OCRAS Level6 resources
OCR AS Level Geology Past Papers
Download OCR AS Level Geology (H014) past papers and mark schemes. Geological processes, rock identification, and Earth history. 3 resources.
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June series (legacy and current)π6 resources availableβ
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6 of 6 resources
June 2023
2 filesJune 2022
2 filesNovember 2020
1 fileβ
Geology β Mark schemes
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1 fileπ
Geology β AS Geology
Sample Assessment Materials
Rock Formation, Geological Time, and Tectonic Processes in AS Geology
OCR AS Level Geology (H014) introduces students to the study of Earth's materials, processes, and history, developing both practical rock and mineral identification skills and conceptual understanding of the geological processes that shape the planet over vast timescales. The qualification is assessed through written papers that draw on data interpretation and applied geological reasoning.
The AS Level geology syllabus covers five main content areas. Earth materials covers the three rock types β igneous (intrusive and extrusive, classified by silica content and grain size), sedimentary (clastic, chemical, and biogenic, and the sedimentary environments that produce them), and metamorphic (contact and regional metamorphism, the effects of temperature and pressure on rock texture and mineralogy) β together with mineral identification using physical properties (hardness using the Mohs scale, cleavage and fracture, colour and streak, lustre, specific gravity, and crystal form).
Earth processes covers plate tectonic theory (the evidence for plate movement β paleomagnetism, seafloor spreading, the distribution of earthquakes and volcanoes β and the geological consequences of constructive, destructive, and conservative plate boundaries), geological structures (folds and their classification, faults and their types, unconformities), and geophysical methods used to investigate Earth's interior.
Earth history covers the geological time scale, the fossil record and its use in biostratigraphy (the use of index fossils to correlate rock sequences and determine relative age), radiometric dating principles (the decay of radioactive isotopes and how this allows absolute dating), and the history of life on Earth including major extinction events.
Geological map reading and interpretation is a central practical skill: candidates must be able to read topographic and geological maps, identify rock types from map symbols, determine dip direction from outcrop patterns, construct and interpret geological cross-sections, and recognise structural features from map evidence.
Exam Paper Structure
Paper 1Calculator β
Earth Materials and Processes
β± Written examinationπ― Variable marksπ 50%% of grade
Igneous, sedimentary, and metamorphic rock identificationPlate tectonic theory and boundary typesGeological structures: folds, faults, unconformitiesMineral identification using physical properties
Paper 2Calculator β
Earth History and Map Skills
β± Written examinationπ― Variable marksπ 50%% of grade
Geological time scale and biostratigraphyFossil record and major extinction eventsRadiometric dating principlesGeological map reading and cross-section construction
Key Information
| Exam Board | OCR |
| Specification Code | H014 |
| Qualification | AS Level |
| Grading Scale | AβE |
| Assessment Type | Written papers |
| Number Of Papers | 2 |
| Exam Duration | Varies by paper |
| Total Marks | Available on OCR specification |
| Calculator Status | Calculator allowed |
| Available Sessions | June series (legacy and current) |
| Total Resources | 3 |
Key Topics in Geology
Topics you need to know
Igneous rock classification by texture and silica contentSedimentary rock identification and depositional environmentsMetamorphic grade and contact vs regional metamorphismPlate tectonic boundary processesIndex fossils and biostratigraphyGeological map reading and cross-sectionsGeological time scale and radiometric dating
Exam Command Words
| Command word | What the examiner expects |
|---|---|
| Identify | Name the rock, mineral, or geological feature from the evidence provided |
| Explain | Give a geological mechanism linking cause to effect or process to outcome |
| Interpret | Draw a geological conclusion from map, cross-section, or data evidence |
| Describe | Give an accurate account of a geological feature, structure, or process |
Typical Grade Boundaries
| Grade | Approximate mark needed |
|---|---|
| A | 68β83% |
| B | 56β67% |
| C | 44β55% |
| D | 32β43% |
| E | 20β31% |
β οΈ OCR AS Geology grade boundaries vary by session.
Rock Classification, Plate Boundary Processes, and Geological Map Interpretation
Rock identification questions require systematic use of observable characteristics, not guesswork. For igneous rocks: coarse-grained texture (visible crystals β granite, gabbro) indicates slow cooling at depth; fine-grained or glassy texture (basalt, obsidian) indicates rapid cooling at the surface. Classify igneous rocks by silica content: felsic rocks (>66% SiOβ β granite, rhyolite) are light-coloured; intermediate rocks (52β66% SiOβ β diorite, andesite); mafic rocks (<52% SiOβ β gabbro, basalt) are dark-coloured and dense. For sedimentary rocks: assess grain size (gravel/conglomerate, sand/sandstone, silt/siltstone, clay/mudstone), sorting (well-sorted implies transport by wind or sustained water; poorly sorted implies rapid deposition), and any fossils or sedimentary structures (cross-bedding, ripple marks, graded bedding).
For plate tectonic questions, associate each boundary type with its characteristic geological features. Constructive (divergent) boundaries produce basaltic volcanism, shallow earthquakes, and new oceanic crust β the Mid-Atlantic Ridge and East African Rift are examples. Destructive (convergent) boundaries produce subduction zones where oceanic crust descends beneath continental or oceanic crust, generating andesitic or calc-alkaline volcanism, deep earthquakes along the Benioff zone, ocean trenches, and fold mountains β the Andes and Japan are examples. Conservative (transform) boundaries produce shallow strike-slip earthquakes but no volcanism β the San Andreas Fault is the classic example.
For geological map cross-sections: plot the topographic profile first using the contour lines; then project each rock boundary onto the cross-section, maintaining the dip angle shown on the map. Rocks dipping toward the observer appear to be at shallower angles on the cross-section than their true dip; use the tangent of the dip angle to ensure accurate projection. Annotate the completed cross-section with formation names, dip directions, and any structural features (faults, unconformities).
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