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  2. 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.

  3. Weald - Wikipedia

    en.wikipedia.org/wiki/Weald

    The geological map shows the High Weald in lime green (9a). The Low Weald, [18] the periphery of the Weald, is shown as darker green on the map (9), [19] and has an entirely different character. It is in effect the eroded outer edges of the High Weald, revealing a mixture of sandstone outcrops within the underlying clay.

  4. Weald Basin - Wikipedia

    en.wikipedia.org/wiki/Weald_Basin

    The Weald Basin has yielded significant quantities of gypsum from Jurassic Purbeck beds and a number of brickworks exploit the lower Cretaceous clays. The inversion of the Weald Basin throughout the late Cretaceous and early Tertiary resulted in the formation of the Wealden Anticline and a number of smaller anticlines within the larger structure.

  5. Geology of East Sussex - Wikipedia

    en.wikipedia.org/wiki/Geology_of_East_Sussex

    The geology of East Sussex is defined by the Weald–Artois anticline, a 60 kilometres (37 mi) wide and 100 kilometres (62 mi) long fold within which caused the arching up of the chalk into a broad dome within the middle Miocene, [1] which has subsequently been eroded to reveal a lower Cretaceous to Upper Jurassic stratigraphy.

  6. Anticline - Wikipedia

    en.wikipedia.org/wiki/Anticline

    The Weald–Artois Anticline is a major anticline which outcrops in southeast England and northern France. ... Structural Geology and Map Interpretation. Lectures in ...

  7. Doggerland - Wikipedia

    en.wikipedia.org/wiki/Doggerland

    A map showing the hypothetical extent of Doggerland from now back to the Weichselian glaciation. Until the middle Pleistocene, Great Britain was a peninsula of Europe, connected by the massive chalk Weald–Artois Anticline across the Strait of Dover.

  8. 10 Types of Valuable Vintage Maps That Could Be Hiding in ...

    www.aol.com/10-types-valuable-vintage-maps...

    More recently, a World Ortelius map sold for £4,000 (about $5,000) at an auction in 2012. These maps are celebrated for their artistry and the way they reflect the geographical knowledge of the ...

  9. List of geological folds in Great Britain - Wikipedia

    en.wikipedia.org/wiki/List_of_geological_folds...

    Weald Anticline: England Weald-Artois Anticline: England Wealden Anticline: England Brenchley & Rawson 2006 Weeton Anticline: Lancashire England E&W 67 Welbeck Trough: England E&W 112 Werrington Anticline: England Smith et al. 2005 Wessington Anticline: England E&W 112 Westbury Anticline: England E&W 264 West Mainland Anticline: Shetland ...