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CANYNGES
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Source
Encyclopaedia Britannica (1911) / britannica_1911
License
public_domain
Chunk ID
1911:canynges:b042909cb273
Section
Hash Algorithm
sha256
Stored Hash
2e49741bb0034711e799de9c3d2b4f9e5380a65741cce907249abbaf2912830d
Computed Hash
2e49741bb0034711e799de9c3d2b4f9e5380a65741cce907249abbaf2912830d
Normalizer
ggnorm 1.0
Observed
2026-02-08 18:42:34
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Verified Text
canynges, canynge, william (c. 1399-1474), english merchant, was born at bristol in 1399 or 1400, a member of a wealthy family of merchants and cloth-manufacturers in that city. he entered, and in due course greatly extended, the family business, becoming one of the richest englishmen of his day. canynges was five times mayor of, and twice member of parliament for, bristol. he owned a fleet of ten ships, the largest hitherto known in england, and employed, it is said, 800 seamen. by special license from the king of denmark he enjoyed for some time a monopoly of the fish trade between iceland, finland and england, and he also competed successfully with the flemish merchants in the baltic, obtaining a large share of their business. in 1456 he entertained margaret of anjou at bristol, and in 1461 edward iv. canynges undertook at his own expense the great work of rebuilding the famous bristol church of st mary, redcliffe, and for a long time had a hundred workmen in his regular service for this purpose. in 1467 he himself took holy orders, and in 1469 was made dean of westbury. he died in 1474. the statesman george canning and the first viscount stratford de redcliffe were descendants of his family. see pryce, _memorials of the canynges family and their times_ (bristol, 1854). canyon (anglicized form of span. _canon_, a tube, pipe or cannon; the spanish form being also frequently written), a type of valley with huge precipitous sides, such as the grand canyons of the colorado and the yellowstone livers, and the gorge of the niagara river below the falls, due to rapid stream erosion in a "young" land. a river saws its channel vertically downwards, and a swift stream erodes chiefly at the bottom. in rainy regions the valleys thus formed are widened out by slope-wash and the resultant valley-slopes are gentle, but in arid regions there is very little side-extension of the valleys and the river cuts its way downwards, leaving almost vertical cliffs above the stream. if the stream be swift as in the western plateau of north america, the cutting action will be rapid. the ideal conditions for developing a canyon are: great altitude and slope causing swift streams, arid conditions with absence of side-wash, and hard rock horizontally bedded which will hold the walls up.