The Maugerville Church and the American Revolution

1938 ◽  
Vol 7 (4) ◽  
pp. 371-380 ◽  
Author(s):  
H. W. Barker

On the east bank of the St. John River, sixty miles above the city of St. John and eighteen miles below Fredericton, is an attractive white church building of the New England type. Its graceful spire cannot fail to catch the eye and call forth expressions of admiration as travelers pass by motor or river steamer. This houses the oldest Protestant church organization in what is now the Province of New Brunswick, though this building is not the original one. It was a “society” of the Congregational order, now an integral part of The United Church of Canada, and known as Sheffield.

2020 ◽  
Vol 94 (3) ◽  
pp. 631-636
Author(s):  
Noam Maggor

Mark Peterson's The City-State of Boston is a formidable work of history—prodigiously researched, lucidly written, immense in scope, and yet scrupulously detailed. A meticulous history of New England over more than two centuries, the book argues that Boston and its hinterland emerged as a city-state, a “self-governing republic” that was committed first and foremost to its own regional autonomy (p. 6). Rather than as a British colonial outpost or the birthplace of the American Revolution—the site of a nationalist struggle for independence—the book recovers Boston's long-lost tradition as a “polity in its own right,” a fervently independent hub of Atlantic trade whose true identity placed it in tension with the overtures of both the British Empire and, later, the American nation-state (p. 631).


1987 ◽  
Vol 65 (6) ◽  
pp. 1163-1179 ◽  
Author(s):  
David G. Green

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.


2005 ◽  
Vol 17 (41) ◽  
pp. 251-264
Author(s):  
Gilbert Cestre

The present study is one of the unpublished research projects which are known to have been conducted in New England and in Eastern Canada under the guidance of the late Richard J. LOUGEE, long-time professor of Geomorphology at Clark University. Over a number of years, this writer has worked in close relationship with Lougee and much evidence in the field was studied together. It is believed that here has been recorded a most detailed work of surveying, and this undoubtedly accounts for the somewhat exceptional results that will be presented. The area selected for this study (about 80% of it is woodland) is located in the highlands of Central Massachusetts in Worcester County, about twenty miles (32 kilo-meters) northwest of the city of Worcester. It consists of the valley of the Otter River draining north, and of a small portion of the East Branch of the Ware River draining south. Since completion of this study, parts of the low area which held the ancient glacial lakes have been flooded to become water reservoirs. That proglacial lakes, though temporary they may have been, once submerged much of the area under study, is shown by an abundance of deltas, kames, eskers and deltaic kames terraces. It is believed that all of these were built under water in such lakes. Other features, such as kettle-holes and glacial outlets, especially ice-marginal channels cut diagonally down the slope, have also been studied. By plotting on a profile of the most characteristic elevations (often carefully surveyed), it is possible to find the water planes of ancient proglacial lakes. To this must be added experiments conducted in a sedimentation tank as also measurements of both the imbrication of cobbles in eskers and the « smoothness indexes » of such stones and pebbles, using A. Cailleux' methods. Thus were obtained results which tend to show that : 1- the area under study probably was in a deep interlobate space created between the Connecticut Valley lobe to the west and the Boston Basin lobe to the east ; 2— ice-marginal channels are an indication of the existence of a thick, fast-retreating ice border ; 3- an isostatic balance restored itself by sometimes quick and strong adjustments of the crust of the earth ; 4— an early upwarping, made up of various zones of tilting articulated on hinge lines, has been referred to as Hubbard Uplift and is the earliest known in the post-Glacial history of New England.


2020 ◽  
Vol 10 (2-3) ◽  
pp. 179-246
Author(s):  
Emma Hart ◽  
Robert J. Allison ◽  
Paul P. Musselwhite ◽  
Daniel K. Richter ◽  
Mark Peterson

Abstract In his book Mark Peterson presents an innovative perspective on the development of Boston and its New England hinterland as an early modern city-state. His purpose was to tell the story of Boston in its own right, shedding US national history as the dominant interpretative framework. The four reviewers pick up various strands, focusing, among others, on the validity of the city-state concept, especially as Boston did not become an incorporated city until 1822, criticize what one of them sees as an attempt to return New England to the center of early American historiography, and assess whether the city-state model can be applied elsewhere in early America and in the Atlantic World. In his response, Peterson argues that his aim was not to propose a city-state paradigm for comparative purposes, but rather to employ the city-state concept as the best way to explain Boston’s historical trajectory over two centuries, and to highlight the contingency of US history.


2019 ◽  
Vol 9 (2-3) ◽  
pp. 163-198
Author(s):  
Sophie H. Jones

This paper responds to most recent works on the complexity of loyalist identities during the American Revolution. It forms a close reading of over 400 claims submitted by self-identified loyalist claimants from the former colony of New York to the Loyalist Claims Commission. Through a case study of three New York counties (the city and county of New York, Albany County and Tryon County), the paper demonstrates that the loyalist experience differed greatly between the three distinct geographic regions; different counties entered the war at different stages, while demonstrations of loyalism and the range of services provided by loyalists to advance the British cause varied considerably. The paper also outlines (and justifies the use of) the potential of three broad categories by which to analyze loyalist claimants: namely, ‘active’, ‘reluctant’ and ‘passive’. Ultimately, this paper concludes that the varying nature of loyalism was largely the product of local contextual circumstance.


Geosciences ◽  
2019 ◽  
Vol 9 (6) ◽  
pp. 265 ◽  
Author(s):  
David S. Ullman ◽  
Isaac Ginis ◽  
Wenrui Huang ◽  
Catherine Nowakowski ◽  
Xuanyu Chen ◽  
...  

The southern New England coast of the United States is particularly vulnerable to land-falling hurricanes because of its east-west orientation. The impact of two major hurricanes on the city of Providence (Rhode Island, USA) during the middle decades of the 20th century spurred the construction of the Fox Point Hurricane Barrier (FPHB) to protect the city from storm surge flooding. Although the Rhode Island/Narragansett Bay area has not experienced a major hurricane for several decades, increased coastal development along with potentially increased hurricane activity associated with climate change motivates an assessment of the impacts of a major hurricane on the region. The ocean/estuary response to an extreme hurricane is simulated using a high-resolution implementation of the ADvanced CIRCulation (ADCIRC) model coupled to the Precipitation-Runoff Modeling System (PRMS). The storm surge response in ADCIRC is first verified with a simulation of a historical hurricane that made landfall in southern New England. The storm surge and the hydrological models are then forced with winds and rainfall from a hypothetical hurricane dubbed “Rhody”, which has many of the characteristics of historical storms that have impacted the region. Rhody makes landfall just west of Narragansett Bay, and after passing north of the Bay, executes a loop to the east and the south before making a second landfall. Results are presented for three versions of Rhody, varying in the maximum wind speed at landfall. The storm surge resulting from the strongest Rhody version (weak Saffir–Simpson category five) during the first landfall exceeds 7 m in height in Providence at the north end of the Bay. This exceeds the height of the FPHB, resulting in flooding in Providence. A simulation including river inflow computed from the runoff model indicates that if the Barrier remains closed and its pumps fail (for example, because of a power outage or equipment failure), severe flooding occurs north of the FPHB due to impoundment of the river inflow. These results show that northern Narragansett Bay could be particularly vulnerable to both storm surge and rainfall-driven flooding, especially if the FPHB suffers a power outage. They also demonstrate that, for wind-driven storm surge alone under present sea level conditions, the FPHB will protect Providence for hurricanes less intense than category five.


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