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  2. Category:Sandbanks of the North Sea - Wikipedia

    en.wikipedia.org/wiki/Category:Sandbanks_of_the...

    Pages in category "Sandbanks of the North Sea" The following 25 pages are in this category, out of 25 total. This list may not reflect recent changes. C.

  3. List of shoals and sandbanks in the southern North Sea

    en.wikipedia.org/wiki/List_of_shoals_and...

    Water flows parallel to the shore and this is reflected in the orientation of sandbanks. Typically, sandbanks of the English Channel and southern North Sea rise 10 to 25 m above the sea floor and are 10 to 30 km long and 1 to 3 km wide. [2] [1] [3] The volume of material in some of the banks has been estimated at between 70 and 1100 Million m 3 ...

  4. Shoal - Wikipedia

    en.wikipedia.org/wiki/Shoal

    Shoals can appear as a coastal landform in the sea, where they are classified as a type of ocean bank, or as fluvial landforms in rivers, streams, and lakes. A shoal–sandbar may seasonally separate a smaller body of water from the sea, such as: Marine lagoons; Brackish water estuaries; Freshwater seasonal stream and river mouths and deltas.

  5. Inner and Outer Dowsing sand banks - Wikipedia

    en.wikipedia.org/wiki/Inner_and_Outer_Dowsing...

    The centre of the bank is about 13 km north-east off Ingoldmells Point, Lincolnshire. The water depth ranges from 1 m to 30 m below sea-level. [1] The Inner Dowsing Bank together with the adjacent Race Bank and North Ridge Bank have been designated a Special Area of Conservation (SAC) and a Marine Protected Area (MPA). [1]

  6. Dogger Bank - Wikipedia

    en.wikipedia.org/wiki/Dogger_Bank

    Dogger Bank (Dutch: Doggersbank, German: Doggerbank, Danish: Doggerbanke) is a large sandbank in a shallow area of the North Sea about 100 kilometres (62 mi) off the east coast of England. During the last ice age, the bank was part of a large landmass connecting mainland Europe and the British Isles , now known as Doggerland .

  7. Doggerland - Wikipedia

    en.wikipedia.org/wiki/Doggerland

    During the most recent glaciation of the Last Glacial Maximum, the North Sea and much of the British Isles were covered with glacial ice, and the sea level was about 120 m (390 ft) lower. The climate later became warmer, and around 12,000 BCE, Great Britain, as well as much of the North Sea and the English Channel, was an expanse of low-lying ...

  8. Why are houses falling into the sea in Rodanthe, North ... - AOL

    www.aol.com/why-houses-falling-sea-rodanthe...

    A portion of debris from the collapsed house at 23039 G A Kohler Court is shown near houses at 23047 G A Kohler Court and 23237 Sea Oats Drive in Rodanthe.

  9. Cleaver Bank - Wikipedia

    en.wikipedia.org/wiki/Cleaver_Bank

    The Cleaver Bank (Dutch: Klaverbank) is a sandbank in the North Sea about 160 kilometres (99 miles) off the west coast of the Netherlands and south of the Dogger Bank. The size of the bank is about 1235 km 2. The bank is 30-40 metres below sea level. [1]