A History of the Mohawk Valley and Early Lumbering. By Louis E. Polley, assisted by Sue Bailey. (Marcola, Oregon: Polley Publishing, 1984. ii + 146 pp. Illustrations, credits, glossary, maps. Paper $19.50.)

1985 ◽  
Vol 29 (4) ◽  
pp. 188-188
Author(s):  
W.D. Hagenstein
Keyword(s):  
Mohawk Valley ◽  
History Of

Northward subglacial drainage during the Mackinaw Interstade in the Cayuga basin, central New York, USA

2020 ◽  
Vol 57 (8) ◽  
pp. 981-998 ◽  
Author(s):  
Daniel E. Karig ◽  
Todd S. Miller
Keyword(s):  
New York ◽  
Drainage System ◽  
Seismic Profiles ◽  
Mohawk Valley ◽  
Subglacial Lake ◽  
Proglacial Lakes ◽  
Lake Outlet ◽  
Water Wells ◽  
History Of ◽  
Subglacial Drainage

The history of deglaciation in the Finger Lakes region since the Valley Heads readvance is questioned by recent research in the Cayuga basin, which concludes that, instead of forming a series of proglacial lakes, drainage during the Mackinaw Interstade was into the Laurentide ice sheet. First suspected in the Dryden–Virgil Valley where there is an absence of a lake outlet or surficial lacustrine deposits, this conclusion was explicitly revealed in the Sixmile–Willseyville trough where ice margin channels funneled water into the ice front. Further support was found in the Cayuga Inlet Valley, where a kettle kame terrane sloped northward into the ice front. Northward drainage was preceded by southerly drainage, with reversal occurring about 16.3 kyr ago. Multi-channel seismic profiles at the south end of Lake Cayuga reveal a south-sourced subaqueous sedimentary fan at the base of the lacustrine sequence. This fan is correlated with a coarse and heterogeneous clastic sequence penetrated in water wells in the City of Ithaca and requires northward drainage into a subglacial lake, which precludes the existence of proglacial lakes Ithaca, Newberry, and Hall. The proposed subglacial flow path is through the Cayuga trough, exiting the ice front eastward in the Mohawk Valley. Subglacial drainage from the Cayuga trough probably was part of a regional subglacial drainage system during the Mackinaw Interstade. Studies north of Lake Ontario have led to the proposal of a subglacial lake in the Ontario basin at that time, which likely also drained into the Mohawk Valley.

The Social Origins and Provenance of the English Bishops during the Reign of Edward II

1959 ◽  
Vol 9 ◽  
pp. 51-79
Author(s):  
K. Edwards
Keyword(s):  
Middle Ages ◽  
Social Background ◽  
Early Career ◽  
The Political ◽  
Social Origins ◽  
Political Activities ◽  
Edward Ii ◽  
The Social ◽  
Complete Study ◽  
History Of

During the last twenty or twenty-five years medieval historians have been much interested in the composition of the English episcopate. A number of studies of it have been published on periods ranging from the eleventh to the fifteenth and early sixteenth centuries. A further paper might well seem superfluous. My reason for offering one is that most previous writers have concentrated on analysing the professional circles from which the bishops were drawn, and suggesting the influences which their early careers as royal clerks, university masters and students, secular or regular clergy, may have had on their later work as bishops. They have shown comparatively little interest in their social background and provenance, except for those bishops who belonged to magnate families. Some years ago, when working on the political activities of Edward II's bishops, it seemed to me that social origins, family connexions and provenance might in a number of cases have had at least as much influence on a bishop's attitude to politics as his early career. I there fore collected information about the origins and provenance of these bishops. I now think that a rather more careful and complete study of this subject might throw further light not only on the political history of the reign, but on other problems connected with the character and work of the English episcopate. There is a general impression that in England in the later middle ages the bishops' ties with their dioceses were becoming less close, and that they were normally spending less time in diocesan work than their predecessors in the thirteenth century.

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