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Questions and Answers
What is the main effect of hydraulic action in coastal erosion?
What is the main effect of hydraulic action in coastal erosion?
It compresses trapped air in cracks, creating pressure that breaks the rock.
Explain the formation of a cliff's wave cut platform.
Explain the formation of a cliff's wave cut platform.
A wave cut notch is created through hydraulic action, and backwash transports material, leading to the formation of the platform.
Define longshore drift and its impact on coastal landforms.
Define longshore drift and its impact on coastal landforms.
It's the zigzag movement of sediment along the coast caused by waves, leading to features like spits and bars.
How is a tombolo formed?
How is a tombolo formed?
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What process leads to the formation of sand dunes?
What process leads to the formation of sand dunes?
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Describe how a spit develops its hook shape.
Describe how a spit develops its hook shape.
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What distinguishes a headland from a bay in coastal geography?
What distinguishes a headland from a bay in coastal geography?
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Identify two erosional features found on the Jurassic Coast.
Identify two erosional features found on the Jurassic Coast.
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What is the primary role of solution in the erosion process?
What is the primary role of solution in the erosion process?
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Explain the difference between traction and saltation in sediment transportation.
Explain the difference between traction and saltation in sediment transportation.
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What are the main factors contributing to the diversity of the UK's landscape?
What are the main factors contributing to the diversity of the UK's landscape?
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How does the length of fetch affect wave formation?
How does the length of fetch affect wave formation?
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What characterizes constructive waves and their impact on beaches?
What characterizes constructive waves and their impact on beaches?
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Define weathering and identify its three types.
Define weathering and identify its three types.
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Explain the freeze-thaw process as a form of physical weathering.
Explain the freeze-thaw process as a form of physical weathering.
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What are the characteristics of destructive waves and their effect on coastlines?
What are the characteristics of destructive waves and their effect on coastlines?
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How does biological weathering occur?
How does biological weathering occur?
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What causes chemical weathering, particularly with regard to acid rain?
What causes chemical weathering, particularly with regard to acid rain?
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Describe the impact of rock type on the UK's various landscapes, citing examples.
Describe the impact of rock type on the UK's various landscapes, citing examples.
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How do rivers like the Thames and Severn relate to the UK's diverse landscape?
How do rivers like the Thames and Severn relate to the UK's diverse landscape?
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Study Notes
UK's Landscape: Diverse Features
- Composed of upland and lowland areas
- Upland areas characterized by resistant rocks (e.g., granite, slate) forming dramatic mountain ranges (e.g., Arran, Scotland)
- Lowland areas shaped by less resistant rocks (e.g., clay, limestone) forming gentle landscapes (e.g., Cotswolds)
- Extensive river systems (e.g., Thames, Severn, Wye)
- Varied coastlines, including erosion-prone clay coastlines (e.g., Holderness) and areas with prominent cliffs (e.g., White Cliffs of Dover)
Wave Formation and Breaking
- Waves form from wind friction on water surface, creating swells
- Wave strength dependent on fetch (wind distance over water)
- Wave base slows due to bottom friction, leading to elliptical orbits and wave break
- Wave types, constructive and destructive, affect beach profiles
Weathering Processes
- Weathering is the breakdown of rocks in place
- Biological weathering: Rocks weakened by plants (roots) and animals (e.g., grazing)
- Chemical weathering: Rocks broken down by chemical reactions (e.g., acid rain dissolving rock components).
- Physical weathering: Rocks broken down by geological processes (e.g., freeze-thaw, exfoliation)
Freeze-thaw and Exfoliation
- Freeze-thaw weathering: Water in cracks freezes and expands, widening cracks and breaking rocks apart
- Exfoliation weathering: Repeated heating and cooling in hot regions cause surface layers to break off, creating rounded shapes.
Erosion Processes
- Erosion is the wearing away and movement of sediment.
- Solution: Rocks dissolve in chemicals
- Attrition: Rock fragments collide, becoming smaller and smoother
- Hydraulic action: Wave force compresses air in cracks, causing rock breakage.
Sediment Transportation
- Transportation involves moving sediment.
- Suspension: Small particles carried by water
- Traction: Large particles rolled along the seabed
- Saltation: Medium particles bounce along the seabed
- Solution: Dissolved particles carried in water
Deposition
- Deposition is the dropping of sediment when water loses energy or sediment becomes too heavy.
Coastal Landform Formation
- Cracks, caves, arches, stacks, and stumps: Cracks widen to caves, caves enlarge, breaching to form arches, arches collapse leaving stacks, stacks erode into stumps
- Wave-cut platforms: Wave action creates notches in cliffs, undercutting results in wave-cut platforms, cliff collapse replenishes the platform.
- Longshore drift: Waves approach beaches at an angle, swash and backwash transport sediment in a zig-zag pattern, creating spits, bars, and tombolos.
Spit Formation
- Spit is sediment protruding into the sea
- Accumulation at a change in wave energy (e.g., river mouth)
- Development of a hook due to wind shift
- Salt marshes and sand dunes may form
Bar Formation
- Bar connects two headlands
- Longshore drift deposits sediment across a bay, creating the bar
Tombolo Formation
- Tombolo connects an island to the mainland through deposited sediment
Beach Formation
- Beaches are accumulations of sediment (sand, shingle)
- Sediment color reflects local rock types
- Sandy beaches from constructive waves; shingle from destructive waves
- Fine sediment closer to water, coarser towards the back
Sand Dune Formation
- Accumulated sediment, often behind beaches
- Embryo dunes develop and mature with more sediment and vegetation
Headlands and Bays Formation
- Headlands are projecting pieces of land
- Bays are inlets where sediment gathers
- Formed at discordant coastlines where rock layers are perpendicular to the water, softer rock erodes into bays, harder rock forms headlands.
- Accumulation of sediment within the bay.
Jurassic Coast Case Study
- Covers 95 miles of Devon and Dorset coastline.
- Diverse landforms (erosional and depositional) due to varied geology (soft clays/sand vs. hard limestone/chalk) and longshore drift.
- Includes features like Old Harry Stack, Durdle Door, and Chesil Beach.
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Description
Explore the diverse geographical features of the UK, including its upland and lowland areas, extensive river systems, and varied coastlines. Learn about wave formation and breaking, as well as the weathering processes that shape the landscape. This quiz covers important concepts in physical geography essential for understanding the Earth's surface.