9 resultados para Indian textile fabrics
em Brock University, Canada
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An ad extolling the benefits of the Lightning Zephyr nylon zipper. This ad was directed towards the garment industry.
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The Horwood Peninsula - Gander Bay area is located at NE Newfoundland in the Botwood Zone (Williams et a1., 1974) or in the Dunnage Zone (Williams, 1979) of the Central Mobile Belt of the Newfoundland Appalachians. The area is underlain by Middle Ordovician to possible Lower Silurian rocks of the Davidsville and Indian Islands Groups, respectively. Three conformable formations named informally : the Mafic Volcanic Formation, the Greywacke and Siltstone Formation and the Black Slate Formation, have been recognized in the Davidsville Group. The Greywacke and the Black Slate Formations pass locally into a Melange Formation. From consideration of regional structure and abundant locally-derived mafic volcanic olisto- 1iths in the melange, it is considered to have originated by gravity sliding rather than thrusting. Four formations have been recognized in the Indian Islands Group. They mainly contain silty slate and phyllite, grey cherty siltstone, green to red micaceous siltstone and limestone horizons. Repetition of lithological units by F1 folding are well-demonstrated in one of formations in this Group. The major structure in this Group on the Horwood Peninsula is interpreted to be a synclinal complex. The lithology of this Group is different from the Botwood Group to the west and is probably Late Ordovician and/or Early Silurian in age. The effects of soft-sediment deformation can be seen from the lower part of the Davidsville Group to the middle part of the Indian Islands Group indicating continuous and/or episodic slumping and sliding activities throughout the whole area. However, no siginificant depOSitional and tectonic break that could be assigned to the Taconian Orogeny has been recognized in this study. Three periods of tectonic deformation were produced by the Acadian Orogeny. Double boudinage in thin dikes indicates a southeast-northwest sub-horizontal compression and main northeast-southwest sub-horizontal extension during the D1 deformation. A penetrative, axial planar slaty cleavage (Sl) and tight to isocJ.ina1 F1 folds are products of this deformation. The D2 and D3 deformations formed S2 and S3 fabrics associated with crenulations and kink bands which are well-shown in the slates and phyllites of the Indian Islands Group. The D2 and D3 deformations are the products of vertical and northeast-southwest horizontal shortening respectively. The inferred fault between the Ordovician slates (Davidsville Group) and the siltstones (Indian Islands Group) suggested by Williams (1963, 1964b, 1972, 1978) is absent. Formations can be followed without displacement across this inferred fault. Chemically, the pillow lavas, mafic agglomerates, tuff beds and diabase dikes are subdivided into three rock suites : (a) basaltic komatiite (Beaver Cove Assemblage), (b) tholeiitic basalt (diabase dikes), (c) alkaline basalt (Shoal Bay Assemblage). The high Ti02 , MgO, Ni contents and bimodal characteristic of the basaltic komatiite in the area are comparable to the Svartenhuk Peninsula at Baffin Bay and are interpreted to be the result of an abortive volcano-tectonic rift-zone in a rear-arc basin. Modal and chemical analyses of greywackes and siltstones show the trend of maturity of these rocks increasing from poorly sorted Ordovician greywackes to fairly well-sorted Silurian siltstones. Rock fragments in greywackes indicate source areas consisting of plagiogranite, low grade metamorphic rocks and ultramafic rocks. Rare sedimentary structures in both Groups indicate a southeasterly provenance. Trace element analyses of greywackes also reveal a possible island-arc affinity.
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Reprint of the 1810 ed. printed by Samuel Wood, New York,
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In September 1968, the Indian Affairs Branch of Canada within the Department of Indian Affairs and Northern Development (DIAND), ceased to exist as a result of a major reorganization. In its place the Indian and Eskimo Affairs Program emerged including elements from both the former Indian Affairs and Northern Administration branches. This new structure was based on function rather than on geographic location or ethnic origin. The Program included the areas within the Department responsible for adminstration of; education, social, cultural, community and economic development as well as statutory commitments. After 1978 the Program became known as the Indian and Inuit Affairs Program (IIAP).
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Reprint of the 1810 ed. printed by Samuel Wood, New York, Reprinted by Ipswich By J. Bush, Tavern-Street
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Receipt from James D. Tait of St. Catharines for fabrics and trims, Aug. 24, 1886.
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Receipt from John Henderson and Co., Manufacturers of Hats, Caps and Furs and dealers in Indian Curiosities, Montreal for furs and buttons, Oct. 13, 1887.
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Certificate, 51 cm. x 75 cm. with a coloured picture of the Colonial and Indian Exhibition in London, 1886. This was presented with a commemorative medal to Henry Pafford who was the Mayor of Niagara-on-the-Lake 1863-74, 1876-1880 and 1888-1896. He also ran a drug store and a fruit farm. The award is signed by the Executive President and Secretary to the Royal Commission. [There is no indication what the award is for and the medal is not included in this collection], n.d.
Resumo:
Certificate, 51 cm. x 75 cm. with a coloured picture of the Colonial and Indian Exhibition in London, 1886. This was presented with a commemorative medal to W. Woodruff. The award is signed by the Executive President and Secretary to the Royal Commission. [There is no indication what the award is for and the medal is not included in this collection], n.d.