two datasets of nearsurface groundwater, collected at 0.2 m and 1.1 m below ground surface in peat. Results revealed that (1) there is a significant difference in the behaviour of elements in groundwater near the surface compared to those in deeper groundwater, which is sheltered from the effects of the atmosphere; (2) for both datasets, the first factor is dominated by elements known to be enriched in kimberlite, notably rare earth elements (REE), U, Th, Ti – the composition of factor one is consistent with their derivation from kimberlite in a limestone background where such elements are in very low concentration; (3) high-valence and lowvalence kimberlite indicator elements (KIE) are found separated into distinct factors suggesting that once released from the kimberlite after weathering, KIE are subjected to various geochemical processes to be differentiated as they migrate upward to the surface; and (4) Fe and Mn load on a factor distinct from other metals, suggesting that in this environment Fe-Mn-O-OH is not a significant controller of metal mobility in groundwater. Overall, this research has further highlighted the multivariate nature of geochemical processes in groundwater. Compared with previous work in geochemical exploration where often only univariate or bivariate statistics or single element profiles over concealed ore bodies were used, this thesis has shown that factor analysis, as a multivariate data analysis technique, is a robust exploration tool, able to shed light on relevant geochemical processes hidden within geochemical datasets. This thesis shows that high-valence KIE, notably U,V, Th, Ti and the REE, as a group, are better indicators of the presence of kimberlites than other well-known KIE. Single element concentration profiles such as Ni or Cr (known KIE) show similar anomalies over a concealed kimberlite as a factor score profile for factor one (U, V, Th, Ti, REE, Ni) would; however, it is the peculiar assemblage of elements in factor one that makes it unique to kimberlites, a feature that can be used in future exploration work for concealed kimberlites in similar surficial environments, such as the Siberian wetlands. The results suggest that future geochemical exploration work involving groundwater should focus on the more stable groundwater located below the zone of oxidation, sheltered from the effects of the atmosphere.

In the James Bay Lowlands of northern Ontario, kimberlite pipes are concealed by peat, thick layers of till, and Tyrell sea sediments. Studies have shown that buried ore bodies produce geochemical signatures in surface media. This thesis explores the geochemistry of near-surface groundwater above concealed kimberlite pipes using factor analysis to determine whether (1) a factor analysis can reveal an underlying structure (factors) in a multivariate groundwater geochemical dataset, and whether (2) those factors are related to the presence of concealed kimberlite. Factor analysis was performed on two datasets of nearsurface groundwater, collected at 0.2 m and 1.1 m below ground surface in peat. Results revealed that (1) there is a significant difference in the behaviour of elements in groundwater near the surface compared to those in deeper groundwater, which is sheltered from the effects of the atmosphere; (2) for both datasets, the first factor is dominated by elements known to be enriched in kimberlite, notably rare earth elements (REE), U, Th, Ti – the composition of factor one is consistent with their derivation from kimberlite in a limestone background where such elements are in very low concentration; (3) high-valence and lowvalence kimberlite indicator elements (KIE) are found separated into distinct factors suggesting that once released from the kimberlite after weathering, KIE are subjected to various geochemical processes to be differentiated as they migrate upward to the surface; and (4) Fe and Mn load on a factor distinct from other metals, suggesting that in this environment Fe-Mn-O-OH is not a significant controller of metal mobility in groundwater. Overall, this research has further highlighted the multivariate nature of geochemical processes in groundwater. Compared with previous work in geochemical exploration where often only univariate or bivariate statistics or single element profiles over concealed ore bodies were used, this thesis has shown that factor analysis, as a multivariate data analysis technique, is a robust exploration tool, able to shed light on relevant geochemical processes hidden within geochemical datasets. This thesis shows that high-valence KIE, notably U,V, Th, Ti and the REE, as a group, are better indicators of the presence of kimberlites than other well-known KIE. Single element concentration profiles such as Ni or Cr (known KIE) show similar anomalies over a concealed kimberlite as a factor score profile for factor one (U, V, Th, Ti, REE, Ni) would; however, it is the peculiar assemblage of elements in factor one that makes it unique to kimberlites, a feature that can be used in future exploration work for concealed kimberlites in similar surficial environments, such as the Siberian wetlands. The results suggest that future geochemical exploration work involving groundwater should focus on the more stable groundwater located below the zone of oxidation, sheltered from the effects of the atmosphere.

First Nations people have experienced dramatic life changes in a very short period of time. The process of change was not a conscious decision made by First Nations peoples but rather the result of successive stages of European contact and formal colonization by what is now the government of Canada. With such constant changes and the history of assimilation that overshadows the Aboriginal population, it is becoming difficult for Elders to sustain their roles within the family unit and in their community as a whole. This study provides a description of the oral accounts of Elders living in two remote First Nations communities in Northwestern Ontario. I conducted three summers of ethnographic research that involved participant observation of local cultural practices and 12 semi-structured interviews from 2009 to 2011. Guided discussions with Elders about their lives and their relationship to the land provide important insight into local cultural and personal values. Three primary themes emerged from the conversations with the Elders about life during the childhood: the intense physicality of life in the past, the connection between health and local foods and the changing role of Elders. Findings suggest that Elders are eager to transmit their knowledge to provide a healthier lifestyle for future generations. In addition, I provide a description of the current living conditions of Elders in both communities. First Nations Elders, who were once crucial to the survival of a band, are now facing the highest degree of vulnerability and are desperately searching for a new identity that gives them purpose. Meeting with Elders in their homes and at several community events provided insight into their lives and the challenges they are currently facing. These challenges and experiences are hardly one-dimensional, as they each have varying degrees of family support, financial stability and housing conditions. However, the consistent thread in all the cases was the ongoing struggle Elders have faced trying to reconcile traditional perspectives with the growing dominance of contemporary western lifestyle practices.

<p>The Long Rapids Formation in the Moose River Basin of northern Ontario is Upper Devonian in age and can be correlated with similar shale deposits in the Michigan, Appalachian, and Illinois Basins . The southern Ontario equivalent to the Long Rapids Formation is the Kettle Point Formation. </p> <p> The Long Rapids Formation is a marine black shale deposited predominantly under depleted oxygen conditions. Large amounts of marine organic matter from the water column and from terrestrial sources accumulated in reducing bottom waters with little recycling to produce brown to black, organic-rich sediments . The depositional basin was stratified, and anoxic bottom waters and oxic surface waters were separated by a pycnocline. The position of the pycnocline (or the absence of it) dictated the type of sediment deposited, and the relative depth of the pycnocline to the sediment-water interface was more important than the absolute depth of the water column. The Moose River Basin in Late Devonian times was located on the Laurasian Continent in an area experiencing tropical conditions and was affected by a period of transgression following the Acadian Orogeny. The black shales in the Long Rapids Formation represent a period of transgression of the large epicontinental Catskill Sea, whereas the green-grey mudstones and carbonates represent periods of minor eustatic changes. </p> <p> Dark-coloured facies with abundant bioturbation are overlain by lighter-coloured facies. Bioturbation is variable in the less abundant green-grey mudstone and carbonate facies, and were also low in organic matter. The ichnofauna suite Chondrites-Planolites-Zoophycos-Alcyonidiopsis-(?Teichichnus) represents an oxygen-minimum ichnofacies found predominantly in dark shale facies. As more oxygen was introduced to the sediment-water interface, more permanent burrow structures were constructed such as Teichichnus, Terebellina, ?Cylindrichnus, Skolithos, and Ichnogenus "A" in the green-grey mudstones and carbonates. As well, body fossils were more commonly found in those facies. The Leiorhynchus brachiopod fauna in the dark-coloured shales probably represents a sparse epifauna living in poorly oxygenated or temporarily oxic conditions in a basinal or open-shelf environment. </p> / Thesis / Master of Science (MSc)

What happens after a place has been exploited, isolated, and neglected? What occurs when that place is bound – confined – by impenetrable voids of dereliction? Its core, slowing diffracting, with no opportunity to perceive outward – beyond the derelict terrain to the boundless expanses of earth and water that have perpetuated its vitality. And what then, if for a moment, this decaying place is given a view beyond these boundaries? Deindustrialization has invariably altered modern cultural conceptions of control over nature. The terrain remaining after decades of resource exploitation is composed of deep voids and fissures that reside physically, psychologically, and theoretically in-between the accepted realms of culture and nature. This thesis explores the perversion and dissolution of these two opposing realms within the sublime and fantastical derelict landscape of a declining town. Deindustrial voids are considered as both barrier and bridge; serving as persistent symbolic reminders of the volatile and hubristic relationship between culture and nature, and offering potential reconnection to the natural landscape of a city’s foundation. Reacting to collective nostalgia through memorialisation, totemism, and erasure, typical design interventions continue to prioritize cultural domination and emphasize the designer as creator in order to reassert control over the chaos of deindustrialization, often resulting in placeless infilling of the void. Ideas of extimacy, alterity, and ruination, with influences from the fields of industrial archaeology and landscape architecture, ground contemporary reactions to the deindustrial void and explore the role of landscape in the creation and fragmentation of ideas of place for the dissolving North American industrial city. Both inspired and situated within the declining former town of Fort William, Ontario, this thesis surveys an abandoned industrial corridor that encircles the town, severing it from the liminal water’s edge and landscape beyond. Viewed as a palimpsest, this site is considered beyond its most recent industrial usage to expose a place-specific natural/cultural terrain comprised of material and immaterial layers of evolution and exploitation. This thesis positions the architect as perceiver, hoping to inspire sensitivity, pause, and reflection and resists ideas of forced transformation as a means of outwardly expressing progress. It immerses itself within the in-between places that blur preconceived boundaries – natural and cultural, past and future, controlled and chaotic – in order to encounter the inherent existential qualities of a site in transition.

What happens after a place has been exploited, isolated, and neglected? What occurs when that place is bound – confined – by impenetrable voids of dereliction? Its core, slowing diffracting, with no opportunity to perceive outward – beyond the derelict terrain to the boundless expanses of earth and water that have perpetuated its vitality. And what then, if for a moment, this decaying place is given a view beyond these boundaries? Deindustrialization has invariably altered modern cultural conceptions of control over nature. The terrain remaining after decades of resource exploitation is composed of deep voids and fissures that reside physically, psychologically, and theoretically in-between the accepted realms of culture and nature. This thesis explores the perversion and dissolution of these two opposing realms within the sublime and fantastical derelict landscape of a declining town. Deindustrial voids are considered as both barrier and bridge; serving as persistent symbolic reminders of the volatile and hubristic relationship between culture and nature, and offering potential reconnection to the natural landscape of a city’s foundation. Reacting to collective nostalgia through memorialisation, totemism, and erasure, typical design interventions continue to prioritize cultural domination and emphasize the designer as creator in order to reassert control over the chaos of deindustrialization, often resulting in placeless infilling of the void. Ideas of extimacy, alterity, and ruination, with influences from the fields of industrial archaeology and landscape architecture, ground contemporary reactions to the deindustrial void and explore the role of landscape in the creation and fragmentation of ideas of place for the dissolving North American industrial city. Both inspired and situated within the declining former town of Fort William, Ontario, this thesis surveys an abandoned industrial corridor that encircles the town, severing it from the liminal water’s edge and landscape beyond. Viewed as a palimpsest, this site is considered beyond its most recent industrial usage to expose a place-specific natural/cultural terrain comprised of material and immaterial layers of evolution and exploitation. This thesis positions the architect as perceiver, hoping to inspire sensitivity, pause, and reflection and resists ideas of forced transformation as a means of outwardly expressing progress. It immerses itself within the in-between places that blur preconceived boundaries – natural and cultural, past and future, controlled and chaotic – in order to encounter the inherent existential qualities of a site in transition.

This study examines intricately related questions of consciousness and learning, textually-mediated social coordination, and human relationships within nature, anchored in the everyday life practices and concerns of a remote First Nation community in the Treaty 9 region. Through the use of Institutional Ethnography, community-based research and narrative methods, the research traces how the ruling relations of land use planning unfold within the contemporary period of neoliberal development in Northern Ontario. People’s everyday experiences and access to land in the Mushkego Inninowuk (Swampy Cree) community of Fort Albany for example, are shaped in ways that become oriented to provincial ruling relations, while people also reorient these relations on their own terms through the activities of a community research project and through historically advanced Indigenous ways of being. The study examines the coordinating effects of provincially-driven land use planning on communities and territories in Treaty 9, as people in local sites are coordinated to others elsewhere in a complex process that serves to produce the legislative process called Bill 191 or the Far North Act. Examining texts, ideology and dialectical historical materialist relations, the study is an involved inquiry into the text process itself and how it comes to be put together. The textually mediated and institutional forms of organizing social relations—effectively land relations—unfold with the involvement of people from specific sites and social locations whose work is coordinated, as it centres on environmental protection and development in the region north of the 51st parallel. A critique of the textually mediated institutional process provides a rich site for exploring learning within the context of neoliberal capitalist relations and serves to illuminate ways in which people can better act to change the problematic relations that haunt settler-Indigenous history in the contemporary period. The work asks all people involved in the North how we can work to address historic injustices rooted in the relations and practices of accumulation and dispossession. The voices and modes of governance of Aboriginal people, obfuscated within the processes and relations of provincial planning, must be afforded the space and recognition to flourish on their own terms.

This study examines intricately related questions of consciousness and learning, textually-mediated social coordination, and human relationships within nature, anchored in the everyday life practices and concerns of a remote First Nation community in the Treaty 9 region. Through the use of Institutional Ethnography, community-based research and narrative methods, the research traces how the ruling relations of land use planning unfold within the contemporary period of neoliberal development in Northern Ontario. People’s everyday experiences and access to land in the Mushkego Inninowuk (Swampy Cree) community of Fort Albany for example, are shaped in ways that become oriented to provincial ruling relations, while people also reorient these relations on their own terms through the activities of a community research project and through historically advanced Indigenous ways of being. The study examines the coordinating effects of provincially-driven land use planning on communities and territories in Treaty 9, as people in local sites are coordinated to others elsewhere in a complex process that serves to produce the legislative process called Bill 191 or the Far North Act. Examining texts, ideology and dialectical historical materialist relations, the study is an involved inquiry into the text process itself and how it comes to be put together. The textually mediated and institutional forms of organizing social relations—effectively land relations—unfold with the involvement of people from specific sites and social locations whose work is coordinated, as it centres on environmental protection and development in the region north of the 51st parallel. A critique of the textually mediated institutional process provides a rich site for exploring learning within the context of neoliberal capitalist relations and serves to illuminate ways in which people can better act to change the problematic relations that haunt settler-Indigenous history in the contemporary period. The work asks all people involved in the North how we can work to address historic injustices rooted in the relations and practices of accumulation and dispossession. The voices and modes of governance of Aboriginal people, obfuscated within the processes and relations of provincial planning, must be afforded the space and recognition to flourish on their own terms.