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The map is possibly the first recorded use of the term English Channel and the description suggests the name had recently been adopted. [ 9 ] In the sixteenth century, Dutch maps referred to the sea as the Engelse Kanaal (English Channel) and by the 1590s, William Shakespeare used the word Channel in his history plays of Henry VI , suggesting ...
Geologic map of southeast England and the region around the English Channel, showing the Weald-Artois anticline in its regional context. Cross-section over the Wealden 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 ...
English: Geologic map of southeastern England, the English Channel and Pays-de-Calais. Based on: British Geological Survey ; 2005 : Bedrock geology UK South, 1:625 000 scale (5 th ed.), HarperCollins Publishers Ltd.
The sediments were uplifted and faulted within the Variscan Orogeny, with the land now occupied by the Weald Basin being a low external fold belt to the main orogeny, which was located within the present day English Channel. [2] The remnants of the mountain belt can be seen today in Devon and Cornwall in what is known as the Cornubian Massif.
Though pitted by troughs and rivers, the English Channel was almost mainly land at the height of the last ice age. [6] The predominant geology of both and of the seafloor is chalk. Although somewhat resistant to erosion, erosion of both coasts has created the famous white cliffs of Dover in the UK and the Cap Blanc Nez in France.
Hurd Deep running from bottom left to top right of an extract from a 1955 Admiralty Chart 1955 Admiralty Chart No 2649 showing Hurd Deep in the context of the English Channel. Hurd's Deep (or Hurd Deep) is an underwater valley in the English Channel, northwest of the Channel Islands. Its maximum depth is about 180 m (590 ft; 98 fathoms), making ...
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.
The Hampshire Basin is the traditional name for the landward section of a basin underlying the northern English Channel and much of central southern England, known more fully as the Hampshire-Dieppe Basin. It stretches a little over 100 miles (160 km) from the Dorchester area in the west to Beachy Head in the east.