Norfolk Coast Water and landforms

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NORFOLK COAST                                Water & Landforms        

Case Study of:

  • Landform management scheme
  • Landforms affecting people’s activities

Landforms at Sidestrand / Overstrand Cromer

We studied 2 landforms

  1. Cliffs
  2. Beach

Solid geology along this stretch of coast is chalk (at Overstrand chalk lies about 5 metres below the beach level). Above the chalk lie superficial deposits of unconsolidated glacial deposits: sands, gravels and clays. These are visible in cliffs. The beach is made up of sand, pebbles, cobbles, flints which have been washed along the coast. These accumulate to form a beach.

How were the cliffs formed ?

Cliffs at Overstrand & Cromer about 60 – 70 metres high. Materials transported by ice sheets over the last two million years. The ice sheets eroded transported & deposited rock material of different kinds. The main material is glacial till, tougher, grey, sandy boulder clays, outwash from glaciers in Scotland and Scandinavia.

Some tills have remains of pebbles of chalk, flints, quartz.

On melting & retreat of glaciers some left in sheet form, some in ridges e.g Cromer Ridge (glacial sands and gravels ....outwash). Active melting gave floodwater which could carry materials further from the snout of the glacier.finer clays carried away from snout & sedimented in basins of water away from the snout.

The cliffs in this area were laid down like this. Fine soft texture. Note thin bands of harder material can be seen in the cliff at some places ....perhaps where heavier sands/gravel materials were carried further in a time of greater melting due to higher temperatures.

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How was the beach formed ?

Materials are broken up by the sea eroding cliffs. The erosion of cliffs takes place through

  • attrition,
  • corrasion,
  • undercutting,
  • abrasion
  • solution

Once material is eroded it is transported along the coast and deposited. This is a process called Longshore Drift. Material is washed up the beach at the angle of the waves but comes back down the beach at right angles. When wave direction is at an angle (not at right angles) this leads to a movement along the coast, like a saw tooth motion. The movement ...

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