Longshore Drift
Transportation
Deposition and Landforms
waves & processes
Erosion
100

what is longshore drift?

The movement of sediment along the coastline by waves

100

what is solution

the transportation of dissolved material in seawater

100

When does deposition occur?

When waves carrying sediment reach the shore, they will deposit it in areas where they lose energy

100

what is deposition

the laying down of sediment

100

Define erosion

Erosion is when the rocks are worn away, in this case by the action of waves.

200

what does longshore drift do? 

it move sediment along the coastline

200

what does suspension do

it carries fine sediment within the water, the sediment is floating in the water

200

Name 2 landforms created by deposition

Beaches, spits, bars, tombolos

200

what does erosion do

it wears away and removes material from the coastline 

200

Name the 4 types of erosion

Hydraulic action, Abrasion, Attrition, Solution

300

How does longshore drift move sediment?

Swash carries sediment up the beach at an angle, while backwash carries it back down the beach at 90 degreees back into the sea producing a zig zag movement

300

what are four types of transportation

solution, suspension, saltation and traction

300

Landform created due to alternating bands of hard and soft rock

Headlands and bays

300

why does deposition occur when waves lose energy

the waves have less energy to transport sediment , so they drop it as there is not enough energy to carry on carrying them

300

Define hydraulic action

Waves crash against a cliff and force air into cracks in the rock. The force of this trapped air causes the rock to weaken and eventually break.

400

A coastline changes direction. What is likely to happen to sediment being transported by longshore drift?

The change in coastline direction can cause sediment to be deposited as the waves lose energy

400

A river transports large rocks and fine particles towards the sea. Which transportation processes could carry each type of sediment?

Large rocks are transported by traction, smaller rocks by saltation, and very fine particles by suspension. Dissolved minerals can be transported by solution.

400

Explain the stages in the formation of caves, arches, stacks and stumps

As headlands are unsheltered, they will be assaulted by waves. Any faults or weaknesses in the headland will start to be worn away. Gradually, these faults will deepen until they form a cave. If a cave forms on both sides of the headland, this may break through, forming an arch.

Over time, the arch will get increasingly wide until the roof collapses, leaving a pillar of rock known as a sea stack. This will be eroded and eventually collapse to leave a stump.

400

A coastline contains both a headland and a bay. Predict where erosion and deposition are most likely to occur and explain why

Erosion is greatest around the headland because wave energy is concentrated there. Deposition is more likely in the bay because wave energy is lower.

400

This is where sediment being carried by the water wears away the surface, almost like sandpaper.

Abrasion

500

explain how longshore drift can contribute to the formation of a tombolo

Waves approach the coastline at an angle, causing swash to move sediment up the beach at an angle. Backwash moves sediment back towards the sea at right angles. This creates a zig-zag movement of sediment along the coastline. Continued transportation and deposition can move sediment towards an offshore island until it eventually connects the island to the mainland, forming a tombolo.

500

Explain how solution, suspension, saltation and traction transport sediment.

Solution transports dissolved material. Suspension carries fine particles within the water. Saltation causes smaller particles to bounce along the seabed. Traction causes larger rocks and boulders to roll along the seabed.

500

How does geology influence the formation of landforms?

Soft rocks erode faster; hard rocks are slow to erode

500

Explain how wave refraction affects erosion around headlands and bays

As waves enter shallow water, friction with the seabed slows them down. This causes the waves to bend or refract. Wave energy becomes concentrated around headlands, increasing erosion. Wave energy is lower in bays, meaning there is less erosion and deposition is more likely.

500

Define Attrition 

Rocks crashing into each other result in them becoming smoother and more rounded.