How is a directed geological field investigation planned and carried out?
A directed field investigation answers a geological problem or question through a planned enquiry: forming a question or hypothesis, choosing a suitable site and methods, collecting data safely and systematically (measurements, samples, logs and sketches), recording it accurately and located, then analysing the data and drawing a justified conclusion while evaluating the reliability and limitations of the method; a minimum of two days of fieldwork, including such an investigation, is required.
A focused answer to the Eduqas GCSE Geology statement on the directed field investigation. Covers forming a question or hypothesis, choosing the site and methods, collecting and recording data safely and systematically, analysing it to reach a justified conclusion, and evaluating the reliability and limitations, within the required fieldwork.
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What this dot point is asking
Eduqas wants you to describe how a directed field investigation answers a geological problem through a planned enquiry: forming a question or hypothesis, choosing a suitable site and methods, collecting data safely and systematically (measurements, samples, logs and sketches), recording it accurately and located, then analysing it to reach a justified conclusion while evaluating the reliability and limitations. You also need to know that a minimum of two days of fieldwork, including such an investigation, is required. The exam tests this as planning and evaluation, not just description.
The answer
What a directed field investigation is
A directed field investigation is a structured enquiry that sets out to answer a specific geological question using field evidence, rather than just describing an area. It follows the scientific method applied to geology, and it is the kind of investigation Eduqas requires you to carry out at least once during the course.
Planning the enquiry
Good planning is where most of the marks are:
- Form a question or hypothesis. State a clear, testable prediction (for example "pebbles become more rounded along the direction of longshore drift"), ideally with a null version (no change).
- Choose a suitable site. Pick a location where the question can actually be tested and that is safe and accessible.
- Choose appropriate methods. Decide what to measure or collect and how (a consistent technique), so the data will answer the question.
- Plan the sampling. Decide how many samples and sites, and how to select them without bias (for example every fifth pebble), so the data are representative.
Collecting and recording data
In the field, data must be gathered safely and systematically:
- take measurements, samples, graphic logs and field sketches as the question requires;
- use the same method at every site so results are comparable;
- record everything in a clear table, located by grid reference and dated, measuring objectively (evidence, not expectation);
- work safely, mindful of tides, unstable faces, slippery rock and weather.
Analysing and concluding
Back from the field, the data are analysed:
- summarise with tables, graphs and simple statistics (mean, range, percentages);
- look for patterns or trends that test the hypothesis;
- draw a justified conclusion that refers explicitly to the data and states whether the hypothesis is supported.
Evaluating reliability and limitations
A conclusion is only as good as the data behind it, so you must evaluate:
- Reliability: were measurements repeated, the method kept consistent, and enough samples and sites used?
- Limitations: small sample size, measurement error or subjectivity, too few or biased sites, restricted access, and uncontrolled variables.
- Improvements: how the investigation could be made more reliable (more samples, more sites, a more objective method).
Evaluation shows how much confidence to place in the conclusion and is heavily rewarded in the exam.
Examples in context
Example 1. Roundness along a beach. A classic investigation tests whether pebbles round downdrift: measure roundness at several located sites with a consistent method, plot the trend, conclude, and evaluate sample size and the subjectivity of judging roundness.
Example 2. Comparing two rock units. An investigation might compare the grain size of two sandstone units to infer their environments, collecting measured samples from each, analysing the means and ranges, and evaluating how representative the sampling was.
Try this
Q1. State what should be formed at the start of a directed field investigation. [1 mark]
- Cue. A clear, testable question or hypothesis.
Q2. Explain why a large, unbiased sample improves a field investigation. [2 marks]
- Cue. A large, unbiased sample is more representative of the whole, so the results and conclusion are more reliable and less affected by chance or selection bias.
Q3. Give one limitation a student might note when evaluating a field investigation. [1 mark]
- Cue. Any one of: small sample size; measurement error or subjectivity; too few sample sites; restricted or unsafe access; uncontrolled variables.
Exam-style practice questions
Practice questions written in the style of WJEC Eduqas exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.
Eduqas 20226 marksA student plans a field investigation to test whether pebbles on a beach become more rounded along the direction of longshore drift. Describe how they should plan and carry out the investigation to make it reliable.Show worked answer →
Take the enquiry through its stages: question, method, sampling, recording and reliability.
- The question or hypothesis
- State a clear, testable hypothesis: pebbles become more rounded in the direction of longshore drift (and a null version: there is no change).
- The method and sites
- Choose several sample points along the beach in the drift direction, located by grid reference, and at each measure the roundness of a set of pebbles using a consistent method (for example a roundness chart or measuring corners).
- Sampling fairly
- Take a large enough sample at each site (say 20 to 30 pebbles) and select them without bias (for example every fifth pebble along a line), to make the data representative.
- Recording
- Record results in a table, located and dated, measuring objectively and safely (tides, slippery rocks).
- Reliability
- Repeat measurements, keep the method identical at every site, and use enough sites and pebbles. Markers reward a testable hypothesis, located sample sites, a consistent unbiased sampling method, accurate recording, and steps that improve reliability."
Eduqas 20195 marksAfter collecting field data, a student concludes that their hypothesis is supported. Explain why they must also evaluate the reliability and limitations of their investigation, and give two examples of limitations they might mention.Show worked answer →
Explain the purpose of evaluation, then give two valid limitations.
Why evaluate. A conclusion is only as trustworthy as the data behind it. Evaluating the reliability and limitations shows how much confidence to place in the conclusion, identifies sources of error, and suggests how the investigation could be improved. Without it, a conclusion could rest on flawed or insufficient data.
Two limitations (any two). A small sample size, which may not be representative; measurement error or subjectivity (for example judging roundness by eye); too few sample sites; uneven or biased sampling; the difficulty of access or safety limiting where data could be taken; and uncontrolled variables (other processes affecting the result).
Markers reward the purpose of evaluation (judging confidence, finding errors, improving the method) and two genuine limitations such as small sample size, measurement error, or too few or biased sample sites."
Related dot points
- Fieldwork involves recording observations systematically: making annotated field sketches, recording rock type, colour, grain size, texture, structures and fossils, measuring features such as dip and bed thickness, and identifying hand specimens of minerals and rocks using their physical properties; observations must be objective, located on a map or grid reference, and recorded safely and accurately so they can be interpreted later.
A focused answer to the Eduqas GCSE Geology statement on field observation. Covers recording observations systematically (annotated field sketches, rock type, grain size, texture, structures, fossils), measuring features in the field, identifying hand specimens by physical properties, and recording objectively, located and safely.
- A simplified geological map shows the distribution of rock units at the surface using colours and a key, with a scale, a north arrow and grid lines; features are located using grid references (four-figure for a square, six-figure for a precise point), and the map is read together with topography to identify the rock units present, the order of the beds, and structures such as folds and faults shown by the outcrop pattern.
A focused answer to the Eduqas GCSE Geology statement on geological maps. Covers what a simplified geological map shows (rock units, key, scale, north arrow, grid), how to give four-figure and six-figure grid references, and how the outcrop pattern reveals the rock units, the order of beds and structures.
- A geological cross-section is a vertical slice through the ground constructed from a map by transferring the topography and the boundaries of the rock units onto a profile and drawing the beds at their measured dip; a graphic (sedimentary) log records a vertical sequence of beds to scale, showing thickness, grain size, rock type and structures; both turn observations into a diagram from which the order of beds, the structures and the geological history can be read.
A focused answer to the Eduqas GCSE Geology statement on cross-sections and logs. Covers how a cross-section is built from a geological map (topographic profile, transferring boundaries, drawing the dip), how a graphic sedimentary log records a vertical sequence to scale, and how both are read for the order of beds and the geological history.
- Geological investigations use quantitative skills: converting between map distance and real distance using the scale, calculating rates (of deposition, erosion or plate movement) from an amount and a time, reading and plotting graphs and gradients, and handling data with means, ranges and percentages; the distance to an earthquake epicentre can be estimated from the gap between P-wave and S-wave arrivals, and rates and ages are calculated using simple formulae and the half-life idea.
A focused answer to the Eduqas GCSE Geology statement on quantitative skills. Covers converting map distance to real distance using the scale, calculating rates of deposition, erosion and plate movement, reading graphs and gradients, handling data, and estimating epicentre distance from P-wave and S-wave arrivals.
- Sedimentary rocks form by weathering, erosion, transport, deposition, and lithification (compaction and cementation); they are classified as clastic (conglomerate, breccia, sandstone, shale), biological (limestone) or chemical (evaporites); grain size, shape, sorting, sedimentary structures and fossil content are used to interpret the depositional environment; fossils form by preservation of hard parts and record past life.
A focused answer to the Eduqas GCSE Geology statement on sedimentary rocks. Covers weathering, transport, deposition and lithification, the clastic, biological and chemical classes (conglomerate, sandstone, shale, limestone, evaporites), reading the depositional environment from grain size, sorting and structures, and how fossils form and what they record.
Sources & how we know this
- WJEC Eduqas GCSE (9-1) Geology specification (teaching from 2017) — WJEC Eduqas (2017)