OCR A-Level Geography Physical systems (01), June 2025: Question 1
33 marks · Hard difficulty · Extended Response
Answer a series of questions on coastal landscapes, including the formation of salt marshes, statistical analysis of cliff erosion data, processes shaping a fjord, and an essay evaluating the relative influence of management strategies versus economic development.
Practise this questionQuestion
Question text
Option A – Coastal Landscapes
(a) Explain the influence of flows of energy in the formation of a salt marsh. [8]
(b) Study Table 1, which shows cliff erosion rates on the East Yorkshire coast, UK.
Table 1 Cliff erosion rates on East Yorkshire coast, UK
Rate of erosion
Location
(m / year)
Bridlington 1.00
Barmston 2.00
Hornsea 0.25
Mappleton 1.50
Aldbrough 0.80
Grimston 1.10
Tunstall 0.75
Withernsea 2.20
Out Newton 1.90
Spurn neck 3.10
(i) Using Table 1, calculate the mean rate of erosion.
Show your workings. [2]
(ii) The standard deviation for the rate of erosion in Table 1 is 0.8.
State what this indicates about the dispersion (spread) of the data set. [2]
(iii) Explain why standard deviation is a more accurate measure of dispersion (spread) than range
and interquartile range. [2]
(c) Study Fig. 1, a coastal landscape in Norway.
With reference to Fig. 1, explain the influence of one geomorphic process in shaping landform A
(fjord). [3]
(d)* ‘Coastal landscape systems are influenced more by management strategies than by the
unintentional impacts of economic development.’
To what extent do you agree with this statement? [16]
Mark scheme
Show the mark scheme
Question Answer Mark Guidance
1 (a) Explain the influence of flows of energy in the 8 Indicative content:
formation of a salt marsh. AO1 x8 AO1 – 8 marks
Knowledge and understanding of the reasons for the
Level 3 (6-8 marks) influence of flows of energy (e.g. thermal, kinetic,
Demonstrates thorough knowledge and understanding gravitational) in the formation of a salt marsh could
of the influence of flows of energy in the formation of a potentially include:
salt marsh. (AO1). • As a spit develops across a river mouth kinetic
energy in the channel reduces as the spit
This will be shown by including well-developed ideas creates a barrier reducing speed causing
with a clear appreciation of the reasons for the increased deposition
influence of flows of energy in the formation of a salt • In the widening sheltered area behind the spit,
marsh. kinetic energy continues to reduce causing
continued fluvial deposition creating mud flats
Level 2 (3-5 marks)
exposed at low tide
Demonstrates reasonable knowledge and
understanding of the reasons for the influence of flows • On the margins of the salt marsh fluvial currents
of energy in the formation of a salt marsh. have higher kinetic energy (greater speed) as
they can flow out to sea – these are likely to
This will be shown by including developed ideas with change with the tide
some appreciation of the reasons of the influence of • Flocculation of clay particles creates flocs which
flows of energy in the formation of a salt marsh. are heavier and require more energy to move
• Over time energy levels in the salt marsh
Level 1 (1-2 marks) change as vegetation develops through thermal
Demonstrates basic knowledge and understanding of energy from the sun. This produces more
the reasons for the influence of flows of energy in the friction, causing lower velocities and increased
formation of a salt marsh (AO1). deposition as kinetic energy lowers
• After further succession and development of
This will be shown by including simple ideas and with
creeks faster flow and greater kinetic energy will
no or limited appreciation of the reasons for the
influence of flows of energy in the formation of a salt be found here as there is less friction
marsh. • Salt marshes can also form in gently sloping
inter-tidal zones where kinetic energy reduces
0 marks due to friction leading to vertical deposition and
No response or no response worthy of credit. salt marsh formation
1 (b) (i) Study TABLE 1, which shows cliff erosion rates on 2 AO3 - 2 marks
the East Yorkshire Coast, UK. Using TABLE 1, AO3 x2 1 x 1 (✓) for calculating the mean rate of erosion using
calculate the mean rate of erosion. Show your TABLE 1.
workings. 1 x 1 (✓) for showing workings.
• 1+2+0.25+1.5+0.8+1.1+0.75+2.2+1.9+3.1 / 10
( ) or 14.6 / 10 ( )
• Mean value is 1.46 ( )
1 (b) (ii) The standard deviation for the rate of erosion in 2 AO3 – 2 marks
TABLE 1 is 0.8. State what this indicates about the AO3 x2 1 x 1 (✓) for general point about dispersion
dispersion (spread) of the data set. 2 x 1 (✓) for specific point about dispersion
• The sample suggests that approximately 68% of
the values ( ) lies in the range 0.66 - 2.26
(within 0.8 of the mean) ( )
• The sample is clustered around the mean /
limited dispersion (✓) but there are a couple of
locations more than one SD from the mean (e.g.
Hornsea (0.25) (✓)
• The sample suggests that 8/10 or 80% of the
values ( ) lie within 1 SD of the mean / within
0.8 ( )
1 (b) (iii) Explain why standard deviation is a more accurate 2 AO3 – 2 marks
measure of dispersion (spread) than range and AO3 x2 1 x 1 (✓) for explanation of why standard deviation is
interquartile range. more accurate than the range
1 x 1 (✓) for explanation of why standard deviation is
• Standard deviation is more useful than the more accurate than the interquartile range
range which only uses the maximum and
minimum value so gives you limited information
about the spread of data ( )
• Standard deviation is more useful than the
range, as the range can be skewed by
outliers/anomalies’ ( )
• Standard deviation is more useful than the IQR
which only uses half the values / the middle 50%
of the data set ( )
• The range only uses the highest and lowest
values ( )
1 (c) Study FIG. 1, a coastal landscape in Norway. 3 Indicative content:
With reference to FIG. 1, explain the influence of AO2 x3 AO2 – 3 marks
ONE geomorphic process in shaping landform A For analysing Fig. 1 to explain the influence of ONE
(fjord). geomorphic process in shaping landform A (fjord)
• Biological weathering where roots grow into • The original formation of the U shaped valley by
cracks in the rock ( ) causing the rocks to break glacial erosion is creditworthy
apart (DEV), creating landslides (DEV) • Naming a geomorphic process of its own is not
• Mechanical weathering e.g. freeze-thaw where sufficient for a mark.
water gets into cracks in the rock face ( ). As it • A geomorphic process must be present within
freezes it expands (DEV) causing disintegration the answer to achieve full marks.
and the formation of steep valley sides (DEV)
• Marine erosion, such as abrasion at the base of
valley sides, involves waves carrying rock
particles that scour and wear away the rock (✓),
Question Answer 12 Mark Guidance
leading to its removal (DEV) and potentially
triggering mass movement (DEV)
• As the ice moves down the valley, plucking would
occur ( ) so the valley became deeper and
wider (DEV)
1 (d*) ‘Coastal landscape systems are influenced more by 16 Indicative content
management strategies than by the unintentional AO1 x8
impacts of economic development.’ To what extent AO2 x8 AO1 – 8 marks
do you agree with this statement? Knowledge and understanding of management
strategies and economic development on coastal
AO1 landscape systems could potentially include:
Level 3 (6-8 marks) • Influence of management strategies
Demonstrates thorough knowledge and understanding o Groynes – building the beach minimising
of the influence of management strategies and movement of sediment influencing
economic development on coastal landscape systems. landforms down coast with increased
erosion rates reducing beaches
The answer should include accurate place-specific o Beach recharge – building up the beach
detail. annually
o Recurved seawalls – reflecting waves to
Level 2 (3-5 marks)
reduce erosion, results in less cliff collapse
Demonstrates reasonable knowledge and
understanding of the influence of management and less sediment carried so more erosion
strategies and economic development on coastal down coast
landscape systems. o Influence of managed retreat on width of
salt marshes
The answer should include place-specific detail which • Influence of unintentional change caused by
is partially accurate. economic development
o Sand dredging for construction resulted in
Level 1 (1-2 marks) wider, flatter beaches which are less
Demonstrates basic knowledge and understanding of effective at absorbing energy leading to
the influence of management strategies and economic more breached beaches, dunes and spits.
development on coastal landscape systems. o Breakwaters at ports/harbours may disrupt
longshore sediment supply downdrift
reducing size of beaches.
There is an attempt to include place-specific detail but o Construction on slopes/cliff tops adds
it is inaccurate. weight increasing likelihood of mass
movement.
0 marks
No response or no response worthy of credit. AO2 – 8 marks
Apply knowledge and understanding to analyse and
AO2
evaluate to what extent coastal landscape systems are
Level 3 (6-8 marks)
influenced more by management strategies than
Demonstrates thorough application of knowledge and
unintentional change caused by economic development
understanding to provide clear and developed analysis
could potentially include:
that shows accuracy. Includes a detailed evaluation that
• Importance will vary depending on use of case
offers generally secure judgements, with some link
between rational conclusions and evidence, of the study
extent to which coastal landscape systems are • Sandbanks, Dorset erosion rates lowered from
influenced more by management strategies than 1.6m/yr building wider and deeper beach, and
unintentional change caused by economic creating more mass movement and erosion at
development. Barton Cliffs however, rotational slumping is
continuing and new escarpments are being
Level 2 (3-5 marks) created regularly.
Demonstrates reasonable application of knowledge • At Mangawhai-Pakiri, New Zealand rates of
and understanding to provide sound analysis that extraction are unsustainable in closed system,
shows some accuracy. Includes a sound evaluation of beaches being breached more and shape
the extent to which coastal landscape systems are changing to be wider and flatter. Breaches have
influenced more by management strategies than affected tidal currents increasing sedimentation,
unintentional change caused by economic fore dunes undercut by waves causing more
development. Judgement and conclusions are
mass movement and aeolian erosion. Coastal
generalised, with limited use of evidence.
retreat estimated at 35m, with width of coastal
Level 1 (1-2 marks) zone vulnerable to erosion between 48-111m by
Demonstrates basic application of knowledge and the end of the century
understanding to provide simple analysis that shows • Economic development had greater impact –
limited accuracy to provide an un-supported evaluation over time, also unsustainable indicating greater
that offers simple conclusions of the extent to which (irretrievable) impact, wider scale of impact e.g.
coastal landscape systems are influenced more by widespread sedimentation of harbour and fore
dunes undercut
management strategies than unintentional change Highest level likely to refer to dynamic equilibrium /
caused by economic development. spatial / temporal variations.
0 marks
No response or no response worthy of credit.
Quality of extended response
Level 3
There is a well-developed line of reasoning which is
clear and logically structured. The information
presented is relevant and substantiated.
Level 2
There is a line of reasoning presented with some
structure. The information presented is in the most-part
relevant and supported by some evidence.
Level 1
The information is basic and communicated in an
unstructured way. The information is supported by
limited evidence and the relationship to the evidence
may not be clear.
How to answer it
OCR A-Level Geography: Coastal Landscapes & Quantitative Skills
This paper tests core conceptual, statistical, and evaluative competencies across the Coastal Landscapes module:
- Systems & Flows of Energy: Understanding kinetic, thermal, and gravitational energy in low-energy depositional environments (salt marshes).
- Fieldwork & Quantitative Skills: Calculating arithmetic mean, interpreting standard deviation (dispersion of cliff retreat data), and critically evaluating measures of spread (standard deviation vs. range vs. interquartile range).
- Geomorphic Processes in Relict/Glaciated Landscapes: Explaining shaping processes (freeze-thaw, plucking, marine erosion) on landforms of submergence (fjords).
- Extended Synoptic Evaluation (16-mark essay): Comparing intentional management intervention against unintended consequences of human economic activity (sand dredging, development, harbours) across space and time, with reference to dynamic equilibrium.
Explain the Influence of Flows of Energy in the Formation of a Salt Marsh
AO1: Demonstration of Knowledge and Understanding (Systems Approach)
💡 Key Knowledge: Energy in a Coastal System
- Kinetic Energy (Water/Wind): Low wave and current velocity behind a spit or barrier island promotes flocculation and sedimentation of fine clays/silts.
- Frictional Dissipation: Pioneer species (e.g., Salicornia) create friction, dissipating tidal kinetic energy and accelerating deposition.
- Gravitational Potential Energy: Tides bring water in and out twice daily. At high slack water, kinetic energy drops to zero, allowing vertical sediment accumulation.
- Thermal Energy (Solar): Warms mudflats, encouraging halophytic vegetative growth and biological cohesion.
✅ Model Answer Points (Level 3: 6–8 marks)
- Sheltered, Low-Energy Context: Behind a feature like a spit, kinetic wave energy is sharply attenuated. Slack water periods during tidal cycles provide quiet conditions.
- Flocculation: Chemical interaction of salt and clay forms heavier clumps which settle out under reduced kinetic energy conditions.
- Succession Feedback: As eelgrass and cordgrass colonise, increased biological roughness generates friction, reducing kinetic velocity further. Creeks develop where remaining ebb flow kinetic energy is channeled.
🧠 Exam Technique
Frame the answer explicitly around types and flows of energy (kinetic, gravitational, thermal, dissipation via friction) rather than just describing vegetation succession in isolation. Level 3 answers must clearly show how changes in energy flows drive the physical landform's development.
❌ Common Errors
- Only describing plant succession without linking it to the dissipation of wave/tidal energy.
- Failing to mention the low-energy environment (spits, estuaries, sheltered bays) that allows the process to initiate.
Quantitative Skills: Cliff Erosion Rates & Measures of Dispersion
Part (b)(i): Mean Calculation [2 Marks]
📐 Step-by-Step Calculation
- Sum the values:
1.00 + 2.00 + 0.25 + 1.50 + 0.80 + 1.10 + 0.75 + 2.20 + 1.90 + 3.10 = 14.60 - Divide by the number of sites (n = 10):
14.60 ÷ 10 = 1.46 - Final Answer: 1.46 m/year
❌ Common Calculation Traps
- Arithmetic error when adding decimal values without double-checking.
- Not writing down the full working expression: 1 mark is awarded specifically for showing workings ( 14.6 / 10 ).
Part (b)(ii): Interpreting Standard Deviation (s = 0.8) [2 Marks]
✅ Acceptable Statements (Choose 2 for 2 marks)
- General Spread: Indicates moderate/limited dispersion around the mean rate (1.46 m/yr).
- Empirical Rule (68%): Approximately 68% of the data values lie within 1 standard deviation of the mean (range: 1.46 ± 0.8 = 0.66 to 2.26 m/yr ).
- Observed Count: 8 out of 10 locations (80%) fall within 1 SD of the mean.
- Outliers Identified: A small number of locations fall more than 1 SD away, notably Hornsea (0.25 m/yr, defended) and Spurn Neck (3.10 m/yr, highly dynamic).
🧠 Exam Technique
Provide one general statement about what the value means for data clustering, and one specific data-supported statement (such as calculating the 1 SD boundary: 0.66 to 2.26 m/year).
Part (b)(iii): Comparing Measures of Dispersion [2 Marks]
✅ Why SD is Superior to Range and IQR
- Advantage over Range: Range only takes into account extreme values (maximum – minimum) and is heavily distorted by anomalies/outliers, giving no insight into how data is clustered.
- Advantage over IQR: The interquartile range (IQR) only uses the middle 50% of the dataset and ignores the outer 50%, whereas standard deviation incorporates every single data value into its calculation.
❌ Common Errors
Only discussing the range or only discussing IQR. The question explicitly states "than range and interquartile range" — 1 mark is allocated for contrasting with range, and 1 mark for contrasting with IQR.
Explain the Influence of ONE Geomorphic Process in Shaping Landform A (Fjord)
AO2: Application of Knowledge to Photographic Evidence (Fig. 1)
✅ Model Answers (Select ONE Process Only)
- Option 1: Glacial Plucking / Abrasion
As a glacier moves down a pre-existing river valley, meltwater freezes rocks to the glacier base, plucking blocks from the valley floor and sides, while rock fragments abrade bedrock. This creates the steep, sheer rock walls and over-deepened, flat-bottomed U-shaped trough visible in the fjord. - Option 2: Freeze-Thaw Weathering (Periglacial/Post-glacial)
Water enters joints and fractures in the exposed steep fjord valley walls. As temperatures fluctuate around 0°C, water expands by ~9% upon freezing, exerting pressure. Repeated cycles shatter the rock face, supplying scree to the water line and maintaining sheer cliffs. - Option 3: Marine Erosion (Hydraulic Action / Abrasion)
Submergence by post-glacial eustatic sea-level rise exposes the fjord sides to marine waves. High-energy marine processes scour the cliff base, undercut slopes, and initiate rockfalls along bedding planes.
🧠 Exam Technique: Name + Mechanism + Development
- Step 1: Explicitly name ONE process (e.g. freeze-thaw or plucking). (1 mark)
- Step 2: Detail the mechanical steps (e.g. water expansion / ice freezing to bedrock). (1 mark)
- Step 3: Directly link to the observed landform feature (steep valley walls / U-shaped valley floor). (1 mark)
Essay: Management Strategies vs. Unintentional Impacts of Economic Development
"Coastal landscape systems are influenced more by management strategies than by the unintentional impacts of economic development." To what extent do you agree?
💡 AO1 Content: Knowledge & Case Studies
- Intentional Management Strategies:
- Hard engineering: Groynes at Hornsea/Mappleton trap sediment via LSD, starving downdrift coasts (terminal groyne syndrome). Recurved seawalls reflect wave energy, scouring beaches.
- Soft engineering: Beach nourishment, sand dune stabilisation, managed retreat (e.g., Medmerry, Sussex) restoring coastal marshes and dissipating storm energy.
- Unintentional Economic Impacts:
- Offshore Dredging: Mangawhai-Pakiri (New Zealand) — extraction of sand for the construction industry depletes the nearshore sediment budget, leading to flatter, narrower beaches, breaching of dunes, and accelerated coastal retreat.
- Port/Harbour Infrastructures: Jetties, breakwaters, and dredged channels interrupt littoral drift and trap sediment permanently out of the littoral cell.
- Cliff-top Urbanisation: Construction increases surcharge weight on cliff edges, alongside altered drainage/runoff, triggering rotational slumps (e.g., Barton-on-Sea).
🧠 AO2 Evaluation & Structure (Level 3 Criteria)
- Dynamic Equilibrium: Discuss whether human intervention or economic accidents push coastal systems beyond a threshold from which they cannot recover.
- Spatial Scale: Management often has local positive impacts but negative downdrift impacts along the wider sediment cell (e.g., Mappleton groynes causing rapid erosion at Cowden).
- Temporal Scale: Economic impacts (such as deep offshore mining in a closed system) can cause permanent, irreversible changes over decades, whereas soft management requires constant re-investment.
- Nuanced Conclusion: Management is often a reaction to the unintended consequences of prior economic development, making both intrinsically linked within the coastal system.
❌ Pitfalls that Prevent Scoring Top Marks (Level 3)
- Listing without comparing: Writing two disconnected case studies without directly balancing intentional vs. unintentional effects.
- Ignoring the system concept: Forgetting coastal systems terminology (inputs, outputs, sediment cells, feedback loops, equilibrium).
- No evaluative criteria: An answer that concludes "I agree" without evaluating severity, permanence, geographic extent, or time lag.
• AO1 (8 marks): Accurate, place-specific case study detail (Level 3 = 6–8 marks).
• AO2 (8 marks): Clear, reasoned evaluation and balanced judgement linking impacts to dynamic equilibrium and sediment cells (Level 3 = 6–8 marks).
Topics
1.1.1 Option A – Coastal Landscapes · 1.1.2 Option B – Glaciated Landscapes · 1.1.3 Option C – Dryland Landscapes · Topic 1.2 Earth’s Life Support Systems · 2.a. Coastal landforms develop due to a variety of interconnected climatic and geomorphic processes. · 3.b. Submergent coastal landscapes form as sea level rises. · 4.a. Human activity intentionally causes change within coastal landscape systems. · 4.b. Economic development unintentionally causes change within coastal landscape systems. · Topic-specific skills 1.a–4.b
Question and mark scheme from the OCR A-Level Geography examination, Physical systems (01), June 2025. QuestionVault is an independent revision resource; questions remain the copyright of the awarding body.