A Building History of Northern New England

2002 ◽  
Vol 75 (1) ◽  
pp. 169
Author(s):  
W. Barksdale Maynard ◽  
James L. Garvin
APT Bulletin ◽  
2002 ◽  
Vol 33 (1) ◽  
pp. 56
Author(s):  
Robert A. Young ◽  
James L. Garvin

Author(s):  
John Reid

This article traces the author’s path from early life in the United Kingdom to graduate school in Newfoundland and New Brunswick and then to a series of faculty positions – ultimately, at Saint Mary’s University. Early work in the seventeenth-century history of northern New England gave way to a more broadly comparative approach to this era and, eventually, to an effort to coordinate imperial, colonial, and Indigenous history in northeastern North America. A variety of career uncertainties and evolutions also led to involvement in the history of higher education, the history of Atlantic Canada, and the history of sport. Through it all, collaborative work developed as a recurrent approach, with Atlantic Canada themes frequently underpinning responses to a variety of historiographies.


2002 ◽  
Vol 24 (2) ◽  
pp. 109-111
Author(s):  
Claire W. Dempsey

2008 ◽  
Vol 45 (3) ◽  
pp. 287-301 ◽  
Author(s):  
David P. West ◽  
Mary K. Roden-Tice ◽  
Jaime K. Potter ◽  
Nellie Q. Barnard

As a part of a regional effort to determine the extent of low-temperature thermochronological discontinuities across major orogen-parallel faults in northern New England, 41 apatite fission track (AFT) ages and 11 (U–Th)/He ages are used to constrain the ∼65 to 100 °C cooling history of rocks flanking a 160 km long segment of the Norumbega fault system in southern and south-central Maine. These data are used to evaluate the role of this structure in the late Mesozoic and younger exhumation history of the northern Appalachians. AFT ages flanking the fault system range from 159 to 95 Ma and record cooling below ∼100 °C in the late Mesozoic. (U–Th)/He ages from the same region range from 126 to 100 Ma and record cooling below ∼65 °C. Previously published AFT ages from an ∼40 km long segment of the fault system just north of Casco Bay reveal a dramatic time–temperature discontinuity across the structure and suggest kilometre-scale late Mesozoic displacement in this region. However, new AFT and (U–Th)/He ages along the strike of the Norumbega fault system to the northeast and southwest of this discontinuity show no significant differences in late Mesozoic cooling and suggest no significant displacements occurred along these portions of the fault system during this time. Collectively the data suggest differential late Mesozoic reactivation of the Norumbega fault system with the reactivation localized in areas that had previously experienced episodes of vertical displacement in the late Paleozoic (i.e., the “Casco Bay restraining bend”).


2000 ◽  
Vol 1 (3) ◽  
pp. 21
Author(s):  
John E. Allen

No more interesting or appealing subject than the Cape Cod Canal could be assigned to one who is engaged in the study and development of navigation in New England. This sea-level canal, located 50 miles south of Boston at the narrow neck of land joining Cape Cod to the mainland, principally serves coastwise shipping to and from Boston and Northern New England. While it was only completed in 1940 no one should entertain the thought that it is of recent origin.


Author(s):  
Oswald J. Schmitz

This chapter examines how humans and nature can become increasingly entwined as a socio-ecological system. Northern cod stocks were once so plentiful in the waters off eastern Canada and northern New England. Five centuries later, the commercial northern cod fishery would collapse in dramatic fashion. To understand how the changes happened, the chapter divides the history of the northern cod fishery into four major periods of human engagement that began in 1500 and lasted until 1990. It also considers the development of new computational tools that have led to new principles that can help ecologists anticipate state changes in complex ecosystems and thereby better guide human engagement with nature's economy. Finally, it explains how the New Ecology can help us better understand the nested hierarchy and mechanisms of the inner workings of socio-ecological systems and the nonlinear responses that arise when they are disturbed or exploited.


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