Coastlal landforms caused by deposition (beaches)

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  • Created on: 11-03-17 11:07
Formation of beaches ONE
Beaches are found on coasts between the high water mark and the low water mark.
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Formation of beaches TWO
They'r fomed by constructive waves depositing material like sand and shingle.
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Sand characteristics
Sand beaaches are flat and wide- sand particles are small and the weak backwash can move them back down the beach, creating a long gentle slope.
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Shingle characteristics
Shingle beaches are steep and narrow - shingle particless are large annd the weak backwash can't move them back down the beach. The shingle particles build up and create a steep slope.
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Spits ONE
Spits form at sharp bends in the coastline.
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Spits TWO
Longshore drift transports sand and shingle past the bendand deposits into the sea.
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Spits THREE
Strong winds and waves can curve the end of the spit.
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Spits FOUR
The sheltered area behind the spit is protected from waves- lots of material accumilates in this area, which means plants can grow there.
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Spits FIVE
Overtime, the sheltered area can become a mud flat or a salt marsh.
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Bars ONE
A bar is formed when a spit joins two headlands together.
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Bars TWO
The bar cuts off the bay between the headlands from the sea.
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Bars THREE
This means a lagoon can form behind the bar.
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Bars FOUR
A bar that connects the shore to an island is called a tombolo.
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Other cards in this set

Card 2

Front

Formation of beaches TWO

Back

They'r fomed by constructive waves depositing material like sand and shingle.

Card 3

Front

Sand characteristics

Back

Preview of the front of card 3

Card 4

Front

Shingle characteristics

Back

Preview of the front of card 4

Card 5

Front

Spits ONE

Back

Preview of the front of card 5
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