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Fashion in the period 1600–1650 in Western clothing is characterized by the disappearance of the ruff in favour of broad lace or linen collars. Waistlines rose through the period for both men and women. Other notable fashions included full, slashed sleeves and tall or broad hats with brims. For men, hose disappeared in favour of breeches.
Fashion in the period 1550–1600 in European clothing was characterized by increased opulence. Contrasting fabrics, slashes, embroidery, applied trims, and other forms of surface ornamentation remained prominent. The wide silhouette, conical for women with breadth at the hips and broadly square for men with width at the shoulders had reached ...
The Infanta Margarita of Spain is shown here wearing a mourning dress of unrelieved black with long sleeves, cloak and hood. She wears her hair parted to one side and severely bound in braids, 1666. Two English ladies wear dresses with short sleeves over chemise sleeves gathered into three puffs. The long bodice front with curving bands of ...
Overview of fashion from The New Student's Reference Work, 1914. Summary of women's fashion silhouet changes, 1794–1887. The following is a chronological list of articles covering the history of Western fashion—the story of the changing fashions in clothing in countries under influence of the Western worldâ —from the 5th century to the present.
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A ruff from the early 17th century: detail from The Regentesses of St Elizabeth Hospital, Haarlem, by Verspronck A ruff from the 1620s. A ruff is an item of clothing worn in Western, Central and Northern Europe, as well as Spanish America, from the mid-16th century to the mid-17th century.
For the private reception at Eaton Hall, Princess Eugenie wore Saloni's embroidered Lea dress, in black. (Though that color is sold out, but the brand makes it in many other colors.)She carried an ...
Portrait of the family of Sir Thomas More shows English fashions around 1528.. Fashion in the period 1500–1550 in Europe is marked by very thick, big and voluminous clothing worn in an abundance of layers (one reaction to the cooling temperatures of the Little Ice Age, especially in Northern Europe and the British Isles).
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