The Mississippi of the North: Trailer Park Boys and Race in Contemporary Nova Scotia

2015 ◽  
Vol 49 (1) ◽  
pp. 180-204
Author(s):  
Peter Thompson
Keyword(s):  
Nova Scotia ◽  
The North

PREDATION BY INSECTS AND SPIDERS INHABITING COLONIAL WEBS OF HYPHANTRIA CUNEA

1972 ◽  
Vol 104 (8) ◽  
pp. 1197-1207 ◽  
Author(s):  
R. F. Morris
Keyword(s):  
Population Dynamics ◽  
Nova Scotia ◽  
North America ◽  
Population Density ◽  
New Brunswick ◽  
Numerical Response ◽  
Initial Number ◽  
Hyphantria Cunea ◽  
The North ◽  
The Mean

AbstractThe number of predators inhabiting nests of Hyphantria cunea Drury was recorded annually for 13 years in four areas in New Brunswick and two areas on the coast of Nova Scotia. The most common groups were the pentatomids and spiders, which sometimes reproduced within the nests, but the mean number per nest was low in relation to the number of H. cunea larvae in the colonies. The rate of predation on fifth-instar larvae was low. Small or timid predators appeared to prey largely on moribund larvae or small saprophagans during the principal defoliating instars of H. cunea.No relationship could be detected between the number of larvae reaching the fifth instar and the number of predators in the colony; nor could any functional or numerical response of the predators to either the initial number of larvae per colony or the population density of colonies be found. It is concluded that the influence of the nest-inhabiting predators is small and relatively stable, and may be treated as a constant in the development of models to explain the population dynamics of H. cunea.H. cunea is a pest in parts of Europe and Asia, where it has been accidentally introduced from North America. The introduction to other continents of the North American predator, Podisus maculiventiis (Say), is discussed briefly.

REPEATED TRENDS OF FOLDS AND CROSS-FOLDS IN PALAEOZOIC ROCKS, PARRSBORO, NOVA SCOTIA

1964 ◽  
Vol 1 (3) ◽  
pp. 167-183 ◽  
Author(s):  
W. K. Fyson
Keyword(s):  
Nova Scotia ◽  
Vertical Movements ◽  
Clastic Rocks ◽  
Three Generations ◽  
The North ◽  
North Side ◽  
Two Generations ◽  
Major Fault ◽  
Granitic Intrusions ◽  
Middle Carboniferous

On the north side of a major fault three generations of folds F1, F2, F3 affect pre-Carboniferous phyllites; south of the fault two generations, C1, C2, affect middle Carboniferous clastic rocks. The F1 folds are isoclinal and obscure. The main folds, F2 in the phyllites and C1 in the Carboniferous rocks, trend east-northeast parallel to the fault. F2 are overturned southward and C1 northward, both toward the fault. Cross-folds, F3 in the phyllites and C2 in the Carboniferous rocks, trend northnortheast. Steeply plunging F3 and C2 are asymmetric and Z-shaped in plan profile.The F2 folds in the phyllites, though similar in geometry to folds in the middle Carboniferous rocks, appear, like F1 and F2, to have formed prior to the middle Carboniferous. This is indicated by the occurrence of unfolded Devonian(?) granitic intrusions crossing F3 folds, and a few miles north of the major fault, by middle Carboniferous rocks lying unconformably- above similar intrusions.One possible explanation for the repeated trends, which also accounts for the sense of overturning and asymmetry of the folds, relates the folding to alternating vertical and horizontal movements along the major fault. The vertical movements were followed by gravity sliding toward the fault to produce the main folds, and the horizontal movements, repeatedly dextral in sense, resulted in the Z-shaped cross-folds.

Business and Technical Aspects of the Building of Cape Breton Miner

1967 ◽  
Vol 4 (01) ◽  
pp. 558-590
Author(s):  
_ Staff ◽  
_ Staff
Keyword(s):  
Nova Scotia ◽  
North Atlantic ◽  
Iron Ore ◽  
Technical Aspects ◽  
The North ◽  
Cape Breton ◽  
Hull Design ◽  
The North Atlantic ◽  
And Performance ◽  
Considerable Damage

The Cape Breton Miner has been in operation since June 1 964. This vessel has transported and self-unloaded coal from Nova Scotia and U. S. A., iron ore from Venezuela, Seven Islands' pellets, gypsum from Nova Scotia, and has recirculated grain through the unloading system in order to unload the grain from one hatch only. To operate successfully an unloading crew requires experience with each type of cargo in the particular vessel. The hull design, the boiler automation, the all-belt unloading feature can be considered completely successful. The sea speeds and performance in ocean storms has been as predicted from trial results. The Cape Breton Miner encountered a full gale in the North Atlantic in January 1965, experiencing winds gusting up to 80 mph. A large American liner suffered considerable damage from this same storm. A sistership Ontario Power was delivered to the owners in May 1965. The latter vessel is of the same hull design and includes all the features of the Cape Breton Miner. Several minor changes were introduced in order to better the unloading performance.

Introduction

2021 ◽  
pp. 1-13
Author(s):  
Brad A. Jones
Keyword(s):  
New York ◽  
Nova Scotia ◽  
French Revolution ◽  
American Revolution ◽  
York City ◽  
Port Cities ◽  
The North ◽  
The Face ◽  
The North Atlantic

This introductory chapter provides an overview of how the American Revolution shaped a popular transatlantic understanding of British loyalism, focusing on the four port cities spanning the North Atlantic: New York City; Kingston, Jamaica; Halifax, Nova Scotia; and Glasgow, Scotland. During the early stages of the revolution, a shared transatlantic understanding of what it meant to be British in these four communities initially crumbled in the face of the Patriots' assertion that their cause was rooted in a defense of Protestant British liberty. Patriot arguments led loyal Britons in these places to question what defined their attachment to the empire. Out of these crises there emerged a new understanding of loyalism rooted in a strengthened defense of monarchy and duly constituted government. After the Franco-American alliance of 1778, loyal Britons were also able to reclaim their belief in the supremacy of Protestant British liberty, which they contrasted with the alleged tyranny of American Patriots and their French Catholic allies. Ultimately, the British loyalism as it developed in the wake of the American war was more conservative and authoritarian, reaching its apogee in the reaction against the radicalism of the French Revolution and the despotism of Napoleon.

The Distribution and Abundance of Wireworms in the Annapolis Valley of Nova Scotia

1961 ◽  
Vol 93 (4) ◽  
pp. 276-279 ◽  
Author(s):  
C. J. S. Fox
Keyword(s):  
Nova Scotia ◽  
Important Species ◽  
The North ◽  
Agricultural Areas ◽  
Annapolis Valley ◽  
North And South

The Annapolis Valley is about 100 miles long and is one of the largest and most important of the agricultural areas of the province. The general relief is undulating to gently rolling, with general slopes from the North and South Mountains to the Annapolis and Cornwallis Rivers. The soils of the Annapolis Valley and Hants County were described by Harlow and Whiteside (6) and Cann, Hilchey and Smith (1). A wireworm survey was conducted between 1951 and 1958 since it was suspected that economically important species of European wireworms, namely Agriotes sputator (L.), A. obscurus (L.), and A. lineatus (L.), which occur elsewhere in the province, might be invading the area. The results of this survey are reported here.

The first report of a macroloxoceratine cephalopod from the North American Mississippian

1988 ◽  
Vol 62 (2) ◽  
pp. 309-311 ◽  
Author(s):  
Gregory D. Edgecombe
Keyword(s):  
New Mexico ◽  
Nova Scotia ◽  
North American ◽  
Upper Devonian ◽  
Canal System ◽  
First Report ◽  
The North ◽  
Rare Group

The pseudorthoceratid subfamily Macroloxoceratinae Flower, 1957, comprises a rare group of nautiloid cephalopods homeomorphic with the Actinoceratida in the development of a siphonal canal system. With the exception of Macroloxoceras Flower, 1957, from the Upper Devonian of Colorado and New Mexico, this subfamily has previously been reported only from the Mississippian of Europe. A specimen described herein from the late Viséan–?early Namurian Kennetcook Limestone of the Windsor Group of Nova Scotia, assigned to Campyloceras cf. C. unguis (Phillips, 1836), extends the range of the Macroloxoceratinae into the North American Mississippian. This discovery further provides new data on the complex siphonal morphology of this poorly known group of nautiloids, and supplements the recent documentation of the pseudorthoceratids in the Windsor Group cephalopod fauna (Edgecombe, 1987).

Viséan limestones front the Newfoundland Shelf

1978 ◽  
Vol 15 (9) ◽  
pp. 1422-1436 ◽  
Author(s):  
L. F. Jansa ◽  
B. Mamet ◽  
A. Roux
Keyword(s):  
Nova Scotia ◽  
North American ◽  
Single Species ◽  
Early Carboniferous ◽  
American Continent ◽  
Lower Carboniferous ◽  
The North

Three short cores of Windsor Group carbonates from the northeast Newfoundland Shelf yielded Late Viséan foraminifers of Zones 15 and 16Inf. This most northeastward occurrence of the marine Lower Carboniferous on the American continent has foraminifers identical to those reported from Windsor carbonates exposed in southwestern Newfoundland and Nova Scotia. The foraminifera belong to the North American realm and not to the Tethyan realm. The algae are exceptionally well preserved. Except for a single species, they are also 'American' and not Tethyan. This confirms that the proto-Atlantic effectively separates the North American and Euro–African continental blocks in Early Carboniferous time.

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