100+ Free Cameroon GCE A-Level Geography Practice Questions

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The Cameroon GCE Advanced Level Geography (0750) is the official pre-university qualification administered by the Cameroon GCE Board (Buea), consisting of Paper 1 (50 MCQs, 1h30m), Paper 2 (Physical & Fieldwork, 3h), and Paper 3 (Human & Cameroon Regional, 3h15m). This 100-question practice bank delivers comprehensive preparation across physical systems, spatial theories, economic development, and Cameroon regional environmental management.

Sample Cameroon GCE A-Level Geography Practice Questions

Try these sample questions to test your Cameroon GCE A-Level Geography exam readiness. Each question includes a detailed explanation. Start the interactive quiz above for the full 100+ question experience with AI tutoring.

1Which of the following lines of evidence provided the most critical paleomagnetic confirmation for the theory of sea-floor spreading proposed by Harry Hess?

A.Symmetrical magnetic zebra-striping of alternating normal and reversed polarities recorded in basaltic rocks flanking mid-ocean ridges.

B.The exact matching of jigsaw continental margins between western South America and eastern Australia.

C.The uniform distribution of thick marine sediment layers of identical age across both oceanic trenches and ocean ridges.

D.The presence of identical active volcanic island arcs along all passive trailing continental shelves.

Explanation: Vine and Matthews (1963) confirmed sea-floor spreading by demonstrating that as basaltic magma cools at mid-ocean ridges, iron-rich minerals align with Earth's magnetic field. As Earth's magnetic field reverses periodically, symmetrical bands of alternating normal and reversed magnetic polarities are preserved on either side of the oceanic ridge crest.

2At a convergent plate boundary where an oceanic plate subducts beneath a continental plate, which distinctive seismic feature defines the inclined zone of dipping earthquake foci?

A.The Benioff-Wadati zone.

B.The Mohorovičić discontinuity.

C.The Gutenberg discontinuity.

D.The Lehmann zone.

Explanation: The Benioff-Wadati zone is a planar zone of seismicity corresponding to the down-going slab in a subduction zone. Earthquake foci become progressively deeper (ranging from shallow near the oceanic trench to deep foci up to 700 km inland) as the oceanic lithosphere sinks into the asthenosphere.

3Which landform and tectonic mechanism characteristically develop along conservative (transform) plate boundaries such as the San Andreas Fault?

A.Offset drainage channels, linear fault scarps, and shallow-focus earthquakes resulting from horizontal strike-slip shearing.

B.Deep oceanic trenches and explosive composite stratovolcanoes resulting from slab subduction.

C.Vast rift valleys flanked by high tilted fault blocks accompanied by plateau basalt outpouring.

D.Fold mountain chains with regional nappe structures formed by intense crustal shortening.

Explanation: At conservative plate boundaries, lithospheric plates slide horizontally past each other along strike-slip transform faults without creating or destroying crust. Frictional resistance produces intense shallow earthquakes, shutter ridges, fault sag ponds, and horizontally displaced (offset) stream channels.

4Which intrusive igneous landform is correctly defined as a concordant, mushroom-shaped intrusion that arches the overlying sedimentary strata upward while maintaining a relatively flat floor?

A.Laccolith

B.Lopolith

C.Phacolith

D.Batholith

Explanation: A laccolith is a concordant igneous intrusion injected between sedimentary bedding planes where viscous, acid magma forces the overlying rock layers upward into a dome or mushroom shape while retaining a relatively flat base.

5Why do shield volcanoes, such as Mauna Loa in Hawaii, exhibit broad, gentle slopes (2° to 10°) compared to the steep, conical profiles (30° or more) of composite stratovolcanoes?

A.Shield volcanoes erupt highly fluid, low-viscosity basic basaltic lava with low silica content that flows over extensive distances before solidifying.

B.Shield volcanoes erupt highly viscous, gas-rich rhyolitic lava that accumulates immediately around the vent.

C.Shield volcanoes are composed almost exclusively of pyroclastic ash and cinders deposited at their angle of repose.

D.Shield volcanoes form exclusively in deep submarine trenches where hydrostatic water pressure flattens the volcanic cone.

Explanation: Basaltic magma erupted at hot spots and divergent boundaries has low silica content (~45-52%) and high temperatures (1000°C–1200°C), making it highly fluid. These effusive basalt flows travel many kilometers across wide areas before freezing, building extensive, gently sloping volcanic shields.

6In periglacial and high-altitude alpine environments, what is the primary physical weathering mechanism responsible for breaking well-jointed bedrock into angular blockfields (felsenmeer) and scree slopes?

A.Frost shattering (gelifraction)

B.Salt crystallization (haloclasty)

C.Exfoliation due to insolation weathering

D.Biological root wedging

Explanation: Frost shattering (gelifraction) occurs when water enters joints and pore spaces in rocks and freezes. Because water expands by approximately 9% in volume upon freezing, it exerts powerful hydrostatic pressures (up to 2,100 kg/cm² at -22°C) against joint walls, eventually prizing rock fragments apart into angular scree and felsenmeer.

7Which chemical weathering reaction involves the chemical breakdown of feldspar minerals in granite into kaolinite clay, releasing soluble silica and potassium ions?

A.Hydrolysis

B.Carbonation

C.Hydration

D.Oxidation

Explanation: Hydrolysis is a chemical reaction between mineral ions and the hydrogen (H+) and hydroxyl (OH-) ions of dissociated water. When orthoclase feldspar reacts with slightly acidic water, it hydrolyzes into kaolinite (clay), dissolved silica, and potassium hydroxide.

8According to the two-stage etchplanation theory of inselberg formation developed by Falconer, Linton, and Thomas, what primary sequence of events leads to the emergence of granite bornhardts in tropical landscapes?

A.Deep subsurface chemical weathering along joint fractures forming a basal weathering front, followed by regional stripping of the weathered saprolite by fluvial and slope erosion.

B.Intense surface wind corrasion and deflation sculpting crystalline bedrock into smooth, rounded rock domes in hyper-arid conditions.

C.Direct volcanic intrusion of granitic magma reaching the surface and cooling instantaneously as steep-sided rock domes.

D.Continuous parallel scarp retreat driven exclusively by sheetwash under an arid climate without any prior chemical decomposition.

Explanation: The two-stage etchplanation model proposes that during a humid phase, intense subsurface chemical weathering (hydrolysis) penetrates deeply along widely spaced joints, etching a subterranean basal weathering surface. During a subsequent drier or tectonic uplift phase, accelerated surface erosion and sheetwash strip away the incoherent saprolite mantle (regolith), exposing massive, unjointed granite domes as bornhardts.

9Which type of mass movement is characterized by a slow, continuous downslope movement of soil and regolith under gravity, typically evidenced by tilted fence posts, curved tree trunks, and terracettes?

A.Soil creep

B.Rotational slumping

C.Rockfall

D.Debris flow

Explanation: Soil creep is the slowest form of mass wasting (typically 1–10 mm per year), driven by cyclic expansion and contraction of soil particles (freeze-thaw or wet-dry cycles) combined with gravity. Characteristic field indicators include tilted telegraph poles, leaning fences, curved 'pistol-butt' tree bases, and stepped terracettes.

10In slope evolution theory, which model argues that hillslopes maintain a constant angle of inclination while retreating backwards parallel to themselves across successive cycles of landscape denudation?

A.Lester King's Pediplanation (Parallel Retreat) Model

B.William Morris Davis's Peneplanation (Slope Decline) Model

C.Walther Penck's Slope Replacement (Waxing/Waning Development) Model

D.Grove Karl Gilbert's Dynamic Equilibrium Model

Explanation: Lester King proposed the model of pediplanation, in which steep scarps retreat parallel to themselves without losing their steep angle (parallel retreat or scarp retreat) through surface runoff and sheetwash, leaving behind gently inclined, concave bedrock pediments at the scarp foot.

About the Cameroon GCE A-Level Geography Exam

The Cameroon General Certificate of Education (GCE) Advanced Level Geography (Subject Code 0750) is the national matriculation examination administered by the Cameroon GCE Board (CGCEB) in Buea for Upper Sixth students. The curriculum provides an in-depth foundation across physical, human, regional, and environmental geography. The examination is structured into three papers: Paper 1 consists of 50 compulsory multiple-choice questions (1h 30m); Paper 2 covers Geomorphology, Climatology, Biogeography, Hydrology, Map Analysis, and Fieldwork Research Methods (2h 30m); and Paper 3 assesses Population Geography, Settlement Systems, Agricultural and Industrial Economics, Development Models, and the comprehensive Regional Geography and Environmental Hazards of Cameroon (2h 30m). Candidates must demonstrate advanced spatial synthesis, graphical and numerical calculation competence, critical evaluation of geographical theories (Davis, King, Penck, Christaller, Weber, von Thünen, Myrdal, Prebisch-Singer), and empirical understanding of Cameroon's physical relief, agro-industrial complexes (CDC, SOCAPALM, SODECOTON), drainage networks (Sanaga, Benue, Congo, Chad), and environmental management challenges (Lake Nyos limnic degassing, volcanic hazards of Mt Cameroon, Douala estuarine flooding, and Far North desertification). This 100-question practice bank covers the complete knowledge syllabus. Format note: this site's practice bank is 100 four-option multiple-choice questions covering the whole official syllabus. Paper 1 of the real examination is genuinely multiple choice (50 compulsory questions), so the format matches that paper, but the bank is a study aid only — it does not simulate the written theory/essay paper(s) or any practical examination, and its length does not describe the official exam.

Assessment

Official Advanced Level structure for subject code 0750 (Geography) per the Cameroon GCE Board June 2026 timetable (Form G6): Paper 1: 50 compulsory multiple-choice questions (1 hour 30 minutes); Paper 2: written theory/structured questions (3 hours); Paper 3: written paper (3 hours 15 minutes). Total written time is 7 hours 45 minutes. The Board does not publish per-paper mark weightings for individual subjects.

Time Limit

Paper 1: 1 hour 30 minutes; total written time 7 hours 45 minutes.

Passing Score

Grade E or better (Cameroon GCE Advanced Level grades A, B, C, D and E are passes; O is a subsidiary pass and F is a fail)

Exam Fee

12,000 FCFA (Cameroon General Certificate of Education Board (CGCEB))

Cameroon GCE A-Level Geography Exam Content Outline

25%

Geomorphology & Hydrology

Comprehensive physical geomorphology: plate tectonics, sea-floor spreading paleomagnetism, Benioff subduction zones, transform strike-slip faults, intrusive igneous forms (laccoliths, batholiths, dykes, sills), volcanic landforms and lava rheology, physical weathering (gelifraction, haloclasty), chemical weathering (hydrolysis, carbonation, oxidation), two-stage etchplanation and bornhardts, mass movements (soil creep, rotational slumping, debris flows), slope evolution theories (W.M. Davis slope decline, Walther Penck slope replacement, Lester King pediplanation parallel retreat), slope stability Factor of Safety and pore water pressure, Hjulström entrainment curve, fluvial transport mechanics (traction, saltation, suspension), river landforms (waterfall knickpoint retreat, helicoidal meanders, oxbows, bird's-foot deltas), drainage basin water balance (P = Q + E ± ΔS), storm hydrographs, drainage patterns (trellis, dendritic, radial), coastal marine erosion (cave-arch-stack-stump), coastal deposition (spits, tombolos, barrier islands), rias vs fjords, arid landforms (yardangs, zeugens, pediment-bajada-playa sequence), and glacial cirque evolution.

20%

Climatology, Biogeography & Soils

Comprehensive atmospheric, biogeographical, and pedological systems: solar radiation budget, planetary albedo, global tri-cellular atmospheric model (Hadley, Ferrel, Polar cells), Coriolis force deflection, West African Monsoon mechanics, seasonal ITCZ/ITD migration, Harmattan cT air mass characteristics, Köppen climate classification (Af, Am, Aw, BSh), tropical cyclogenesis conditions (SST ≥26.5°C, Coriolis, low shear), adiabatic lapse rates (DALR 9.8°C/km, SALR 5-6°C/km, ELR), orographic precipitation and rain shadow effects, ecological trophic energy efficiency (Lindeman's 10% law), Gersmehl nutrient cycling models in tropical rainforests vs savannas, plant succession (prisere, climatic climax, plagioclimax), equatorial rainforest multi-canopy adaptations (buttress roots, lianas, epiphytes, drip tips), savanna pyrophytic adaptations (Baobab water storage, Acacia taproots, thick bark), Hans Jenny's CLORPT pedogenic factors, soil processes (eluviation, illuviation, humification, calcification), master soil horizons (O, A, E, B, C, R), tropical Ferralsol laterisation and sesquioxide chemistry, soil erosion mechanisms (sheet, rill, gully), and soil conservation strategies (strip cropping, terracing).

20%

Population & Settlement

Comprehensive demographic and settlement analysis: Warren Thompson's Demographic Transition Model (Stages 1 to 5), age-sex population pyramids, expansive vs constrictive profiles, dependency ratios, Malthusian geometric check theory vs Ester Boserup's agricultural intensification theory, physiological density vs crude arithmetic density, step migration, transhumance, Wilbur Zelinsky's Mobility Transition Model, urbanization levels vs rates, Walter Christaller's Central Place Theory (threshold, range, k=3 marketing, k=4 transport, k=7 administrative principles), Mark Jefferson's Law of the Primate City vs Zipf's Rank-Size Rule, Ernest Burgess's Concentric Zone Model (Zone II in Transition), Homer Hoyt's Sector Model, Harris and Ullman's Multiple Nuclei Model, Harm de Blij's Sub-Saharan African City Model (colonial, traditional, and periodic market CBDs), urban informal economic sector dynamics, nucleated vs dispersed rural settlement determinants, Johann Heinrich von Thünen's Agricultural Land Use Model (bid-rent rings), rural-urban migration impacts on sending rural source areas, UN megacity definitions (>10 million), and the socio-spatial displacement mechanics of urban gentrification.

15%

Economic & Development Geography

Comprehensive economic and development geography: primary, secondary, tertiary, quaternary, and quinary economic activity classifications, traditional shifting cultivation (swidden/slash-and-burn) agro-ecology and fallow sustainability thresholds, commercial plantation agriculture (export monoculture, high capital, wage labor), intensive subsistence wet-rice farming vs extensive North American prairie commercial grain farming, Green Revolution High-Yielding Varieties (HYVs) and agrochemical packages, Alfred Weber's Least Cost Industrial Location Theory (Material Index MI, locational triangle, weight-losing vs weight-gaining industries), industrial agglomeration external economies of scale, footloose industry characteristics (semiconductors, pharmaceuticals), renewable (hydro, solar, wind, geothermal) vs non-renewable energy resources, Hydroelectric Power (HEP) physical and economic site prerequisites, UNDP Human Development Index (HDI: life expectancy, education, GNI PPP/capita), Gunnar Myrdal's Cumulative Causation Model (backwash vs spread effects), New International Division of Labor (NIDL) and TNC production networks, Prebisch-Singer Thesis on deteriorating primary commodity Terms of Trade, and regional economic integration stages (Free Trade Areas vs Customs Unions, CEMAC, AfCFTA).

20%

Regional Geography of Cameroon & Environmental Management

Comprehensive regional synthesis of Cameroon: Cameroon Volcanic Line (CVL) structure, Mount Cameroon (Fako, 4,095 m), Western Highlands (Grassfields) volcanic soils, temperate microclimate, Fondoms and high population density, Coastal Lowlands and Douala/Rio del Rey sedimentary basins, South Cameroon Precambrian Plateau, dense evergreen rainforests and cocoa production, Adamawa Plateau water tower (château d'eau) and Fulani/Mbororo Gudali zebu cattle rearing, Northern Plains (Benue Basin and Diamaré plain) and Yaéré seasonal floodplains (Muskwari receding-flood sorghum), Sanaga River hydroelectric power cascade (Edéa, Song Loulou, Nachtigal, Lom Pangar storage), Cameroon's four continental drainage basins (Atlantic, Niger-Benue, Congo-Sangha, Lake Chad), Arabica coffee (Western Highlands) vs Robusta coffee (coastal/southern lowlands), Cameroon Development Corporation (CDC) parastatal plantations (rubber, palm oil, bananas), SODECOTON contract outgrower farming and ginning factories in northern Cameroon, 1994 Forestry Law and Forest Management Units (UFAs), petroleum extraction (SNH, SONARA refinery at Limbe, Chad-Cameroon pipeline), Kribi Deep Seaport at Mboro, industrial concentration in Douala (Bassa, Bonabéri), Lake Nyos (1986) and Lake Monoun (1984) limnic carbon dioxide overturn disasters, Mount Cameroon effusive basaltic lava flow hazards (1999 Bakingili flow), chronic urban flooding in Douala informal quarters (mangrove clearance, tidal blockage), Congo Basin tropical deforestation drivers, and desertification management in the Far North (Opération Sahel Vert and the Pan-African Great Green Wall).

How to Pass the Cameroon GCE A-Level Geography Exam

What You Need to Know

Passing score: Grade E or better (Cameroon GCE Advanced Level grades A, B, C, D and E are passes; O is a subsidiary pass and F is a fail)
Assessment: Official Advanced Level structure for subject code 0750 (Geography) per the Cameroon GCE Board June 2026 timetable (Form G6): Paper 1: 50 compulsory multiple-choice questions (1 hour 30 minutes); Paper 2: written theory/structured questions (3 hours); Paper 3: written paper (3 hours 15 minutes). Total written time is 7 hours 45 minutes. The Board does not publish per-paper mark weightings for individual subjects.
Time limit: Paper 1: 1 hour 30 minutes; total written time 7 hours 45 minutes.
Exam fee: 12,000 FCFA

Keys to Passing

Work through all 100 available questions
Review every answer and explanation
Track weak areas and revisit them
Use our AI tutor for tough concepts

Cameroon GCE A-Level Geography Study Tips from Top Performers

1Master Quantitative Geography Formulas: Regularly practice calculating topographic gradients, map scales, adiabatic cooling lapse rates (9.8°C/km DALR), drainage basin water budgets, population densities, and Weberian Material Indices without relying on automated software.

2Integrate Physical Processes with Theoretical Models: Ensure you can clearly contrast William Morris Davis's slope decline, Walther Penck's slope replacement, and Lester King's parallel retreat, as well as the two-stage etchplanation model for tropical bornhardt formation.

3Draw Clear Annotated Geographical Diagrams: The GCE marking schemes award substantial credit for well-labeled sketch diagrams, including storm hydrographs, Gersmehl nutrient cycling triangles, Burgess/Hoyt urban diagrams, and atmospheric tri-cellular circulation cells.

4Master Cameroon's Five Major Physical Regions: Build comprehensive summary matrices comparing the Western Highlands, Coastal Lowlands, South Cameroon Plateau, Adamawa Plateau, and Northern Plains across geology, soils, climate, drainage, human settlement, and primary cash crops.

5Thoroughly Review Environmental Hazards in Cameroon: Master the physical triggering mechanisms, socio-economic impacts, and mitigation engineering for the 1986 Lake Nyos limnic disaster, Mount Cameroon volcanic eruptions, Douala mangrove flood dynamics, and Opération Sahel Vert.

Frequently Asked Questions

What is the structure of the Cameroon GCE Advanced Level Geography (0750) examination?

The Cameroon GCE Advanced Level Geography examination consists of three separate written papers administered over the national examination session in May/June: Paper 1 consists of 50 compulsory multiple-choice questions (1 hour 30 minutes); Paper 2 focuses on Physical Geography, Topographic Mapwork, and Field Research Methods (4 structured/essay questions from 8 choices, 2 hours 30 minutes); and Paper 3 evaluates Human Geography, Economic Theories, and the Regional Geography and Environmental Hazards of Cameroon (4 structured/essay questions from 8 choices, 2 hours 30 minutes).

What grading scale and university matriculation points are used by the Cameroon GCE Board?

The Cameroon GCE Board reports Advanced Level results on the letter scale A, B, C, D, E, O and F. Grades A to E are passes, Grade O is recorded as a subsidiary (Ordinary Level) pass and Grade F is a fail. The Board does not publish the percentage mark ranges behind these grades.

How much does it cost to register for the GCE Advanced Level Geography examination?

Official CGCEB candidate registration fees consist of a mandatory candidate base registration fee of 9,000 FCFA, an individual subject fee of 2,000 FCFA for Geography, and an administrative/practical levy of 1,000 FCFA (totaling 12,000 FCFA for a candidate registering Geography alongside other subjects).

What quantitative and calculation skills are required on the GCE A-Level Geography exam?

Candidates are required to perform precise mathematical calculations, including: topographic map scale conversions, gradient and slope percentage calculations, drainage basin water balance budgets (P = Q + E ± ΔS), storm hydrograph lag time and peak discharge derivations, dry and saturated adiabatic lapse rates (DALR/SALR), demographic metrics (crude and physiological population densities, dependency ratios), and industrial Material Index (MI) calculations under Weber's least-cost model.

Why is the Regional Geography of Cameroon such a major component of this examination?

Paper 3 of the Cameroon GCE syllabus dedicates half of its weighting to Cameroon Regional Geography. Candidates must have in-depth empirical knowledge of Cameroon's physical relief units (Western Highlands, Adamawa, Coastal Lowlands, South Cameroon Plateau, Northern Plains), continental drainage basins, agricultural cash crops and parastatals (CDC, SODECOTON, SOCAPALM), energy infrastructure (Sanaga hydroelectric dams, SNH/SONARA petroleum), and major environmental hazards (Lake Nyos limnic gas disaster, Douala flooding, and Far North desertification).

100+ Free Cameroon GCE A-Level Geography Practice Questions

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