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Printable version; Page information; ... Exhibit in the Textile Museum of Canada, 55 Centre Avenue, Toronto, Ontario, Canada. Photography was permitted in the museum ...
As the access to materials increased, competition to design the most beautiful patterns rose, with an estimate of over 300 different kogin-zashi patterns being created. In the 20th century, the craft of kogin-zashi was streamlined, establishing the three general types that are seen today: nishi-kogin , higashi-kogin , and mishima-kogin . [ 2 ]
Many sashiko patterns were derived from Chinese designs, but just as many were developed by native Japanese embroiderers; for example, the style known as kogin-zashi, which generally consists of diamond-shaped patterns in horizontal rows, is a distinctive variety of sashiko that was developed in Aomori Prefecture.
In fur trade days the Missinaibi was the main route between James Bay and Lake Superior. The route was: James Bay, Moose Factory, Moose River, Missinaibi River, Missinaibi Lake, portage probably via Crooked Lake, Dog Lake, Michipicoten River to Fort Michipicoten on Lake Superior. Trade was contested by the English from the north and the French ...
During the Woodland period, Cree and Ojibwe peoples travelled Missinaibi Lake as part of their waterway network linking the Great Lakes with James Bay.French explorers Pierre-Esprit Radisson and Médard Chouart des Groseilliers may have passed the lake during their Lake Superior expedition of 1659, while the first written record about the lake is a French account from 1666.
Not all National Topographic System maps strictly follow the National Tiling System's linear grid. Some maps also, as an "overedge", cover land in an area which would otherwise be covered by an adjacent map sheet, simply because the latter area does not contain enough land in Canada to warrant a separate printing. [4] [clarification needed]
[1] The formation lies within Missinaibi Provincial Park. [2] It was first identified by geologists in the late 19th century. [3] The Missinaibi Formation is principally known for having nonglacial sediments, which means that dating the formation has helped scientists track the ebb and flow of glacial activity in the region. [1] [3]
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