OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Coastal Landscapes
Lithology, geological structure and the plan of the coast
- 3 things to know
- Component 01
Overview
Recall questions on lithology and geological structure, how clay, chalk, granite and glacial till resist the sea, discordant and concordant coastlines around Swanage, how coves form, how the dip of the strata shapes a cliff profile, and why faults and joints become caves and geos.
What you need to know
Answer each one before you reveal it.
Explain why unconsolidated glacial till erodes far faster than the chalk beside it.
Define lithology as it affects the coast
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define lithology.
Model answer
The physical and chemical make-up of a rock, including its mineral composition and how strongly its particles are cemented together.
- 2
What is meant by geological structure at the coast?
Model answer
The arrangement of the rocks, including their bedding, jointing, faulting and the angle at which the strata dip.
- 3
Why does clay retreat quickly under wave attack?
Model answer
Its particles are weakly bonded and it loses much of its strength when saturated, so waves remove it easily and it slumps readily.
- 4
Why do chalk cliffs stand almost vertically even though chalk is a fairly weak rock?
Model answer
Chalk is permeable and well jointed, so water drains through it rather than building up pressure, and the joints give clean vertical failure surfaces.
- 5
Why is granite highly resistant at the coast?
Model answer
It is a crystalline rock of interlocking crystals with few bedding planes, so there are far fewer lines of weakness for waves to exploit.
- 6
What is a discordant coastline?
Model answer
A coast where bands of rock of differing resistance meet the sea at a high angle, so alternating headlands and bays develop.
Other ways to work this
The same content, four other ways.
What is inside Levo
Six ways to work the same material.
Every question in Coastal Landscapes, on a schedule.
Attempt a question from memory, write the correct version, then attempt it again. Levo records the jump between your first attempt and your last, and brings each question back on the day you are due to forget it.
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