Unit 1C - Coastal Landscapes in the UK - Landforms caused by deposition Flashcards
What is a spit?
An extended stretch of beach material that projects out to sea and is joined to mainland at one end
Where are beaches found?
Found between high- and low-tide levels
How and where does beach material accumulate?
In a sheltered bay around an obstacle
Difference between sand and shingle beaches?
Sand - flat and wide, weak backwash can move small sand particles back down beach, creating long, gentle slope
Shingle - steep and narrow, weak backwash can’t move large single particles back down beach, creating steep slope
What is a spit?
An extended stretch of beach material that projects out to sea and is joined to mainland at one end with a hooked end
5 conditions needed for spit to form? Where do they form?
Change in direction of coastline, large load, constructive waves, shallow water and a weak current.
Form at sharp bends
Why do spits stop growing?
Depth of water increases and current becomes stronger, curving end of spit (recurved end)
What is created and grows in the sheltered area behind a spit?
Mud flats or salt marsh, lots of material accumulates here so plants can grow
Example of a spit in UK?
Spurn Head along Holderness coast
What is a bar?
A ridge of sand or shingle which forms across entrance to a bay or cove linking two headlands
How does a bar and lagoon form?
- Spit develops in a bay, into which no major river flows, and builds across bay to other headland, cutting off bay between headlands, which forms lagoon behind bar
Example of a bar in UK?
Slapton Lay, Devon
Conditions need for sand dunes to form?
Obstacles of beach (human or natural), strong winds and lots of sediment moved by saltation
What happens when wind encounters obstacle?
Velocity falls and sediment deposited
How do sand dunes form?
- Sand deposited by LSD is moved up beach by wind
- Sand deposited behind obstacle
- It is colonised by plants and grasses, which stabilises sand and encourages more sand to accumulate there, forming small dunes (embryo)
- Over time, oldest dunes migrate inland as new dunes form