Academic literature on the topic 'Church of England in Nova Scotia'

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Journal articles on the topic "Church of England in Nova Scotia"

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Doll, Peter M. "American High Churchmanship and the Establishment of the First Colonial Episcopate in the Church of England: Nova Scotia, 1787." Journal of Ecclesiastical History 43, no. 1 (January 1992): 35–59. http://dx.doi.org/10.1017/s0022046900009659.

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The creation in North America of the first overseas diocese of the Church of England was undoubtedly one of the most remarkable and unlikely of the changes in British colonial policy which resulted from the American Revolution. Before the war, the Anglican campaign for the appointment of colonial bishops had been a major reason for the colonial fear of British tyranny; many Americans, particularly Nonconformists, vigorously protested against a scheme which they saw as a bid to recreate a Laudian ecclesiastical tyranny. But the post-war colonial policy envisaged the colonial bishop as a focus of political stability and loyalty. The new prestige and political responsibility accorded by the government to the Church was equally remarkable in view of the government's Erastian suppression of Convocation since 1715 and its politic responsiveness to Dissenting sensibilities. Despite occasional outbreaks of clerical frustration at the Church's inability to act independently, the Church of England had been unable to escape this political domination. This paper will attempt to explain why, given the government's prior hostility to the design, ministries in the 1780s should have decided to extend the church hierarchy to the colonies.
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Poulin, Naythan R. "“Laws that make them slaves there, make them slaves here:” The Status of Slavery in England and its influence on the colony of Nova Scotia." General: Brock University Undergraduate Journal of History 4 (May 6, 2019): 84–95. http://dx.doi.org/10.26522/tg.v4i0.2127.

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Nova Scotia was the only colony in the transatlantic world to possess no statute laws or slave codes; thus, Nova Scotia did not have legal authorization to enforce slavery. The absence of statute law in Nova Scotia engendered significant legal ambiguities on the general status of slavery in the colony. Following 1783, Nova Scotia’s legislative and judicial institutions were greatly destabilized by Loyalist migration, and the colony searched across the transatlantic world for legal answers. England, similarly to Nova Scotia, did not possess any statute laws to enforce slavery; the metropole and the colony of Nova Scotia thus shared a similar ambiguity towards the status and regulation of slavery. Therefore, evidence suggests that judicial rulings made in Nova Scotia regarding the status of slavery were directly influenced by common law established in England. Specifically, Somerset v Stewart and subsequent cases in England legitimized and influenced Chief Justice Blowers and Strange to impose a judicial war of attrition against slavery in Nova Scotia. Although Nova Scotia’s legal system had become effective in eradicating slavery, the system did not always provide permanent freedom, and in many cases freed black men and women risked kidnapping and re-enslavement. Ultimately, slavery in the Canadian colonies is a topic that has been erased from the historiographical narrative and has been ignored by generations of historians. Nonetheless, it signifies that more work is required to establish stronger connections between the metropole and Canadian colonies, but also, the intercolonial and transatlantic influences on slavery.
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Yorke, Alana F., Stephen Mockford, and Rodger C. Evans. "Canada frostweed (Helianthemum canadense (L.) Michx.; Cistaceae) at the northeastern limit of its range: implications for conservation." Botany 89, no. 2 (February 2011): 83–89. http://dx.doi.org/10.1139/b10-088.

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Canada frostweed (Helianthemum canadense) is a perennial herb whose abundance and habitat are declining in Nova Scotia. These sites mark the northeastern limit of this species with nearest populations occurring in Maine and Quebec. To determine the genetic structure of northeastern populations, we used amplified fragment length polymorphisms to examine individuals from Nova Scotia, Maine, New Hampshire, and Quebec. Cluster analyses and analysis of molecular variance identified four groups: (i) Queens County, Nova Scotia; (ii) Kings County, Nova Scotia; (iii) Quebec; and (iv) Northeastern New England. New England samples revealed evidence of gene flow among populations within that region, and several individuals from Quebec and Queens County, Nova Scotia, were assigned to the same cluster. The majority of individuals from Kings County were assigned to a separate cluster from that associated with Queens County, indicating two distinct populations within Nova Scotia. Differences between Nova Scotia populations may be attributed to isolation and drift, or separate postglacial colonization events. We recommend that Queens County and Kings County populations be considered as discrete units for conservation and, because Nova Scotia populations are distinct from other populations in eastern Canada and northeastern United States, we suggest that conservation of populations at the northeastern limits of the range of H. canadense is warranted.
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Apostle, Richard, Leonard Kasdan, and Arthur Hanson. "Work Satisfaction and Community Attachment among Fishermen in Southwest Nova Scotia." Canadian Journal of Fisheries and Aquatic Sciences 42, no. 2 (February 1, 1985): 256–67. http://dx.doi.org/10.1139/f85-033.

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Social scientists have examined the problem of attachment to the New England fisheries in terms of two interacting influences: work satisfaction, based on questionnaire interviews, and attachment to kin and community, based on ethnographic field research. There is a paucity of equivalent information for the Maritimes. This study replicates the New England work satisfaction studies, and includes additional questions concerning community attachment. We demonstrate that fishermen in southwest Nova Scotia are, in contrast with their New England counterparts, satisfied with all questions about their work (save for the common dissatisfaction with government officials found in both the Nova Scotia and New England samples). In particular, although offshore fishermen in southwest Nova Scotia tend to be somewhat less satisfied than those who fish inshore or both inshore and offshore, they have, by comparison with the New Bedford fishermen, scores that are over the "neutral value" on all time and adventure questions. The underlying factors of job satisfaction are comparable with those in the New England studies, except that the factors in our data are more numerous and simpler to interpret. High job satisfaction is combined with strong community attachments in southwest Nova Scotia.
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Green, David G. "Pollen evidence for the postglacial origins of Nova Scotia's forests." Canadian Journal of Botany 65, no. 6 (June 1, 1987): 1163–79. http://dx.doi.org/10.1139/b87-163.

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Pollen diagrams from sites in southwest Nova Scotia and close to the New Brunswick – Nova Scotia border show that after retreat of the Wisconsin ice sheets, most tree taxa arrived in the extreme southwest of Nova Scotia earlier than anywhere else in the province. For most tree taxa, arrival times at sites in maritime Canada and in northeastern New England are consistent with very early dispersal of individuals along the coastal strip via the exposed coastal shelf and with their entering Nova Scotia from the southwest. These scattered pioneer populations acted as centres for major population expansions, which followed much later in some cases. Local environments, fire, and interspecies competition appear to have been more important than propagule dispersal rates as factors limiting the spread of most taxa.
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Gledhill, Dwight, Meredith White, Joe Salisbury, Helmuth Thomas, Ivy Misna, Matthew Liebman, Bill Mook, et al. "Ocean and Coastal Acidification off New England and Nova Scotia." Oceanography 25, no. 2 (June 1, 2015): 182–97. http://dx.doi.org/10.5670/oceanog.2015.41.

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MAJKA, CHRISTOPHER G., and DAVID B. MCCORQUODALE. "The Coccinellidae (Coleoptera) of the Maritime Provinces of Canada: new records, biogeographic notes, and conservation concerns." Zootaxa 1154, no. 1 (March 20, 2006): 49. http://dx.doi.org/10.11646/zootaxa.1154.1.5.

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New records of Coccinellidae in the Maritime Provinces of Canada are reported. The known fauna of the region consists of 47 species: 41 in Nova Scotia, 39 in New Brunswick, and 21 in Prince Edward Island. Of these, records are provided for 13 species newly recorded from Nova Scotia and 14 from Prince Edward Island. Two species, Diomus amabilis (LeConte) and Naemia seriata seriata Melsheimer, are newly recorded in Canada. Didion punctatum (Melsheimer) is removed from the fauna of PEI, and Coccidula lepida LeConte is removed from the fauna of NS, and Scymnus impexus Mulsant is removed from the faunas of NS and NB. Records of two adventive species not established in the region are also reported. Collecting effort in the three provinces and their sub-regions is briefly analyzed and compared. Biogeographic observations are provided in relation to the composition of the fauna as a whole, and of disjunct populations of six Nova Scotia coccinellids, several of which appear to be members of a coastal plain fauna that extends from New England to southern Nova Scotia. The potential vulnerability of the coccinellid fauna is discussed in the context of both adventive species in the region, and habitat loss and conservation.
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MAJKA, CHRISTOPHER G., YVES BOUSQUET, and SUSAN WESTBY. "The ground beetles (Coleoptera: Carabidae) of the Maritime Provinces of Canada: review of collecting, new records, and observations on composition, zoogeography, and historical origins." Zootaxa 1590, no. 1 (September 21, 2007): 1–36. http://dx.doi.org/10.11646/zootaxa.1590.1.1.

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The Carabidae of Nova Scotia and New Brunswick are surveyed. The collecting history of the family in the region is reviewed. New records of 20 species are reported, 6 from New Brunswick and 15 from Nova Scotia. Six species are newly recorded in the Maritime Provinces (New Brunswick, Nova Scotia, and Prince Edward Island) as a whole. Six species are removed from the faunal list of Nova Scotia and one from the faunal list of New Brunswick. Consequently, 282 species of Carabidae are now known from Nova Scotia, 273 species from New Brunswick, and 329 from the Maritime Provinces as a whole. A new and earlier timeline (1942) is reported for the introduced Palearctic carabid, Bembidion properans (Stephens), in North America. The status of Stenolophus carbo Bousquet in the region is reviewed and its presence in Nova Scotia is considered doubtful. The historical origins of the Maritime fauna are discussed based on studies of post-glacial Coleoptera. These indicate at least three colonization phases, some elements of which are still apparent in the contemporary fauna. Elements of the native Nova Scotia fauna not found in New Brunswick (26 species), may represent colonization from New England across post-glacial land bridges and island chains. Elements of the native fauna found in New Brunswick and not Nova Scotia (31 species), may represent species that have reached the eastward limit of their distribution for climatic or environmental reasons; or that have found the Northumberland Strait and/or the isthmus of Chignecto an obstacle to geographical dispersal; or represent widely distributed boreal species (6 species) that should be sought in Nova Scotia. Eighteen species of Nova Scotia carabids have been recorded only from Cape Breton Island, two of which are known in Atlantic Canada solely from there. Although Cape Breton is separated from the mainland by the 1.5 km wide Strait of Canso, the number of flightless, native carabids present is proportionally greater than that in Nova Scotia overall, or the Maritime Provinces as a whole. Despite differences in land mass and distance to the neighbouring mainland, the faunas of Cape Breton, Prince Edward Island, and insular Newfoundland, exhibit similarities in size and composition, although Newfoundland's fauna has twice the proportion of Holarctic species. Cape Breton's carabid fauna is diminished compared to the neighbouring mainland, having only 57% of the native species. This may represent an island-associated diminution, the paucity of collecting, or a combination of both, although in comparison with other groups of Coleoptera the Carabidae appear relatively well represented. Within Atlantic Canada, New Brunswick has the lowest proportion (8.8%) of introduced carabids and the highest proportion (83.2%) of native, Nearctic species. Given the potential utility of carabids as bioindicators, and the wide range of disturbance to which the environment of the Maritime Provinces has been subjected, further research on this diverse group of beetles would be desirable.
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Zentilli, M., and P. H. Reynolds. "40Ar/39Ar dating of micas from the East Kemptville tin deposit, Yarmouth County, Nova Scotia." Canadian Journal of Earth Sciences 22, no. 10 (October 1, 1985): 1546–48. http://dx.doi.org/10.1139/e85-161.

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The East Kemptville tin deposit in Nova Scotia, the largest known tin deposit in North America, lies in a greisen zone within the Davis Lake Pluton, generally considered to be part of the Devonian South Mountain Batholith. Our dating of micas from within the deposit suggests that the greisenization process that accompanied mineralization took place about 295 ± 5 Ma ago, that is, ca. 60 Ma after the emplacement of the batholith.Hydrothermal alteration–mineralization activity in southern Nova Scotia coincided with extensive shearing and tectonism throughout the Hercynian orogen. The East Kemptville deposit appears to be approximately coeval with similar mineralization in southwest England, the Iberian peninsula, and northwest Africa and much younger than the Devonian Acadian orogeny.
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McAleer, J. Philip. "The Chancel of St. Paul’s Anglican Church, Halifax, Nova Scotia: Form Follows Convenience?" RACAR : Revue d'art canadienne 17, no. 1 (1990): 46. http://dx.doi.org/10.7202/1073155ar.

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Dissertations / Theses on the topic "Church of England in Nova Scotia"

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Craigie, Allan. "Regional and national identity mobilization in Canada and Britain : Nova Scotia and North East England compared." Thesis, University of Edinburgh, 2010. http://hdl.handle.net/1842/4482.

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Examining Canada and Britain from 1990 to 2004, the thesis explores how the surge in minority nationalist agitation that occurred in Quebec and Scotland changed the political environment in Canada (outside Quebec) and England allowing regional elites to advance political agendas which mobilized regional and national identities. The thesis considers the role of democratic institutions at the regional level in shaping political demands through a comparative study of regional and national identity mobilization in Nova Scotia and the North East of England. The analysis contends that the relationship between minority and majority nations is dialectical; nationalism stems from fundamentally different interpretations of the state and is not the ‘fault’ of either nation. Using this claim as the basis for analyzing elite debate at the centre and in the regions, the dissertation systematically examines regionalism within the majority nation by investigating debates at the national and regional level. The work looks at parliamentary debates, campaign material, newspaper accounts and elite interviews; and as identity mobilization and political debates are targeted at the electorate, survey analysis is undertaken to see whether elite debate resonated with the masses. The thesis demonstrates that regionalism is a component of the ongoing (re)conception of nation within the majority nation, and that during periods of strong minority nationalist agitation, a political environment is created which allows elites in the majority nation to mobilize national and regional identities. Regional identity mobilization is shown to be part of the nationalism of the majority nation; as the dominant conception of the state within the majority encompasses the minority nations as co-nationals and equal citizens, regional elites are able to use the minority nations as examples of successful agitation without subscribing to their interpretations of the state. Regional levels of democracy did not alter the nature of regionalism in either state and though the demands issued may have been different, the underlying concerns were the same: a lack of voice and efficacy.
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Whalen, William Taylor. "Geochemistry of mafic dikes from the Coastal New England magmatic province in southeast Maine, USA and Nova Scotia, Canada." Thesis, Virginia Tech, 2019. http://hdl.handle.net/10919/90395.

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Mid-Late Triassic-age alkali-basalt dikes were emplaced along the coast of New England between 240-200 Ma. Known as the Coastal New England (CNE) magmatic province, this dike swarm is the immediate magmatic predecessor to the formation of the Central Atlantic Magmatic Province large igneous province at 201 Ma and the breakup of Pangea. The intent of this study is to determine the melt source and mechanisms for melting which produced the Triassic coastal dikes. To achieve this goal, major and trace element compositions were analyzed for 53 CNE dikes from Maine and Nova Scotia. Radiogenic Nd-Sr-Pb-Hf ratios, representing some of the first 176Hf/177Hf data for CNE, are reported for 12 of the dikes. Taken together, the compositional data implicate melting of a deep mantle source that is relatively enriched in incompatible elements, such as a mantle-plume similar to those hypothesized as the source of melting in modern ocean-island basalts (i.e. Hawaii). Dike compositions are inconsistent with melts generated at typical spreading-center ridges (i.e. MORB). Modeling suggests that CNE melts ascended through thick continental crust, consistent with the incipient stages of rifting of Pangea, as evidenced by a heterogeneous mix of melting and crystallization depths, between 0-70km, with no clear geographic pattern. Radiogenic isotope data are relatively consistent and represent a mixture between HIMU, EMI and DMM mantle reservoirs, implying component consisting of relict subducted oceanic crust (or other similarly evolved material). CNE magmatism may have contributed to the breakup of Pangea by destabilizing the lower crust in the limited local area where it erupted, but its true relationship with the breakup of Pangea and later CAMP event requires more study.
Master of Science
Approximately 200-250 million years ago, hundreds of sheets of lava, called dikes, erupted along what is today the coast of New England. As these volcanic dikes rose up from the Earth’s mantle, they traveled along cracks and weak areas of the Earth’s crust. Today, these dikes are found along the New England coast as far south as Rhode Island and as far north as Nova Scotia, Canada. Based on the similarity of their geochemistry and petrology, as well as their geologic age and geography of their eruption, geologists group these dikes and similar volcanics together as a single, related magmatic event. This magmatic event produced the Coastal New England (CNE) magmatic province. 250 million years ago, the coast of New England was actually an interior part of the supercontinent known as Pangea. Around 250 m.yr. ago, Pangea slowly began rifting apart, which is when CNE volcanism began. By 200 m.yr. ago, Pangea had broken up, and CNE volcanism had ended. Further complicating the story, a large-igneous province (LIP) also erupted 200 m.yr. ago. Known as the Central Atlantic Magmatic Province (CAMP), this volcanism consisted of enormous volumes of lava that flooded over the entire east coast of the United States. The intent of this study is to determine what geological conditions led to the CNE volcanism. By learning which part of the Earth melted and why, CNE volcanism’s role in the breakup of Pangea, and the much larger CAMP eruptions that coincided with it, will become clearer. For instance, did the geologic events that resulted in CNE volcanism contribute to the breakup of Pangea, or did the breakup of Pangea cause CNE volcanism followed by CAMP volcanism? To achieve this goal, the geochemical compositions of 53 CNE dikes from Maine and Nova Scotia were analyzed. Radiogenic Nd-Sr-Pb-Hf ratios for a subset of the dikes (12) were also analyzed. This study presents some of the first radiogenic hafnium data for rocks from CNE. The data indicate that the melting which produced the CNE dikes began in the deep mantle, similar to the melting of mantle plumes beneath modern ocean-islands such as Hawaii. In contrast, shallow mantle melting, like the melting at mid-ocean ridges where oceanic crust is produced, is not consistent with the geochemical evidence presented for CNE in this study. Modeling suggests that CNE magmas rose through thick continental crust, which caused them to begin forming crystals at relatively high depths. Radiogenic isotope data suggests that part of the mantle that melted was old, recycled oceanic crust or similar mantle material. CNE magmatism may have contributed to the breakup of Pangea by destabilizing the lower crust in the limited local area where it erupted, but its true relationship with the breakup of Pangea and later CAMP event requires more study.
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Montgomery, Alexandra Lunn. "An Unsettled Plantation: Nova Scotia’s New Englanders and the Creation of a British Colony, 1759-1776." 2012. http://hdl.handle.net/10222/15230.

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The New England Planters were the largest wave of Protestant migration into Nova Scotia prior to the American Revolution. Sponsored by the British government, they represent an attempt to make Nova Scotia a securely British colony in the wake of the Seven Years’ War and the Acadian deportation. Examining the experiences of several families, this thesis argues that the Planters, despite taking up lands in Nova Scotia, remained unsettled. The migration was staggered over a number of years, and Planters maintained close ties with New England. However, the Planters were unable to recreate New England culture completely. Increasing numbers of settlers from the British Isles and revolutionary suspicion marked out Planter Nova Scotia as a separate space, despite the close ties that individual Planters maintained with their homelands. The Revolution forced Planters to choose, but until then many existed between the worlds of Nova Scotia and New England.
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Allaith, Zainab A. "Engagement in Reading and Access to Print: The Relationship of Home and School to Overall Reading Achievement Among Fourth Grade English Speakers." Thesis, 2013. http://hdl.handle.net/1969.1/149385.

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The present study puts forward two models which examine the relationship between at home at school variables of (1) engagement in shared and independent reading and (2) access to print with reading achievement. Participants were fourth grade English speakers from Canada (Alberta, British Columbia, and Nova Scotia), New Zealand, England, and USA. Data from the Progress in International Reading Literacy Study (PIRLS) questionnaires and reading achievement test were used to design the two models, and Hierarchical linear modeling (HLM) was used to analyze the data where students (Level-1) were nested within classrooms (Level-2). The results of the Engagement in Reading Model demonstrate that activities of shared reading at home and at school did not statistically significantly relate or related negatively with reading achievement. Parents helping their children with school readings emerged as the strongest negative predictor of reading achievement in the entire model. However, the relationship between how often participants talked with their families about what they read on their own and reading achievement was positive. Additionally, independent reading at school, reading for fun at home, and reading printed material (books and magazines) at home predicated reading achievement positively; reading for homework did not predict reading achievement; and reading for information and reading on the internet at home predicted reading achievement negatively. The results of the Access to Print Model demonstrate that while access to books and other reading material at home related positively with reading achievement, access to books and other reading material at school did not overall relate to students’ reading achievement. Additionally, access to the library, generally, did not relate to reading achievement; and when statistical significance was found it was not replicated in all or even most of the countries. Based on the results of the present study, it is recommended that fourth graders be given ample opportunities to read books of their own choosing independently at school, and to develop students’ habits and motivation to read for leisure during their free after school time. Additionally, children should be provided with ample access to reading material at home which is geared towards their interests.
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Marsters, Roger Sidney. "Approaches to Empire: Hydrographic Knowledge and British State Activity in Northeastern North America, 1711-1783." 2012. http://hdl.handle.net/10222/15823.

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This dissertation studies the intersection of knowledge, culture, and power in contested coastal and estuarine space in eighteenth-century northeastern North America. It examines the interdependence of vernacular pilot knowledge and directed hydrographic survey, their integration into practices of warfare and governance, and roles in assimilating American space to metropolitan scientific and aesthetic discourses. It argues that the embodied skill and local knowledge of colonial and Aboriginal peoples served vital and underappreciated roles in Great Britain’s extension of overseas activity and interest, of maritime empire. It examines the maritimicity of empire: empire as adaptation to marine environments through which it conducted political influence and commercial endeavour. The materiality of maritime empire—its reliance on patterns of wind and current, on climate and weather, on local relations of sea to land, on proximity of spaces and resources to oceanic circuits—framed and delimited transnational flows of commerce and state power. This was especially so in coastal and riverine littoral spaces of northeastern North America. In this local Atlantic, pilot knowledge—and its systematization in marine cartography through hydrographic survey—adapted processes of empire to the materiality of the maritime, and especially to the littoral, environment. Eighteenth-century British state agents acting in northeastern North America—in Mi’kmaqi/Acadia/Nova Scotia, Newfoundland and Labrador, Quebec, and New England—developed new means of adapting this knowledge to the tasks of maritime empire, creating potent tools with which to extend Britain’s imperial power and influence amphibiously in the eighteenth and nineteenth centuries. If the open Atlantic became a maritime highway in this period, traversed with increasing frequency and ease, inshore waters remained dangerous bypaths, subject to geographical and meteorological hazards that checked overseas commercial exchange and the military and administrative processes that constituted maritime empire. While patterns of oceanic circulation permitted extension of these activities globally in the early modern period, the complex interrelation of marine and terrestrial geography and climate in coastal and estuarine waters long set limits on maritime imperial activity. This dissertation examines the nature of these limits, and the means that eighteenth-century British commercial and imperial actors developed to overcome them.
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Books on the topic "Church of England in Nova Scotia"

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Ritchie, J. N. Twentieth century fund of the diocese of Nova Scotia. [S.l: s.n., 1987.

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Great Britain. Colonial Office. Church convocation (Nova Scotia): Copies of extracts of correspondence between the Secretary of State for the Colonies and the Lieutenant-Governor of Nova Scotia, on the subject of the establishment of a church convocation in the Diocese of Nova Scotia. [London: HMSO, 2002.

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Vernon, Charles William. Bicentenary sketches and early days of the church in Nova Scotia. Halifax, N.S: Church of England Institute, 1996.

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The Church of England in Nova Scotia and the Tory clergy of the Revolution. New York: T. Whittaker, 1989.

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Inglis, John. Letter to the clergy of the United Church of England and Ireland in Nova Scotia. [Halifax, N.S.?: s.n.], 1993.

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Church of England in Canada. Diocese of Nova Scotia. Diocesan Synod. Report of committee on revision of constitution, etc., of the Diocesan synod of Nova Scotia. Halifax, N.S: W. Macnab, 1995.

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Inglis), United Church of England and Ireland Diocese of Nova Scotia Bishop (1825-1850 :. To the clergy and lay members of the established church in the diocese of Nova Scotia. [Halifax, N.S.?: s.n., 1993.

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Binney, Hibbert. Correspondence between the Bishop of Nova Scotia and the Reverend Canon Cochran, M.A., touching the dismissal of the latter from the pastoral charge of Salem Chapel, Halifax, N.S. [Halifax, N.S.?: s.n.], 1986.

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Youle, Hind Henry. Statement of charges against the Right Reverend Hibbert Binney, D.D., Lord Bishop of Nova Scotia, submitted to the Most Reverend the Metropolitan of the Ecclesiastical Province of Canada with documents and correspondence. [Windsor, N.S.?: s.n., 1994.

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Canada. Parliament. House of Commons. Bill: An act respecting the Nova Scotia Steel Company, Limited. Ottawa: S.E. Dawson, 2002.

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Book chapters on the topic "Church of England in Nova Scotia"

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Binasco, Matteo. "The State of the Missionary Church in Acadia in the Years 1654–1669." In French Missionaries in Acadia/Nova Scotia, 1654-1755, 23–47. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-10503-6_2.

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Jordan, Peter G., and Karen R. Polenske. "Multiplier impacts of fishing activities in New England and Nova Scotia." In Input-Output Analysis, 325–66. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2607-3_20.

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Barosh, Patrick J. "Paleozoic Rifting in New England, New Brunswick and Nova Scotia, U.S.A. and Canada." In Basement Tectonics 10, 73–101. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-017-0831-9_15.

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Craigie, Allan. "New Lessons for (and from) the Old World: A study of the politicisation of regional identity in Nova Scotia & North East England." In Travelling Concepts, 211–30. Wiesbaden: VS Verlag für Sozialwissenschaften, 2010. http://dx.doi.org/10.1007/978-3-531-92139-6_11.

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Hardwick, Joseph. "The Church of England, Print Networks and the Book of Common Prayer in the North-Eastern Atlantic Colonies, c. 1750– c. 1830." In Reappraisals of British Colonisation in Atlantic Canada, 1700-1930, 93–112. Edinburgh University Press, 2020. http://dx.doi.org/10.3366/edinburgh/9781474459037.003.0007.

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Despite its ubiquitous presence, the Anglican church in colonial Atlantic Canada has received little attention from scholars. Beginning with the missionary activities of the Society for the Propagation of the Gospel (SPG) which relied on significant revenue from enslaved labour in Barbados, this chapter examines the influence of Anglicanism from Newfoundland to Nova Scotia. It argues that, despite its uniform literature, the Church of England adapted to local circumstances to the extent that it even supplied bi-lingual missionaries to “Foreign Protestants” in the region. This established a diversity of peculiar characteristics and features among Atlantic Canadian congregations that were often maintained after the authority of the episcopal hierarchy was more firmly established during the nineteenth century.
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Ritchie, Holly. "‘For Christ and Covenant’: Scottish Presbyterian Dissent and Early Political Reform in Nova Scotia, 1803–1832." In Reappraisals of British Colonisation in Atlantic Canada, 1700-1930, 113–30. Edinburgh University Press, 2020. http://dx.doi.org/10.3366/edinburgh/9781474459037.003.0008.

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The religious and political implications of Thomas McCulloch’s efforts on behalf of the Pictou Academy in the early nineteenth century are examined in this chapter. McCulloch, a Presbyterian Secessionist minister influenced by the ideas of the Scottish Enlightenment, viewed his Academy as a non-sectarian alternative to the Church of England’s King’s College in Windsor, Nova Scotia, which at the time held a monopoly on advanced education in the colony. The chapter argues that while contemporaries may have viewed the Academy as a subversive institution, McCulloch was also part of the wider British imperial project. His campaign provides one illustration of how dissenting Presbyterians navigated competing loyalties in the colonial context.
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7

"Map: Coast of New England and Western Nova Scotia." In The Diary of Simeon Perkins, 1780-1789 (volume II), 532. Toronto: Champlain Society, 2013. http://dx.doi.org/10.3138/9781442618619_6.

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8

"5. New England Moves North: The South Shore of Nova Scotia." In People of the Wachusett, 165–99. Ithaca, NY: Cornell University Press, 2018. http://dx.doi.org/10.7591/9781501725821-009.

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9

Chopra, Ruma. "Introduction." In Almost Home. Yale University Press, 2018. http://dx.doi.org/10.12987/yale/9780300220469.003.0001.

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This chapter sets the context for the Maroon relocations to Nova Scotia and Sierra Leone. It describes the reconfiguration of the British Empire in the aftermath of the American Revolution, and the importance the British placed on colonizing under-populated zones with loyal subjects. It explores the importance of laborers and settlers—voluntary and involuntary, white and black—for the security of faraway settlements. Second, it examines how the growing abolition movement in England affected the West Indies and shaped utopian visions for Sierra Leone. Last, it explores how the Maroons survived slavery, and benefited from abolitionism and an expanding British Empire. Three successive ex-slave migrations – of the London poor in 1787, of the Nova Scotian loyalists in 1792, and of the Jamaican Maroons in 1800 –established British claims in West Africa. This work describes the circuitous route taken by the last group of free blacks who entered West Africa before the end of the slave trade in 1807.
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Thompson, M. D., S. M. Barr, and J. C. Pollock. "Evolving views of West Avalonia: Perspectives from southeastern New England, USA." In New Developments in the Appalachian-Caledonian- Variscan Orogen. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2554(03).

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ABSTRACT Southeastern New England is largely composed of Ediacaran granitoid and related volcanic rocks formed during the main phase of arc-related magmatism recorded in West Avalonian lithotectonic assemblages extending through Atlantic Canada to eastern Newfoundland. In situ Lu-Hf analyses presented here for zircons from the Dedham, Milford, and Esmond Granites and from the Lynn-Mattapan volcanic complex show a restricted range of εHf values (+2 to +5) and associated Hf-TDM model ages of 1.3–0.9 Ga, assuming felsic crustal sources. The most evolved granites within this suite lie in a belt north and west of the Boston Basin, whereas upfaulted granites on the south, as well as the slightly younger volcanic units, show more juvenile Hf isotopic compositions. Similar inferences have been drawn from previously published Sm-Nd isotopic signatures for several of the same plutons. Collectively, the isotopic compositions and high-precision U-Pb geochronological constraints now available for southeastern New England differ in important respects from patterns in the Mira terrane of Cape Breton Island or the Newfoundland Avalon zone, but they closely resemble those documented in the Cobequid and Antigonish Highlands of mainland Nova Scotia and New Brunswick’s Caledonia terrane. Particularly significant features are similarities between the younger than 912 Ma Westboro Formation in New England and the younger than 945 Ma Gamble Brook Formation in the Cobequid Highlands, both of which yield detrital zircon age spectra consistent with sources on the Timanide margin of Baltica. This relationship provides the starting point for a recent model in which episodic West Avalonian arc magmatism began along the Tonian margin of Baltica and terminated during diachronous late Ediacaran arc-arc collision with the Ganderian margin of Gondwana.
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Conference papers on the topic "Church of England in Nova Scotia"

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Orford, Julian D., and Simon C. Jennings. "Variation in the Organisation of Gravel-Dominated Coastal Systems: Evidence from Nova Scotia and Southern England." In Sixth International Symposium on Coastal Engineering and Science of Coastal Sediment Process. Reston, VA: American Society of Civil Engineers, 2007. http://dx.doi.org/10.1061/40926(239)33.

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2

Keefe, Douglas J., and Joseph Kozak. "Tidal Energy in Nova Scotia, Canada: The Fundy Ocean Research Center for Energy (FORCE) Perspective." In ASME 2011 30th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2011. http://dx.doi.org/10.1115/omae2011-49246.

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Ocean energy developments are appearing around the world including Scotland, Ireland, Wales, England, Australia, New Zealand, Japan, Korea, Norway, France Portugal, Spain, India, the United States, Canada and others. North America’s first tidal energy demonstration facility is in the Minas Passage of the Bay of Fundy, near Parrsboro, Nova Scotia, Canada. The Fundy Ocean Research Center for Energy (FORCE) is a non-profit institute that owns and operates the facility that offers developers, regulators, scientists and academics the opportunity to study the performance and interaction of instream tidal energy converters (usually referred to as TISECs but called “turbines” in this paper.) with one of the world’s most aggressive tidal regimes. FORCE provides a shared observation facility, submarine cables, grid connection, and environmental monitoring at its pre-approved test site. The site is well suited to testing, with water depths up to 45 meters at low tide, a sediment -free bedrock sea floor, straight flowing currents, and water speeds up to 5 meters per second (approximately 10 knots). FORCE will install 10.896km of double armored, 34.5kV submarine cable — one for each of its four berths. Electricity from the berths will be conditioned at FORCE’s own substation and delivered to the Provincial power grid by a 10 km overhead transmission line. There are four berth holders at present: Alstom Hydro Canada using Clean Current Power Systems Technology (Canada); Minas Basin Pulp and Power Co. Ltd. with technology partner Marine Current Turbines (UK); Nova Scotia Power Inc. with technology partner OpenHydro (Ireland) and Atlantis Resources Corporation, in partnership with Lockheed Martin and Irving Shipbuilding. In November 2009, NSPI with technology partner OpenHydro deployed the first commercial scale turbine at the FORCE site. The 1MW rated turbine was secured by a 400-tonne subsea gravity base fabricated in Nova Scotia. The intent of this paper is to provide an overview of FORCE to the international marine energy community during OMAE 2011 taking place in Rotterdam, Netherlands.
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