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Blueschist on Île de Groix, France Photomicrograph of a thin section of blueschist facies metamorphosed basalt, from Sivrihisar, Turkey. Blueschist (/ ˈ b l uː ʃ ɪ s t /), also called glaucophane schist, is a metavolcanic rock [1] that forms by the metamorphism of basalt and rocks with similar composition at high pressures and low temperatures (200–500 °C (392–932 °F ...
Belts have been documented as male clothing since the Bronze Age. Both sexes have used them off and on, depending on the fashion trends. In the western world, belts have been more common for men, with the exception of the early Middle Ages, late 17th century Mantua, and skirt/blouse combinations between 1901 and 1910.
BS 6185:1982 Specification for size designation of men's wear BS 3666:1982, the standard for women's clothing, is rarely followed by manufacturers as it defines sizes in terms of hip and bust measurements only within a limited range.
The metamorphic grade is a blueschist facies, which results from tectonic deformation by the subduction of the African Plate beneath the Eurasian Plate. Subduction occurred between the Oligocene and the Miocene , and the metamorphic grade represents the southernmost extent of the Cycladic blueschist belt.
After losing popularity during World War I, when men became accustomed to uniform belts, suspenders were still regular attire throughout the 1920s. Because of their image as 'underwear', [6] some men switched to belts during the 1930s as the vests (US/Canada) or waistcoats which had hidden suspenders became worn less often. This also signaled ...
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