An Investigation into Sediment Transport along a Beach and The Ways in Which Coastal Processes Such as Transport are Managed.

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An Investigation into Sediment Transport along a Beach and The Ways in Which Coastal Processes Such as Transport are Managed.

A student wanted to examine a shingle beach that was located between two headlands. She wanted to see if the pebbles at one end of the beach were any different to the pebbles at the other end. She thought she would look at the size and shape of the pebbles. She collected 50 pebbles at each end of the beach. Below is a plan of the beach.

The pupil's results taken from sites 1 and 2 showed.

Site 1 Pebble Size

Site 2 Pebble Size

0-4cms

4

0-4cms

1

5-9cms

7

5-9cms

4

0-14cms

2

0-14cms

2

5-19cms

0

5-19cms

3

20-24cms

1

20-24cms

0

25-30cms

5

25-30cms

0

More than 30cms

More than 30cms

0

Site 1 Pebble Shape

Site 2 Pebble Shape

Very Angular

4

Very Angular

2

Angular

30

Angular

4

Rounded

6

Rounded

26

Very Rounded

0

Very Rounded

8

Analyses 1:

What is the Nature of Sediment Transport on this Beach?

These graphs show the pebble sizes taken from sites 1 and 2. As you can see they are both different sets of results from one end of the beach to the other. Site 1 had a wide range of result from 1cm - over 30cms whereas site 2 has a lower range of results from 1cm - 19cms, this shows that site 2 (which is further up the beach) has smaller pebbles than site 1.
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These graphs show that the pebble shapes are very different between the sites. At site 1 the pebbles were mostly angular with no very rounded pebbles, but site 2 had over 30% very rounded and over 50% of them rounded.

The differences between the sites is because of coastal erosion which happens along every coast all over the world.

The four types of erosion are:

Hydraulic power - the sheer force of the waves crashing against cliffs ? air and water trapped in cracks is compressed ? pressure increases ? rock fractures explosively.

Corrasion/Abrasion ...

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