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 question

Question

Exam paper section titled 'Option A – Coastal Landscapes'. Question 1(a) asks to explain the influence of flows of energy in the formation of a salt marsh (8 marks). Question 1(b) provides Table 1 showing cliff erosion rates in metres per year for 10 locations on the East Yorkshire coast: 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), and Spurn neck (3.10). Sub-questions (i) asks to calculate the mean rate of erosion showing workings (2 marks), (ii) asks what a standard deviation of 0.8 indicates about data dispersion (2 marks), and (iii) asks to explain why standard deviation is more accurate than range and interquartile range (2 marks). Question 1(c) asks to explain the influence of one geomorphic process in shaping a fjord with reference to Fig. 1 (3 marks). Question 1(d)* is an evaluative essay asking to what extent coastal landscape systems are influenced more by management strategies than by the unintentional impacts of economic development (16 marks).
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 Mark scheme for Question 1. For 1(a), Level 3 (6-8 marks) requires thorough knowledge of flows of energy (kinetic, thermal, gravitational) and well-developed ideas on how energy reduction creates depositional features of salt marshes. For 1(b)(i), calculation shows the sum 14.6 divided by 10 giving a mean value of 1.46 m/year (2 marks). For 1(b)(ii), notes that standard deviation of 0.8 indicates reasonable or limited clustering around the mean, with 68% between 0.66 and 2.26, or 80% within 1 SD (2 marks). For 1(b)(iii), explains SD uses all data values rather than just extremes (range) or middle 50% (IQR) and is less affected by anomalies (2 marks). For 1(c), identifies and explains one geomorphic process shaping a fjord, such as freeze-thaw weathering, marine erosion, or glacial plucking/abrasion (3 marks). For 1(d)*, Level 3 AO1 (6-8 marks) and AO2 (6-8 marks) require comprehensive place-specific detail of intentional management versus unintentional economic impacts with sustained, substantiated evaluative judgements.

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

What this question tests

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.
Part (a) · 8 Marks

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.
Mark Scheme: Level 3 (6–8 marks) requires thorough knowledge with well-developed ideas showing a clear appreciation of energy flows (AO1).
Part (b) · 6 Marks Total

Quantitative Skills: Cliff Erosion Rates & Measures of Dispersion

Part (b)(i): Mean Calculation [2 Marks]

📐 Step-by-Step Calculation

  1. 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
  2. Divide by the number of sites (n = 10):
    14.60 ÷ 10 = 1.46
  3. 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 ).
Mark allocation: 1 mark for correct working shown, 1 mark for correct calculated mean (1.46).

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).

Mark allocation: 1 mark for general point about dispersion; 1 mark for specific calculation/point about data spread.

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.

Mark allocation: 1 mark for comparison with Range; 1 mark for comparison with IQR.
Part (c) · 3 Marks

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)
Examiner Note: Naming a process alone is not sufficient. You must explicitly unpack the process and connect it directly to the landform visible in the figure.
Part (d)* · 16 Marks

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.
Mark Scheme Breakdown (16 marks total):
• 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.