By Stephen Brunt
This nation and its everyone is made up of an analogous hardy stuff that makes our video game and our league. the gray Cup has helped unite our nation for a hundred years now. And it has published us, outfitted our delight and our experience of Canadianness in annual tributes to attempt, sweat and toil. yet what does a hundred years of historical past and cultural relevance upload as much as? after we Canadians examine the gray Cup, we see way over a sparkling soccer trophy; we see a mirrored image of ourselves. After its first years as an novice problem cup, the gray Cup could cross directly to be presented to the simplest soccer workforce in Canada, with Western challengers touring again east to fall by the hands of the extra confirmed Toronto groups. that's, until eventually a gaggle of pissed off Winnipeggers paid a tremendous sum through the melancholy to shop for up superstar avid gamers and convey the cup west for the 1st time. Following this, the video games turned concerning the satisfaction of the rustic, East as opposed to West, the nationwide id fought over the gridiron, all chronicled dutifully through bestselling writer Stephen Brunt.
From the start of the fashionable CFL in 1958, in the course of the dynastic Edmonton Eskimos and into the nineties, tried united states growth, franchise re-birth in Montreal, 100 gray Cups has all of it: behind-the-scene anecdotes, never-before-seen photos, and unparalleled entry to the CFL information. it's a must-have for all enthusiasts of this nationwide culture
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Additional info for 100 Grey Cups: This Is Our Game
This succession includes suprasedimentary and volcanic rocks for the supergroup and a complex island-arc environment for the rocks of the magmatic subduction-zone type ophiolites along the Niagara fault zone [Schulz, 1987b], calc-alkaline basalt-andesite-rhyolite with terrane. oceanic-arc affinities, and local, bimodal, high-A1203 basaltThe Wisconsin magmatic terrane is separated from the rhyolite suites with associated massive sulfide deposits. ,A. Marquette Range Supergroup by·the Niagara fault zone (Fig.
Oo CONGLOMERATE, CONGLOMERATE 0 SANDSTONE, ARGILLITE 'j f'f j FIGURE 2-7 Generalized Geologic Column of the Reany Creek FOffilation. The left column is modifed from Puffett . Lithologies are simplified on this diagram, which emphasizes the presence of loadstones and dropstones. T145: 25 In contrast to the views of Ojakangas and others, Mattson and Cambray  have interpreted the Reany Creek as a mass-flow deposit. Certainly some of the conglomerate beds and some of the homogeneous pebbly argillites could have originated by mass-flow processes active near the margin of a melting glacier.
Axes of maximum elongation in fold/thrust system that here ramps off the Amasa uplift to the defonned clasts plunge 600 toward the south, parallel to the mineral lineation. south. The south-verging drag folds are more difficult to The defonnation shown in this outcrop is totally different explain. They may have been caused by interbed slip on the from that previously obselVed. A subhorizontal foliation is limb of a larger fold, or they may be part of a south-verging fold/thrust system that fonned in response to an abrupt change lacking, as is any evidence for a southward structural vergence.