The Frank Bay Site, Lake Nipissing, Ontario

1954 ◽  
Vol 20 (01) ◽  
pp. 40-50 ◽  
Author(s):  
Frank Ridley

Lake Nipissing is situated 230 miles north of Lake Ontario and roughly 140 miles within the igneous rock territory. Some 30 by 8 miles in size, it is drained westerly by the French River into Lake Huron. Frank Bay, enclosing an area of one half square mile, is situated on the south shore at the entrance to the French River. Historically the area was occupied by an Algonkian group called “Nipisinieries” or “Nipissings” by the 17th century Jesuits; Galinee's map of 1665 depicts a bay on the south shore of Lake Nipissing at the head of the French River: “In a bay at this place the Nipissings usually locate their village” (Coyne, 1903). The site described here, probably the one figured by Galinee, is a level tract of about one half acre constructed by wave deposition of coarse sand upon a low area at the bottom of the bay.

2015 ◽  
Vol 3 (1) ◽  
pp. cov036 ◽  
Author(s):  
Susan B. Smith ◽  
Allyson C. Miller ◽  
Charmaine R. Merchant ◽  
Amie F. Sankoh

The Auk ◽  
2007 ◽  
Vol 124 (1) ◽  
pp. 122 ◽  
Author(s):  
David N. Bonter ◽  
Therese M. Donovan ◽  
Elizabeth W. Brooks
Keyword(s):  

Author(s):  
A. T. Nicol

The salt-marsh under investigation is situated at Aberlady Bay on the south shore of the Firth of Forth, fifteen miles east of Edinburgh.The marsh is small and occurs at the mouth of a stream. The character of the soil on the two banks differs, being on the one side muddy with permanent pools, and on the other sandy, so that the pools tend to drain dry. The vegetation of the pools is variable, some containing species of Zostera, Ulva, Enteromorpha and Vaucheria, others having only diatoms.


Author(s):  
John F. Storr ◽  
Patricia J. Hadden-Carter ◽  
Julian M. Myers ◽  
A. Garry Smythe
Keyword(s):  

The Auk ◽  
2007 ◽  
Vol 124 (1) ◽  
pp. 122-133 ◽  
Author(s):  
David N. Bonter ◽  
Therese M. Donovan ◽  
Elizabeth W. Brooks

Abstract Assigning conservation priorities to areas used by birds during migration requires information on the relative quality of areas and habitats. The rate at which migratory birds replenish energy reserves during stopover may be used as an indicator of stopover-site quality. We estimated the rate of mass gain of 34 landbird species during stopover at a near-shore terrestrial site on the south shore of Lake Ontario in New York during 12 migration seasons from 1999 to 2004. The average rate of mass gain was estimated by relating a measure of condition to time of capture (hour after sunrise) with linear regression. Data from 25,385 captures were analyzed. Significantly positive rates of mass change were detected for 20 of 30 species during spring migration and 19 of 21 species during autumn migration. No significantly negative trends were detected in either season. Daily rates of mass gain across all species averaged 9.84% of average lean body weight during spring migration and 9.77% during autumn migration. Our regression estimates were significantly greater than estimates from traditional analyses that examine mass changes in recaptured birds. Analyses of mass changes in recaptured birds revealed a mean daily change of −0.68% of average lean mass in spring and 0.13% in autumn. Because of sampling biases inherent in recapture analyses, the regression approach is likely more accurate when the assumptions of the method are met. Similar studies in various habitats, landscapes, and regions are required to prioritize conservation efforts targeting migratory stages of the annual cycle. Cambios de Peso Diarios de Aves Terrestres durante las Paradas Migratorias en la Costa sur del Lago Ontario


1993 ◽  
Vol 30 (6) ◽  
pp. 1236-1241 ◽  
Author(s):  
John W. Hofer ◽  
John P. Szabo

The flow directions of ice lobes within the Erie basin may be deduced from heavy-mineral assemblages of the Hayesville, Hiram, and Ashtabula tills deposited during the Port Bruce Stade after the Erie Interstade. These tills have heavy-mineral assemblages dominated by purple garnet, green hornblende, and clinopyroxene. Oolitic hematite occurs in all tills, but is dominant in the Ashtabula Till. The probable source of hematite is the Furnaceville Ironstone Member of the Clinton Group which crops out south of Lake Ontario. Trilinear plots of purple garnet – red garnet – epidote suggest that the eastern Grenville Subprovince is the provenance of all three tills. Southwestward-flowing ice of an Ontario–Erie lobe deposited these tills in the Erie basin. The Huron–Erie lobe did not deposit tills along the south shore of Lake Erie after the Erie Interstade.


1989 ◽  
Vol 24 (4) ◽  
pp. 589-608 ◽  
Author(s):  
I.K. Tsanis ◽  
J. Biberhofer ◽  
C.R. Murthy ◽  
A. Sylvestre

Abstract Determination of the mass output through the St. Lawrence River outflow system is an important component in computing mass balance of chemical loadings to Lake Ontario. The total flow rate in the St. Lawrence River System at the Wolfe Island area was calculated from detailed time series current meter measurements from a network of current meters and Lagrangian drifter experiments. This flow is roughly distributed in the ratio of 55% to 45% in the South and North channel, respectively. Loading estimates of selected chemicals have been made by combining the above transport calculations with the ongoing chemical monitoring data at the St. Lawrence outflow. A vertical gradient in the concentration of some organic and inorganic chemicals was observed. The measured concentration for some of the chemicals was higher during the summer months and also is higher in the South Channel than in the North Channel of the St. Lawrence River. These loading estimates are useful not only for modelling the mass balance of chemicals in Lake Ontario but also for serving as input loadings to the St. Lawrence River system from Lake Ontario.


2018 ◽  
Author(s):  
Rebeka Smith ◽  
◽  
Thomas Badamo ◽  
David J. Barclay ◽  
Devorah Crupar ◽  
...  

Prospects ◽  
1982 ◽  
Vol 7 ◽  
pp. 249-266
Author(s):  
Lewis P. Simpson

No scene in Faulkner is more compelling than the one that transpires on a “long still hot weary dead September afternoon” in Yoknapatawpha County, Mississippi, toward the end of the first decade of this century. Quentin Compson sits with Miss Rosa Coldfield in a “dim airless room” still called “the office because her father called it that,” and listens to Miss Rosa tell her version of the story of the “demon” Sutpen and his plantation, Sutpen's Hundred. As she talks “in that grim haggard amazed voice”—“vanishing into and then out of the long intervals like a stream, a trickle running from patch to patch of dried sand”—the 22-year-old Mississippi youth discovers he is hearing not Miss Rosa but the voices of “two separate Quentins.” One voice is that of the “Quentin preparing for Harvard in the South, the deep South dead since 1865 and peopled with garrulous baffled ghosts.” The other voice is that of the Quentin “who was still too young to deserve yet to be a ghost, but nevertheless having to be one for all that, since he was born and bred in the deep South the same as she [Miss Rosa] was.” The two Quentins talk “to one another in the long silence of notpeople, in notlanguage: It seems that this demon—his name was Sutpen—(Colonel Sutpen)—Colonel Sutpen. Who came out of nowhere and without warning upon the land with a band of strange niggers and built a plantation”.


2021 ◽  
pp. 205789112110211
Author(s):  
Zafar Khan

This article primarily focuses on how the increasing US–China competing strategies in Asia-Pacific affect the policies of South Asian rivals India and Pakistan when, on the one hand, the US as part of its offshore balancing grand strategy has been increasing its strategic partnership with India through the transfer of emerging technologies in terms of military modernization process, and on the other hand, China and Pakistan have improved their geo-economic and geostrategic partnership as part of the Chinese grand strategy via the Belt and Road Initiative while enabling Pakistan to produce effective countermeasures against its potential adversary. The article presumes that, in doing so, such competing strategies frame a quadrangle setting comprising of US and India to deter and contain China on the one hand and China and Pakistan to produce countermeasures and try to create a balance to potentially prevent the risk of conflict in South Asia out of such competing strategies at the quadrangle order conceived here. However, in fact, neither the US nor rising China would desire such a possibility of conflict otherwise unintendedly occurring from the intense US–China competing strategies while affecting the policies of the South Asian rivals. The article concludes that the shaping of this quadrangle framework may bring both opportunities and challenges for the South Asian rivals. It also concludes that the more intense the competition between the US and China becomes, the more intense its implications could be on the South Asian rivals, while the reduced tension between China and the US, although unlikely, would have reduced pressure on India and Pakistan relations as well.


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