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  2. Weald Basin - Wikipedia

    en.wikipedia.org/wiki/Weald_Basin

    The Weald Basin (/ ˈ w iː l d /) is a major topographic feature of the area that is now southern England and northern France from the Triassic to the Late Cretaceous. Its uplift in the Late Cretaceous marked the formation of the Wealden Anticline .

  3. Weald–Artois Anticline - Wikipedia

    en.wikipedia.org/wiki/Weald–Artois_Anticline

    The Weald–Artois Anticline, or Wealden Anticline, is a large anticline, a geological structure running between the regions of the Weald in southern England and Artois in northern France. The fold formed during the Alpine orogeny , from the late Oligocene to middle Miocene as an uplifted form of the Weald basin through inversion of the basin.

  4. Weald - Wikipedia

    en.wikipedia.org/wiki/Weald

    The name "Weald" is derived from the Old English weald, meaning "forest" (cognate of German Wald, but unrelated to English "wood"). This comes from a Germanic root of the same meaning, and ultimately from Indo-European. Weald is specifically a West Saxon form; wold is the Anglian form of the word. [1]

  5. Boulonnais (land area) - Wikipedia

    en.wikipedia.org/wiki/Boulonnais_(land_area)

    It is a well-wooded zone almost entirely within the Caps et Marais d'Opale Regional Natural Park and is the east end of the Weald-Artois Anticline. [1] [2] Its coast all faces west to the English Channel (la Manche), apart from a short north coast, including the small beach of Cap Gris-Nez which faces the Strait of Dover ("le Pas de Calais ...

  6. Geology of East Sussex - Wikipedia

    en.wikipedia.org/wiki/Geology_of_East_Sussex

    For much of its history the Weald had been slowly subsiding basin, but the growth of the Alpine Chain to the south during the Cenozoic caused a reactivation of the Variscan basement basin-bounding faults, the rocks were arched into a broad anticline which stretched across the English Channel to Northern France, the Weald–Artois anticline.

  7. Greensand Ridge - Wikipedia

    en.wikipedia.org/wiki/Greensand_Ridge

    The Greensand Ridge, formed of Lower Greensand, much of which is sandstone and where hardest is locally termed Bargate stone, is a remnant of the Weald dome, part of the great Weald-Artois Anticline that runs from south-east England into northern France. The Weald dome consists of a series of geological strata laid down in the Cretaceous that ...

  8. Wealden cloth industry - Wikipedia

    en.wikipedia.org/wiki/Wealden_cloth_industry

    Cloth-making was, apart from iron-making, the other large-scale industry carried out on the Weald of Kent and Sussex in medieval times. The ready availability of wool from the sheep of the Romney Marsh, and the immigration from Flanders in the fourteenth century of cloth-workers – places like Cranbrook attracted hundreds of such skilled workers – ensured its place in Kentish industrial ...

  9. William of Cassingham - Wikipedia

    en.wikipedia.org/wiki/William_of_Cassingham

    William of Cassingham (or Willikin of the Weald) (died 1257) was a country squire of Cassingham (now Kensham) in Kent at the time of the First Barons' War. During that conflict, he raised a guerrilla force of archers which opposed the otherwise total occupation of the south-east by Prince Louis of France .