100% satisfaction guarantee Immediately available after payment Both online and in PDF No strings attached
logo-home
AQA GCSE Geography Coastal Landscapes Summary Notes £8.99   Add to cart

Summary

AQA GCSE Geography Coastal Landscapes Summary Notes

 7 views  0 purchase

AQA GCSE Geography Coastal Landscapes Summary Notes from Hodder textbook Concise, detailed, easy-to-revise Includes case studies and examples

Preview 2 out of 14  pages

  • No
  • Coastal landscapes
  • May 29, 2023
  • 14
  • 2022/2023
  • Summary
book image

Book Title:

Author(s):

  • Edition:
  • ISBN:
  • Edition:
All documents for this subject (686)
avatar-seller
rdas07
Coastal landscapes

Waves
What causes waves?

Waves: transfer of energy from wind to sea due to friction of wind on water’s surface. Waves shape
coast through erosion + deposition

In deep water, water molecules in wave move in circular movement, waves move forward in shallow
water.

Strength of wave

Depends on:

- Speed of wind (more energy transferred to waves)
- Time the wind has been blowing longer = more energy
- Fetch (maximum distance of open sea that wind can blow over): longer fetch, higher chance
of large waves

Terminology

 Crest: top of wave
 Trough: base of wave
 Wave height: vertical
distance from trough to crest
 Wave length: horizontal
distance between two
successive crests
 Wave frequency: number of
waves breaking/minute



Constructive and destructive waves

Constructive Destructive
- Sheltered bays, sloping sandy beaches - Exposed bays, steep pebble beaches
Swash goes far forward (large area). Wave loses Backwash stronger than swash (both stronger
energy (friction with sand), weak backwash- than constructive). Waves comb beach
build up beach (not destroy) material, lowering beaches in winter
- Long wave length (low frequency)- 8-10 - Waves erode headland
waves/minute - Short wave length (high frequency)- 10-
- Low wave height (under 1m), gently 14 waves/minute
sloping wave front - Steep wave front, over 1m high wave,
does not travel far up beach


Weathering and mass movement
How does weathering affect cliff face?

Weathering: breaking down on rock in situ. Caused by changes in atmosphere, e.g. precipitation +
extremes of temperature

, Chemical weathering- Caused by chemical reaction (rainwater decomposes/eats rock)

 Carbonation- carbonic acid in rainwater reacts with CaCO 3 (limestone) = sodium
bicarbonate. This is soluble- limestone carried in solution
 Hydrolysis- acidic rainwater causing rock to rot (granite  clay)
 Oxidation- rocks broken down by O2 and water, giving iron-rich rocks rust-coloured surface

Mechanical (physical) weathering- Rocks disintegrated, associated with extremes of temperature

 Freeze-thaw weathering: water enters cracks, freezes in cold temperatures (night), ice
expands by 9%, creating pressure. Temperature increases, ice thaws, process repeats,
causing fragments to break off (scree at base of cliff)
 Salt weathering: salt spray from ocean gets into crack, salt crystallises, creating pressure,
weakening structure

How does mass movement happen?

Mass movement: downslope movement of rock, soil, or mud under influence of gravity. Usually
triggered by heavy rainfall, scale of damage determined by extent of weathering

Sliding- Downhill movement of large amount of rock, soil and mud occurs on
landslide steep cliffs weakened by weathering
- Rain infiltrates soil, percolates into rocks, making it heavier.
- Heavier, saturated rock falls along slip plane (line of weakness-
fault/bedding plane).
- Slide starts by tearing vegetation, descent aided by lubrication
from wet rocks.
- Cliffs in Durdle Door, Dorset, suffered large landslides.

Sliding- Large amount of rock slips along fairly straight slip plane.
rock Rock falls as a block, maintains contact with cliff
slide Leading edge = pile of rocks in sea
Sliding- Wet + rapid, occur on slopes > 10°, e.g. Monmouth Beach (Lyme Regis,
mud Dorset)
slide Vegetation sparse, cannot hold in place
Rock Bare, well-jointed rocks prone to freeze-thaw weathering  falling
falls rocks lose contact with cliff face. Form scree slope at bottom.
Common on vertical cliffs
Burton Bradstock, Dorset- 400 tonnes fell from 49m vertical cliff In July
2012
Slumping Has concave slip plane
Material rotated backwards onto cliff face, e.g. Barton-on-Sea,
Hampshire, slumping at 30cm/day
Marine processes
Processes of coastal erosion

Marine erosion: removal of material by waves

Higher rate of erosion where;

 Rock has many joints
 Coastline exposed to large fetch (Needles, Isle of Wight, 8000km fetch)
 Strong winds = destructive waves (winter)

The benefits of buying summaries with Stuvia:

Guaranteed quality through customer reviews

Guaranteed quality through customer reviews

Stuvia customers have reviewed more than 700,000 summaries. This how you know that you are buying the best documents.

Quick and easy check-out

Quick and easy check-out

You can quickly pay through credit card for the summaries. There is no membership needed.

Focus on what matters

Focus on what matters

Your fellow students write the study notes themselves, which is why the documents are always reliable and up-to-date. This ensures you quickly get to the core!

Frequently asked questions

What do I get when I buy this document?

You get a PDF, available immediately after your purchase. The purchased document is accessible anytime, anywhere and indefinitely through your profile.

Satisfaction guarantee: how does it work?

Our satisfaction guarantee ensures that you always find a study document that suits you well. You fill out a form, and our customer service team takes care of the rest.

Who am I buying these notes from?

Stuvia is a marketplace, so you are not buying this document from us, but from seller rdas07. Stuvia facilitates payment to the seller.

Will I be stuck with a subscription?

No, you only buy these notes for £8.99. You're not tied to anything after your purchase.

Can Stuvia be trusted?

4.6 stars on Google & Trustpilot (+1000 reviews)

73918 documents were sold in the last 30 days

Founded in 2010, the go-to place to buy revision notes and other study material for 14 years now

Start selling
£8.99
  • (0)
  Add to cart