Do cave sizes change from west to east in Pegwell Bay?

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5th form GCSE Geography Coursework

Do cave sizes change from west to east in Pegwell Bay?

A project to investigate rates of erosion in the chalk cliffs of Pegwell Bay, East Kent.

Introduction

About 20 well-formed caves show that active wave erosion is taking place along this coastline between the old seaweed tunnel and the sea-wall in Pegwell Cove. The cliff is about 15 metres high in the west (tunnel end) rising to 20 metres in the east (Pegwell Cove) Cliffs are made of well-jointed Chalk with few flints, but many faultlines. Faults, once exposed, form distinct lines of weakness, which are easily exploited in hydraulic action, abrasion, attrition and corrosion to form caves. The cliff face retreats at about 25cm per year, but in the more exposed eastern end, erosion is faster than this. In this western end (towards the old hoverport) erosion is slower.

The main rock in Pegwell bay is chalk, overlain by the later Thanet Formation. There is an age gap between the two layers of rock, which took place some 60-80 millions years ago, as earth movements raised the chalk out of the sea. Later, the sea rose again, and the Thanet beds were laid down on the eroded chalk surface. When chalk is weakened by faults, wave erosion has resulted in the formation of caves in the cliffs. Another feature, which can be seen in the cliffs, is brickearth. This was formed of wind-blown silt deposited over the ice-free plains on the edge of the ice-sheets.

The 2 basic things controlling wave erosion of the cliffs are:

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  1. Wave strength
  2. Rock resistance

Wave strength can cause different sizes of caves because different place have different wave strength. If the wave strength is greater then the cliff will erode faster.

Rock resistance also controls wave erosion of the cliffs. Rocks vary in hardness. Softer rock will erode faster and harder rock will erode slower. Rocks are of different hardness because rocks are of different types. They can be sedimentary, igneous or metamorphic. It also cause by the density and the age of rocks.

Thanet is in the south east corner of the UK ...

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