Case Study - The Holderness Coast

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  • Holderness Coast
    • Location
      • It's found along the East Coast of England
      • It's found between Flamborough Head (North) and Spurn Head (south), with Mappleton in the middle
      • It erodes by 2 metres per year because till is made from bedrock from glaciers
    • Geology
      • The chalk is very resistant rock, however, the clay is very neasily eroded
      • The processes of erosion are hydraulic action, freeze-thaw, abrasion, solution and carbonation
    • Spurn Head
      • 6 Km long spit, caused by wind, waves and river estuary
    • Mappleton
      • Lies upon unconsolidated till, which is soft and erodes quickly
    • Flamborough Head
      • Many features e.g. arches, wave-cut platforms and caves
      • Chalk rock (not easily eroded)
    • Impacts
      • Enironmental
        • SSSI are threatened e.g. lagoons South of Easington
        • Groynes make beaches narrow in other areas
        • Rising sea levels threaten coastline more
      • Economic
        • Caravan  sites have had to expand inland
        • Property prices have dropped, insurance is difficult to get at Mappleton
      • Social
        • B1242 was nearly lost
        • Mappleton could be 30th village to be lost to sea
        • Homes near cliffs at Skipsea are at risk of collapsing into sea

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