Lesson Y8-U02-L05
Y8-U02-L05 Depositional Landforms: Beaches, Spits and Bars Quiz: KS3 Geography, Unit 8
20 questions
In partnership with Revision Ninja
Lesson Y8-U02-L05, Depositional Landforms: Beaches, Spits and Bars: 20 multiple choice questions for the KS3 Geography (National Curriculum), Unit 8: Year 8: Coasts: A Changing Landscape, written with Revision Ninja.
Host it live on the board and students join with a game code on their own devices, or revise alone with Free Play. The answers are revealed in the game.
The 20 questions
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What is deposition?
- When the sea drops the material it is carrying because it loses energy
- When sediment is dissolved by weak acid in seawater, so it disappears from view
- When waves wear rock away and carry it off, leaving the cliff face bare and jagged
- When water freezes in cracks and splits the rock, breaking it into smaller pieces
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What is sediment on a coast?
- Water trapped behind a bar or spit
- Hard rock that resists the waves at a headland
- A long ridge of sand joined to the land at one end
- Loose sand, shingle and rock carried along by the sea
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What is a spit?
- A tall pillar of rock left after an arch collapses
- A ridge of sand that grows across a bay and joins two headlands
- A shallow pool of water trapped behind a bar
- A long, narrow ridge of sand or shingle joined to the land at one end
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What is a bar?
- A pool of calm water trapped behind a spit
- A ridge of sand that grows across a bay and joins two headlands
- A ridge joined to the land at one end only
- A curved dip in the coast where soft rock was worn away
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What is a lagoon?
- A shallow pool of water trapped behind a bar or spit
- A curved bay where soft rock has been worn back
- A deep channel carved by the sea into a headland
- A pillar of rock left standing in the sea
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Which type of wave builds a beach up?
- Destructive waves
- Tsunami waves from distant earthquakes
- Constructive waves
- Tidal bores running up river estuaries
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What causes the end of a spit to curve into a hook?
- Hydraulic action forcing cracks in the tip
- Backwash dragging the sand straight back out to sea
- Freeze-thaw weathering of the ridge
- Changing wind directions that push the end round
-
On an OS map, what does pale yellow shading along the coast usually show?
- Solid rock cliffs
- Sand and shingle
- Mud flats left uncovered at low tide
- Deep open water
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Waves lose energy in a sheltered bay and drop sand. Which process is this?
- Solution
- Deposition
- Hydraulic action
- Erosion
-
A destructive wave drags shingle off a beach. Which process is this?
- Erosion
- Deposition
- Mass movement
- Weathering
-
A coastline bends at a river mouth and longshore drift reaches it. What happens to the sediment?
- It is dissolved by the freshwater flowing from the river
- It is frozen in place by winter weather
- It is deposited, building a ridge out into the water
- It is carried straight out to sea by the backwash
-
A ridge grows out from the land and then turns into a hook at its tip. Which landform is this?
- A stump
- A stack
- A spit
- A bar
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A ridge grows all the way across a bay, joining two headlands. What is trapped behind it?
- A stack
- A tributary river
- An arch
- A lagoon
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Why does a river mouth often stop a spit from reaching the far side?
- The river current keeps a gap open
- The river deposits so much sand that the spit sinks
- The river freezes the spit in place
- The river carries the spit's sand inland
-
Put these steps of spit formation in the correct order.
- Sediment is deposited, the end hooks, the coastline bends, drift carries sediment
- The end hooks, sediment is deposited, drift carries it, the coastline bends
- The coastline bends, the end hooks, drift carries sediment, sediment is deposited
- Longshore drift carries sediment, the coastline bends, sediment is deposited, the end hooks
-
Why does a beach grow in a calm, sheltered bay?
- The backwash is strongest there, dragging material back to the bay
- The waves are so strong that they carry the sand far out
- Waves are weak there, so they drop sand and shingle that builds up
- Hydraulic action forces sand up the cliffs at the back of the bay
-
Why are a spit, a bar and a beach all built by the same kind of process?
- They form only where the waves carry no sediment at all
- They are all formed only by freezing water in cracks
- They are all built where the sea loses energy and deposits sediment
- They are all carved by the sea wearing rock away
-
Suggest how rising sea levels might affect a low spit such as Spurn Point.
- Rising seas would stop longshore drift entirely, freezing the spit in its current shape
- The spit would grow higher because the water pushes sand upward into a taller ridge
- The spit would become a headland as the sea hardens it into solid rock over time
- Higher seas could cover or wash away the low ridge, so it might shrink or be breached
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Explain why a bar does not usually form where a river keeps a gap open.
- The river deposits so much sand that the ridge sinks below the surface of the water
- The river freezes the ridge in place so that it can no longer extend across the gap
- The river current stops the ridge from growing all the way across the gap
- The river erodes the ridge away before it can grow, carrying the sand off to sea
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Why is a spit likely to grow where the coastline bends?
- Bends stop longshore drift, so sediment piles up under cliffs
- The sea loses energy at the bend and deposits the sediment it was carrying
- The bend makes the waves stronger, so sediment is thrown further out
- Bends cause hydraulic action that carries sand inland
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