Re-imagining Democracy in the Age of Revolutions

This book charts a transformation in how people thought about democracy in the North Atlantic region in the years between the American Revolution and the revolutions of 1848. In the mid-eighteenth century, ‘democracy’ was a word known only to literate publics; it was associated primarily with the ancient world, and had negative connotations: democracies were conceived to be unstable, warlike, and prone to mutate into despotisms. By the mid-nineteenth century, by contrast, democracy had become an important category for thinking about the modern world, and had passed into general use – though it was still not necessarily an approving term; in fact, there was much debate about whether democracy could achieve robust institutional form in advanced societies. In this book, an international cast of contributors shows how common trends worked through in four settings: the United States, France, Britain and Ireland, with special attention to the eras of the 1789 and 1848 revolutions. It is argued that ‘modern democracy’ was not invented in one place and then diffused elsewhere, but instead was the subject of parallel re-imaginings, as ancient ideas and examples were selectively invoked and reworked for modern use in different ways in different environments. The book significantly enhances our understanding of the diversity and complexity of our democratic inheritance

2006 ◽  
Vol 11 ◽  
pp. 30-44
Author(s):  
Michael R. MacLeod

Is there an emerging fundamental divide between the United States and Europe in the post 9/11 world? This article examines the transatlantic relationship from a constructivist theoretical approach, emphasizing a security community underlying the North Atlantic region. Constructivists have emphasized how a transnational collective identity develops and builds stable expectations of peaceful relations amongst states, but they have not had much to say about how security communities become de-constructed, i.e. how they break down. To what extent do conflicts in values and norms undermine the collective identity? What I ask here is whether there is a widening difference in the European and American political-strategic cultures that is undermining the security community? My argument is, yes, there is, and the emerging post 9/11 transatlantic security community may look quite different from its predecessor.


1949 ◽  
Vol 3 (2) ◽  
pp. 344-346

The Council convened for its sixth session on January 18, 1949 at ICAO headquarters in Montreal. It adopted a resolution establishing an Air Navigation Commission, which was to assume the functions of the former Air Navigation Committee. The commission was to consist of twelve members, with Argentina, Brazil, Canada, China, France, Netherlands, Sweden, United Kingdom, and the United States having already appointed representatives. Annex 7 (Standards and Recommended Practices for Aircraft Nationality and Registration Marks) to the Convention of International Civil Aviation was adopted by the Council, and approval was granted to the provisional agenda of the third ICAO Assembly, scheduled to open in Montreal on June 7, 1949. Also approved by the Council was the convening in London on April 20 of a combined conference to deal with the problems of North Atlantic weather stations, joint support to Greece in respect to the development of the Ellinikon airport, and provision of essential air navigation services requested by Denmark for its Loran station in the Faeroe Islands. Approval was given to the convening on April 11 in London of a meeting of experts to consider revision of the communications network for carrying meteorological information in the North Atlantic region.


1998 ◽  
Vol 1 (1) ◽  
pp. 41-54 ◽  
Author(s):  
Tom Amorosi ◽  
Paul C. Buckland ◽  
Kevin J. Edwards ◽  
Ingrid Mainland ◽  
Tom H. McGovern ◽  
...  

1989 ◽  
Vol 145 ◽  
pp. 103-108
Author(s):  
M.J Hambrey ◽  
J.S Peel ◽  
M.P Smith

The Caledonides of East Greenland contain the best exposures of Upper Riphean to Ordovician sediments in the Arctic - North Atlantic region. At its thickest the sequence contains 13 km of Eleonore Bay Group clastic sediments and carbonates, the 0.8 km thick Tillite Group and 3 km of Cambro-Ordovician strata (Henriksen & Higgins, 1976; Henriksen, 1985). These sediments crop out in a belt stretching for nearly 300 km through the fjord region, between 71° 38' and 74° 25'N. Those in the northern part of the region, between Brogetdal in Strindberg Land and southern Payer Land, and especiaIly Albert Heim Bjerge and C. H. Ostenfeld Nunatak, were the subject of investigation during 1988 (figs 1, 2).


2021 ◽  
Author(s):  
Helen Mackay ◽  
Gill Plunkett ◽  
Britta Jensen ◽  
Thomas Aubry ◽  
Christophe Corona ◽  
...  

Abstract. The 852/3 CE eruption of Mount Churchill, Alaska, was one of the largest first millennium volcanic events, with a magnitude of 6.7 (VEI 6) and a tephra volume of 39.4–61.9 km3 (95 % confidence). The spatial extent of the ash fallout from this event is considerable and the cryptotephra (White River Ash east; WRAe) extends as far as Finland and Poland. Proximal ecosystem and societal disturbances have been linked with this eruption; however, wider eruption impacts on climate and society are unknown. Greenland ice-core records show that the eruption occurred in winter 852/3 ± 1 CE and that the eruption is associated with a relatively moderate sulfate aerosol loading, but large abundances of volcanic ash and chlorine. Here we assess the potential broader impact of this eruption using palaeoenvironmental reconstructions, historical records and climate model simulations. We also use the fortuitous timing of the 852/3 CE Churchill eruption and its extensively widespread tephra deposition of the White River Ash (east) (WRAe) to examine the climatic expression of the warm Medieval Climate Anomaly period (MCA; ca. 950–1250 CE) from precisely linked peatlands in the North Atlantic region. The reconstructed climate forcing potential of 852/3 CE Churchill eruption is moderate compared with the eruption magnitude, but tree-ring-inferred temperatures report a significant atmospheric cooling of 0.8 °C in summer 853 CE. Modelled climate scenarios also show a cooling in 853 CE, although the average magnitude of cooling is smaller (0.3 °C). The simulated spatial patterns of cooling are generally similar to those generated using the tree-ring-inferred temperature reconstructions. Tree-ring inferred cooling begins prior to the date of the eruption suggesting that natural internal climate variability may have increased the climate system’s susceptibility to further cooling. The magnitude of the reconstructed cooling could also suggest that the climate forcing potential of this eruption may be underestimated, thereby highlighting the need for greater insight into, and consideration of, the role of halogens and volcanic ash when estimating eruption climate forcing potential. Precise comparisons of palaeoenvironmental records from peatlands across North America and Europe, facilitated by the presence of the WRAe isochron, reveal no consistent MCA signal. These findings contribute to the growing body of evidence that characterizes the MCA hydroclimate as time-transgressive and heterogeneous, rather than a well-defined climatic period. The presence of the WRAe isochron also demonstrates that no long-term (multidecadal) climatic or societal impacts from the 852/3 CE Churchill eruption were identified beyond areas proximal to the eruption. Historical evidence in Europe for subsistence crises demonstrate a degree of temporal correspondence on interannual timescales, but similar events were reported outside of the eruption period and were common in the 9th century. The 852/3 CE Churchill eruption exemplifies the difficulties of identifying and confirming volcanic impacts for a single eruption, even when it is precisely dated.


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