the work of the sea

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The Work of the Sea

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Junior Cert Geography slides on the work and activity of the Sea - coastal processes, coastal erosion, coastal deposition and features.

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Page 1: The Work of the Sea

The Work of the Sea

Page 2: The Work of the Sea

Erosion – rocks are worn down and broken into smaller rocks

Transportation – rocks and sand are moved from one area to another by waves and sea currents

Deposition – material is deposited (dropped) in some areas, forming beaches and sand dunes

Processes at work in the Sea

Page 3: The Work of the Sea

Hydraulic Action – force of moving water Compressed Air – air gets trapped in rock, the pressure

of the air can crack rock Abrasion – rocks and stones can be thrown against the

coastline, wearing it away Attrition – rocks and stones are worn down themselves

How Waves Erode

Page 4: The Work of the Sea

Name the erosion process?

Page 5: The Work of the Sea

Formation of Bays and Headlands

The hard rock in a coastline erodes more slowly than the soft rock

The hard rock that has not eroded, juts out to the sea, forms a headland. The spaces between the hard rock are known as Bays

BAY

BAY

Headlands

Page 6: The Work of the Sea

Sea Cliffs – Cliffs of Moher

Page 7: The Work of the Sea

Formation of Cliffs – steep parts of the coast

A Cliff is formed when◦ Waves erode the coast and form a small notch.◦ The erosion continues until the notch gets bigger. ◦ The section of rock above the notch cannot be supported

anymore and collapses.◦ The slope becomes steeper◦ A cliff is formed.

◦ The former base of the cliff remains as a wave cut platform.

Page 8: The Work of the Sea

Sea Caves, Sea Arches, Sea Stacks

Page 9: The Work of the Sea

Formation of Sea Caves

A large hole or tunnel at

the base of the Cliff is

called a cave. If there is a weak spot

such as a crack or a joint

in the rock, the waves will

attack it and erode a

passage called a sea cave

Page 10: The Work of the Sea

If a Cave erodes right through a headland (or if two caves erode from each side) an arch is formed

If the roof of an arch collapses, a sea stack is formed The sea stack can eventually be eroded down to a

stump.

Formation of Sea Arches

Page 11: The Work of the Sea

Sea Stack

Page 12: The Work of the Sea

Formation of a Blow Hole

Draw diagram p54

• A blow Hole is a hole which joins the roof of a cave with the surface above.

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Page 14: The Work of the Sea

2011 Junior Cert

Page 15: The Work of the Sea

Transportation by the Sea

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Waves approach the shore at an angle. The swash of each wave pushes material up the beach (A-B). Because of the slant the backwash drags the material straight

down (B-C) The process is repeated so the material is transported (moved)

along in a zig zag pattern.

Long Shore Drift

Page 17: The Work of the Sea

How can you stop Long Shore Drift?

A Groyne is a low wall built into the sea to stop long shore drift.

Page 18: The Work of the Sea

Sea Deposition

A beach is a gently sloping area of sand, pebbles or stones along the shore.

It lies between the high-tide mark and the low-tide mark.

It is formed by the swash pushing materials up the beach and the weaker backwash pulls finer materials back down.

Formation of a Beach:

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A Storm Beach is formed when large stones are deposited at the top of a beach during a storm.

Page 22: The Work of the Sea

Sand Dunes

Sand dunes are mounds of sand at the back of a beach.

Sand dunes are formed because of the wind blowing the sand inland.

Page 23: The Work of the Sea

Marram Grass

Marram grass is long, dry and has long roots.

These roots bind the sand together and protect it from the wind and the rain

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The Formation of a SPIT

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A sand spit is a ridge of sand or shingle that juts out into the sea.

Long shore drift stops when it reaches a bay or sheltered place.

The material may build up gradually to form a spit.

Eg. Portmarnock, Co. Dublin

The formation of a SPIT

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Formation of a SAND BAR

Page 29: The Work of the Sea

A sand bar is a sand spit (explain formation) that stretches across a bay to connect the two sides of the bay.

The lake behind the sand bar is called a lagoon

Example: Lady’s Island, Co. Wexford

Formation of a SAND BAR

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Formation of a TOMBOLO

Page 32: The Work of the Sea

A tombolo is a ridge of sand or shingle that joins an island to the mainland

A tombolo forms when a sand spit juts out into the sea and links with an island

Example: Sutton, Co Dublin

Formation of a TOMBOLO

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Page 34: The Work of the Sea

2012 Ordinary Level Junior Cert

Page 35: The Work of the Sea

2011 Higher Level Junior Cert

Page 36: The Work of the Sea

2010 Junior Cert Higher Level

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Defence: Protecting land and people from erosion

Economic activities: Making money from the sea and its resources.

Interaction with the Sea

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Made of Reinforced Concrete Stops waves from eroding land away Has NO effect on Longshore drift Expensive to build

Defence – Sea Walls

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Also known as “Rock Armour” Simple to build, cheap Can cause safety concerns and look ugly Has NO effect on longshore drift

Defence - Boulders

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Low walls, built at right angles to the coast Made of wood (cheap) or concrete (expensive) Reduce longshore drift

Defence - Groynes

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“Walls” made of wire mesh filled with stones Reduce Erosion Cheap to build – but can cause safety concerns and do not

last too long

Defence - Gabions

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Economic use of the Sea - Fishing

Page 44: The Work of the Sea

Economic Use of the Sea – Tourism/Recreation

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Economic use of the Sea – Wind Energy

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Economic use of the Sea – Wave Energy

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Economic use of the Sea – Fossil Energy

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Litter from people at the coast Overfishing and damage to wildlife Oil Spills and pipe breaks

Misuse of the sea - pollution

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2008 Leaving Cert Higher