scholarly journals Geology of the West Branch North River and the Bothan Brook Plutons of the South-Central Cape Breton Highlands, Nova Scotia

1986 ◽  
Author(s):  
A M O'beirne-ryan ◽  
R A Jamieson
Author(s):  
Peter Mitchell

Taking in the Andean cordillera, the Pampas grasslands of Argentina and Uruguay, the desert steppes of southern Patagonia, and the temperate lowlands of south-central Chile (Araucanía), this chapter explores the horse’s arrival and impact in South America’s Southern Cone. Convention divides the Cone along the spine of the mountains between Chile and Argentina. To their east it contrasts the Pampas in the north with Patagonia in the south. I follow most recent scholarship in stressing the historical connections that such boundaries obscure. Similarly, I emphasize not only the acquisition of horses, but also the significance of hunting, taking, and trading feral livestock and the adoption of elements of food production. Both developments formed part of the inclusion of ‘free’ Native Americans within broader international political and commercial systems. At the same time, the work of anthropologists and the comments of contemporary European observers make the Southern Cone one of the most richly documented regions of all for studying the emergence of Horse Nations post-1492. The Southern Cone is environmentally far more complex than a simple tripartite classification into Araucanía, Patagonia, and Pampas suggests. In the north the Pampas reach to the Paraná and Salado drainages, to the south as far as the Río Colorado and its tributaries. They extend east to include Uruguay and the Brazilian state of Rio Grande do Sul and in the west reach the Andean foothills. A basic division follows the 500 mm isohyet: to its west the Dry Pampa is increasingly water-deficient, while to the east the Humid Pampa ultimately benefits from as much as 800 mm of rain a year (Plate 23). The Uruguayan Savannah forms a third ecological subdivision that includes areas with palms and some forest enclaves. Generally, the Pampas comprise a gently sloping plain covered by extensive grasslands, but drier-adapted shrub occurs in the west and a wedge of forest penetrates their centre from the north. The Sierra de Tandilia and Sierra de la Ventana south of Buenos Aires are rare areas of higher relief. Climate is temperate, but surface water is often scarce, stone for tool-making rare, game dispersed.


1949 ◽  
Vol 14 (3) ◽  
pp. 172-194 ◽  
Author(s):  
Wesley R. Hurt ◽  
Daniel McKnight

The San Augustin Plains of south central New Mexico contain several pluvial lake basins, on the terraces of which are numerous blowout sites with remains of Early Man. The major portion of the Plains lies to the south of U.S. Highway 60, between Magdalena and Datil, New Mexico. This is the area of the basin of extinct Lake San Augustin. The small portion of the Plains to the north of the highway contains the basins of White Lake and North Lake. The Plains consist of a large basin some 60 miles long from northeast to southwest, varying in width from 20 miles at the northeast end to about 6 miles at the southwest. On three sides of the Plains are a series of mountain ranges, while on the west are the ranges that form the continental divide (Fig. 41).


1987 ◽  
Author(s):  
R A Jamieson ◽  
P Tallman ◽  
J A Marcotte ◽  
H E Plint ◽  
K A Connors

1989 ◽  
Vol 26 (10) ◽  
pp. 2081-2091 ◽  
Author(s):  
P. H. Reynolds ◽  
R. A. Jamieson ◽  
S. M. Barr ◽  
R. P. Raeside

Forty new 40Ar/39Ar age spectra on micas and amphiboles from both granitic and metamorphic rocks show that two geologically distinct terranes in the Cape Breton Highlands (Nova Scotia) have had contrasting thermal histories. Some plutons in the Bras d'Or Terrane in the southeastern highlands apparently cooled through the hornblende (or muscovite) closure temperature immediately following Precambrian to Cambrian intrusion. Other rock units in this terrane, particularly in the west, have been variably overprinted by a Silurian tectonothermal event, probably associated with juxtaposition of the Bras d'Or Terrane with the Aspy Terrane to the northwest. Gneisses at Kellys Mountain in the southeastern Bras d'Or Terrane apparently were not overprinted by this event.Argon data from the Aspy Terrane suggest that Silurian deposition, deformation, and metamorphism were followed by rapid cooling through hornblende and biotite closure temperatures in the Middle Devonian. This probably resulted from uplift and exhumation of the terrane as it collided with the Appalachian Orogen to the northwest. The Cheticamp Pluton in the western part of the Aspy Terrane, which does not appear to have been significantly affected by Silurian–Devonian tectonothermal events, may represent an outlier of the Bras d'Or Terrane. The Aspy Terrane records an Acadian tectonothermal history similar to that of the Gander Zone in southwestern Newfoundland.


1894 ◽  
Vol 38 (984supp) ◽  
pp. 15724-15725
Author(s):  
Hugh Fletcher
Keyword(s):  

2007 ◽  
Vol 30 (5) ◽  
pp. 279-286 ◽  
Author(s):  
David J. Mossman ◽  
James D. Duivenvoorden ◽  
Fenton M. Isenor

Author(s):  
Esraa Aladdin Noori ◽  
Nasser Zain AlAbidine Ahmed

The Russian-American relations have undergone many stages of conflict and competition over cooperation that have left their mark on the international balance of power in the Middle East. The Iraqi and Syrian crises are a detailed development in the Middle East region. The Middle East region has allowed some regional and international conflicts to intensify, with the expansion of the geopolitical circle, which, if applied strategically to the Middle East region, covers the area between Afghanistan and East Asia, From the north to the Maghreb to the west and to the Sudan and the Greater Sahara to the south, its strategic importance will seem clear. It is the main lifeline of the Western world.


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