Brie (/briː/; French: [bʁi]) is a soft cow's milk cheese named after Brie, the French region from which it originated (roughly corresponding to the modern département of Seine-et-Marne). It is pale in color with a slight grayish tinge under a rind of white mold. The whitish moldy rind is typically eaten, with its flavor depending largely upon the ingredients used and its manufacturing environment.

Production

Brie may be produced from whole or semi-skimmed milk. The curd is obtained by adding rennet to raw milk and warming it to a maximum temperature of 37 °C (99 °F). The cheese is then cast into molds, sometimes with a traditional perforated ladle called a pelle à brie. The 20 cm (8 in) mold is filled with several thin layers of cheese and drained for approximately 18 hours. The cheese is then taken out of the molds, salted, inoculated with cheese mold (Penicillium candidum, Penicillium camemberti) or Brevibacterium linens, and aged in a cellar for at least four to five weeks.

If left to mature for longer, typically several months to a year, the cheese becomes stronger in flavor and taste, the pâte drier and darker, and the rind also darker and crumbly, and it is called Brie Noir (French for "black brie"). Around the Île-de-France where brie is made, people enjoy soaking this in café au lait and eating it for breakfast.

Brie is both a given name and a surname. Notable people with the name include:

See also

Brie is a historic region of northern France notable in modern times for Brie cheese. It was once divided into three sections ruled by different feudal lords: the western Brie française, corresponding roughly to the modern department of Seine-et-Marne in the Île-de-France region; the eastern Brie champenoise, forming a portion of the modern department of Marne in the historic region of Champagne (part of modern-day Champagne-Ardenne); and the northern Brie pouilleuse, forming part of the modern department of Aisne in Picardy.

The Brie forms a plateau with few eminences, varying in altitude between roughly 100–150 metres (325–500 ft) in the west, and 150–200 metres (500–650 ft) in the east. Its scenery is varied by forests of some size—the chief being the Forêt de Sénart, the Forêt de Crécy-la-Chapelle, and the Forêt d'Armainvilliers. The surface soil is clay in which are embedded fragments of siliceous sandstone, used for millstones and constructional purposes; the subsoil is limestone. The Marne and its tributaries the Grand Morin and the Petit Morin are the chief rivers, but the region is not abundantly watered and the rainfall is only between 50–60 centimetres (20–24 in).