Comprehensive Geography Study Guide - Year 10 Senior Secondary
Overview and Scheme of Work
School: King's Care Universal School ("…a school with a difference")
Subject: Geography E-Notes
Level: Year
Term: Summer Term
Author: Mr. Adeniyi Femi
Primary Reference Text: Essential Geography for Senior Secondary Schools by O.A. Iwena
Summer Scheme of Work Schedule
Week : Basic concepts of GIS (Definition of terms, Components of GIS)
Week : Earth's external processes (Action of running water)
Week : Action of wind (Features of wind erosion)
Week : Action of glacier
Week : Action of waves
Weeks : Types of climate (Hot: Equatorial and Sudan climate; Cold: Polar and Tundra; Desert: hot and cold; Temperate climate) and Classification of climate (Greek system, Koppen's system)
Week : Environmental resources (Types of resources, Renewable and non-renewable)
Week : Revision
Week : Examination
Week 1: Basic Concepts of Geographic Information System (GIS)
Definition of GIS
Geographic Information System (GIS) is a computer-based system used to collect, store, analyse, manage, and display geographically referenced data (spatial data).
Core Functions of GIS in Simple Terms:
Study the Earth
Analyse locations
Understand patterns and relationships in space
Key Terms in GIS
Geography: The study of the earth and its features, and the relationship between people and their environment on earth.
Data: Raw facts or figures that can be processed.
Spatial Data: Data that has a location on the Earth's surface.
Examples:
Location of Abuja
Rivers in Nigeria
Distribution of rainfall
Attribute Data: Descriptive information about spatial data.
Examples:
Population of Abuja
Length of River Niger
Annual rainfall amount
Information: Processed data that is meaningful.
System: A set of connected parts working together.
Remote Sensing: The use of satellites or aircraft to obtain information about the Earth without physical contact.
GPS (Global Positioning System): A satellite-based navigation system used to determine exact locations on Earth.


Components of GIS
Hardware: Physical equipment used in GIS.
Examples: Computers, GPS devices, Printers, Scanners, Plotters
Software: Programs used to process GIS data.
Examples: ArcGIS, QGIS, Google Earth
Data: This is the most important part of GIS. It includes Spatial data and Attributive data.
Primary Data Sources:
Satellite imagery
Field survey
Maps
Census data
People: Trained personnel who operate GIS.
Examples: Geographers, Surveyors, Environmental planners, Urban planners
Methods (Procedures): Rules and techniques for collecting and analysing data.
Functions of GIS
Produce maps and store geographical data
Support decision-making
Carry out urban planning
Predict environmental changes
Assist in disaster management
Support agricultural planning
Support transportation planning
Enhance resource management
Analyse patterns and relationships in space
Applications of GIS
Applications in Nigeria:
Flood mapping in the Niger Delta
Election boundary demarcation
Mining and oil exploration
Urban planning in major cities such as Abuja and Lagos
Environmental impact assessment
Global Applications:
Climate change studies
Disaster monitoring (e.g., earthquakes, hurricanes)
Disease tracking
Limitations of GIS
High cost of software
Requirement for specialized, trained experts
Data collection processes can be expensive
Technical errors may occur during data processing
Power supply instabilities (especially in developing countries like Nigeria)
Review Questions
. Define Geographic Information System (GIS).
. Explain the term spatial data.
. Differentiate between spatial and attributive data.
. List and explain the five main components of GIS.
. Mention three sources of GIS data.
. What is vector data?
. What is raster data?
. State three uses of GIS in Nigeria.
. Explain the importance of GIS in urban planning.
. What is remote sensing?
. Define GPS.
. Mention three GIS software.
. State four functions of GIS.
. Outline four advantages of GIS.
. State three limitations of GIS.
. Explain the relationship between GIS and geography.
. Describe the role of people in GIS.
. Mention two types of data used in GIS.
. Explain how GIS helps in disaster management.
. Differentiate between hardware and software in GIS.
Reference
Essential Geography for Senior Secondary Schools by O.A. Iwena, pages .
Week 2: Earth's External Processes – Action of Running Water
Meaning of Earth's External Processes
Earth's external processes are natural activities or processes that occur on the surface of the Earth, leading to the creation or modification of various landforms.
Primary Agents:
Running water
Wind
Glaciers
Waves
Fundamental Geological Operations:
Erosion
Transportation
Deposition
Stages of River Development
Early stage or Upper course of a river
Mature stage or Middle course of a river
Old stage or Lower course of a river

Major River Systems
Rivers in Nigeria:
Niger
Benue
Cross
Kaduna
Sokoto
Owena
Osun
Ogun
Anambra
Imo
Hadejia
Gongola
Taraba
Donga
Major Rivers in Africa:
Nile
Niger
Senegal
Congo
Orange
Limpopo
Zambezi
Volta
Okavango
Chari
Processes of River Action
. Erosion (Wearing away of the land surface):
Hydraulic action: The physical force of moving water dislodging material.
Abrasion (corrasion): The wearing away of the river bed and banks by materials carried by the river.
Attrition: The wear and tear that occurs when boulders and stones collide with each other and break into smaller pieces.
Solution (corrosion): The chemical action of river water dissolving soluble rocks (e.g., limestone).
Note: Corrasion (mechanical wearing) is distinct from corrosion (chemical dissolving).
. Transportation (Movement of eroded materials):
Solution: Dissolved mineral matter is carried along invisibly.
Suspension: Fine particles like clay and silt are held up within the water body.
Saltation: Medium-sized pebbles and particles bounce along the river bed.
Traction: Large boulders and heavy materials roll or slide along the river bed.
. Deposition (Dropping of transported materials when velocity drops):
Primary locations of deposition:
Lower course of the river
Inside bends of meanders
At the river mouth or terminus
Characteristics and Features of River Stages
Upper Course:
Characteristics:
Steep slope gradient
Fast water flow
Vertical and headward erosion are dominant
Landform Features:
Interlocking spurs
Waterfalls
V-shaped valleys
River capture
Plunge pools
Rapids and cataracts
Pot holes
Gorges
Middle Course:
Characteristics:
Gentle slope
Lateral erosion becomes dominant
Deposition begins to occur
Water volume increases
Flow speed reduces
Landform Features:
Wide U-shaped valley
Meanders
Beginning of flood plains (depositional feature)
River cliffs and slip-off slopes
Lower Course:
Characteristics:
Very gentle slope / nearly flat land
Deposition is the primary action
Landform Features:
Wide flood plains
Natural levees
Deltas:
Arcuate delta: Nile, Niger, and Po rivers
Bird's foot delta: Omo and Mississippi rivers
Estuarine delta: Amazon and Ob rivers
Oxbow lakes
Braided stream
Drainage Patterns
Dendritic Drainage: Irregular branching structure resembling the veins of a leaf or tree branches.
Trellis Drainage: Tributaries join the main stream at right angles following rock structures.
Radial Drainage: Streams flow outwards and downhill from a central elevated point such as a crater or lava cone.
Review Questions
. Define erosion.
. List four processes of river erosion.
. Explain attrition.
. Differentiate between erosion and deposition.
. List four methods of river transportation.
. Describe features of the upper course.
. Explain formation of waterfalls.
. What is a gorge?
. Describe the mode of formation of meanders.
. What is an oxbow lake? How does it form?
. Define flood plain.
. State the characteristics of lower course.
. What is a delta?
. Explain how levees are formed.
. Mention two Nigerian rivers.
. Describe River Niger briefly.
. State three erosional landforms.
. State three depositional landforms.
. Explain lateral erosion.
. Outline importance of rivers.
Reference
Essential Geography for Senior Secondary Schools by O.A. Iwena, pages .
Week 3: Action of Wind
Wind as an Agent of Erosion
Wind is the principal agent of erosion, transportation, and deposition in arid (desert) and semi-arid regions.
Major Global Deserts:
Sahara (West Africa)
Namib (South Africa)
Atacama (South America)
Mohave (USA)
Processes of Wind Action
Processes of Wind Erosion:
Deflation: The blowing away and lifting of loose, dry particles of rock, sand, and dust.
Abrasion: Sand-charged winds blast and sand-paper exposed rock surfaces.
Attrition: Air-borne sand particles collide against each other, breaking into smaller, rounded grains.
Processes of Wind Transportation:
Suspension: Fine dust particles held in the air and carried over vast distances.
Saltation: Sand grains bouncing along the ground surface in a series of leaps.
Surface creep: Heavy, coarse sand particles rolling or sliding along the ground.



Landforms produced by Wind Action
Erosional Features:
Deflation hollows
Desert pavement (deflation lag)
Inselbergs
Yardangs
Zeugens
Rock pedestals
Mesas and buttes
Depositional Features:
Sand dunes:
Barchan dune (crescent-shaped dune)
Seif dune (longitudinal ridge)
Transverse dune
Blowout dune
Parabolic dune
Barchanoid ridge
Dome dune
Loess: Fine, fertile, yellow silt wind-borne and deposited far outside desert regions.
Review Questions
. Define deflation.
. Explain abrasion.
. Mention three wind erosion processes.
. What is a yardang?
. Describe desert pavement.
. Explain formation of sand dunes.
. Mention three types of dunes.
. What is loess?
. Differentiate between wind and river erosion.
. State importance of wind deposition.
. Explain attrition in wind action.
. Where is wind action most effective?
. What is surface creep?
. Describe barchan dune.
. Mention two deserts.
. Explain Sahara Desert briefly.
. State three erosional features of wind action.
. State three depositional features of wind action.
. Outline disadvantages of wind erosion.
. Suggest control measures.
Reference
Essential Geography for Senior Secondary Schools by O.A. Iwena, pages .
Week 4: Action of Glacier
Meaning and Distribution of Glaciers
A glacier is a massive body of ice formed from accumulated, compacted snow that moves slowly downhill over land under the influence of gravity.
Geographic Distribution:
Polar regions (Greenland, Antarctica)
High mountain ranges (Himalayas, Alps, Rockies)
Types of Glaciers
Valley (Alpine) Glacier: Glaciers confined within mountain valleys.
Continental Glacier (Ice Sheet): Massive ice sheets covering vast continental areas.
Processes of Glacial Erosion
Plucking:
Meltwater freezes into rock joints and cracks on the valley bed.
As the glacier moves forward, it pulls and tears away rock fragments.
Abrasion:
Rock fragments embedded in the base and sides of the moving glacier scour and rasp the bedrock surface.
Leaves smooth, polished, and striated rock surfaces.

Glacial Landforms
Erosional Features:
Cirque (Corrie): An armchair-shaped or bowl-shaped hollow at the head of a mountain valley.
Formation: Snow accumulates in a mountain basin; freeze-thaw weathering, plucking, and abrasion deepen it; melting leaves a steep-sided basin.
Arête: A steep, knife-edged rock ridge formed between two adjacent cirques eroding backwards into each other.
Pyramidal Peak (Horn): A sharp, pointed mountain summit created when three or more cirques erode headwards into the same peak.
U-Shaped Valley (Glacial Trough): A steep-sided, flat-bottomed valley created when a glacier widens, deepens, and straightens a pre-existing V-shaped river valley.
Hanging Valley: A tributary valley ending high above the main glacial trough floor, often forming waterfalls.
Formation: Main glacier erodes deeper than tributary glacier.
Depositional Features:
Moraines: Ridge-like accumulations of glacial debris (till).
Types: Lateral moraine (along valley sides), Medial moraine (down the center where two lateral moraines join), Terminal moraine (at the maximum extent of the glacier snout).
Drumlin: An elongated, oval-shaped hill ("egg-shaped") composed of unsorted glacial till.
Formation: Deposited under moving ice and streamlined parallel to ice flow.
Esker: A long, winding, serpentine ridge of stratified sand and gravel deposited by meltwater streams flowing beneath a melting glacier.
Review Questions
. Define glacier.
. Mention two types of glaciers.
. Explain plucking.
. Describe abrasion.
. What is a cirque?
. Explain formation of arête.
. Describe pyramidal peak.
. Differentiate U-shaped and V-shaped valley.
. What is a hanging valley?
. Define moraine.
. Mention types of moraines.
. Explain drumlin formation.
. Describe esker.
. State two erosional features.
. State two depositional features.
. Where are glaciers found?
. Mention one effect of glaciation.
. Explain continental glacier.
. Describe valley glacier.
. Outline importance of glacial landforms.
Reference
Essential Geography for Senior Secondary Schools by O.A. Iwena, pages .
Week 5: Action of Waves
Waves as an Agent of Marine Coastal Processes
Ocean waves are generated by wind friction blowing across the sea surface. Waves continuously shape coastlines through erosion, transportation, and deposition.
Processes of Marine Erosion
Hydraulic Action: The direct force of breaking waves striking coastal cliff faces and trapping air in cracks, expanding crevices.
Abrasion: Waves hurl rock fragments, pebbles, and sand against cliff bases, grinding rock down.
Attrition: Transported rock fragments continually collide against each other, grinding down into rounded pebbles and sand grains.
Solution (Corrosion): Dissolving of soluble coastal rock formations (e.g., chalk, limestone) by coastal water chemistry.
Coastal Landforms
Erosional Features:
Sea Cliff: Steep vertical rock face facing the ocean created by wave undercut.
Wave-Cut Platform: Flat, smooth rock bench left behind at the base of a retreating cliff.
Sequential Cave-Arch-Stack-Stump Complex:
Cave: Deepened hollow at a weakness in the cliff face.
Arch: Cave eroded entirely through a headland.
Stack: Isolated pillar of rock standing in sea water left when an arch collapses.
Stump: Undercut, collapsed stack base visible primarily at low tide.
Depositional Features:
Beach: Accumulation of sand, shingle, and pebbles along the shoreline.
Spit: Long, narrow ridge of sand or shingle connected to land at one end, extending out into open water due to longshore drift.
Tombolo: Sand ridge or bar connecting an island to the mainland.
Sandbar: Submerged or exposed ridge of sand parallel to the coastline.
Review Questions
. Define waves in geography.
. Explain the term marine erosion.
. List and explain four processes of wave erosion.
. What is hydraulic action?
. Explain abrasion as a process of coastal erosion.
. Define attrition in relation to wave action.
. What is solution (corrosion) in coastal processes?
. Describe how a sea cliff is formed.
. Explain the formation of a wave-cut platform.
. Describe the stages involved in the formation of cave, arch, stack, and stump.
. What is a coastal cave?
. Explain how a sea arch is formed.
. Describe the formation of a stack.
. What is a beach? Explain how it is formed.
. Define longshore drift.
. Explain the formation of a spit.
. What is a tombolo? Describe its formation.
. Differentiate between erosional and depositional coastal features.
. Mention three erosional and three depositional features of waves.
. State four ways in which wave action affects human activities along the coast.
Reference
Essential Geography for Senior Secondary Schools by O.A. Iwena, pages 260\text{–}265$.\n\n# Weeks 6–9: Types and Classification of Climate\n\n## Hot Climates\n\n- Equatorial Hot Climate:\n - Geographic Location: 0^ullet\text{–}5^ullet\text{ North and South} (Congo Basin, Amazon Basin, Coast of West Africa)\n - Key Features:\n - High temperature (26\text{–}28\,^\circ\text{C}) sustained throughout the year\n - Heavy annual rainfall exceeding 2000\,\text{mm} with no distinct dry season\n - High relative humidity (consistently over 80\%)\n - Dense equatorial rainforest vegetation with thin undergrowth\n - Heavy cloud coverage\n - Economic Activities: Lumbering, hunting, plantation farming, fishing\n- Sudan Hot Climate (Tropical Savanna):\n - Geographic Location: 5^\circ\text{–}20^\circ\text{ North and South} (Northern Nigeria, Ghana, Sudan, East Africa, Brazil [Campos], Bolivia, Australia, India, Southeast Asia)\n - Key Features:\n - Alternating distinct wet and dry seasons\n - Annual rainfall ranging between 1000\,\text{mm}1500\,\text{mm}\n - Vegetation dominated by tall grasses and scattered short trees\n - Clear, cloudless skies during dry seasons\n - Economic Activities: Pastoral livestock farming, arable crop farming, hunting, wildlife reserves / tourism\n\n## Desert Climates\n\n- Hot Desert Climate:\n - Geographic Location: 15^\circ\text{–}30^\circ\text{ North and South}\n - Key Features:\n - Extremely high daytime temperatures\n - Very low annual precipitation (< 250\,\text{mm})\n - Rare, sudden, violent convectional downpours\n - Cloudless skies with high diurnal temperature ranges\n - Drought-resistant (xerophytes) and salt-tolerant (halophytes) sparse vegetation\n - Economic Activities: Food gathering, nomadic pastoralism, mineral mining\n- Cold Desert Climate:\n - Geographic Location: 45^\circ\text{–}60^\circ\text{ North and South} (Eurasian interior, Patagonia in South America, Central Asia / Mongolia)\n - Key Features:\n - Low annual precipitation (< 250\,\text{mm})\n - Extreme annual range: hot summers (38\,^\circ\text{C}-7\,^\circ\text{C})\n - Sparse vegetation: short grasses and dry shrubs\n - Economic Activities: Food gathering, nomadic pastoralism\n\n## Cold Climates\n\n- Polar Climate:\n - Geographic Location: Around 90^\circ\text{ North and South} (Antarctica, Greenland, Iceland)\n - Key Features:\n - Temperatures remain below freezing (0\,^\circ\text{C})\n - Permanently snow and ice-covered surface (no vegetation)\n - Low precipitation (10\text{–}15\,\text{cm})\n - Violent blizzards\n - Continuous long dark winter nights and short summer days\n- Tundra Climate:\n - Geographic Location: 60^\circ\text{–}90^\circ\text{ North and South} (Northern Canada, Greenland, Alaska, Siberian Eurasia, Antarctica fringe)\n - Key Features:\n - Short, cool summers (10\,^\circ\text{C}-29\,^\circ\text{C}\text{ to }-40\,^\circ\text{C})\n - Low precipitation (250\,\text{mm})\n - Presence of permafrost (permanently frozen subsoil)\n - Vegetation: Mosses, lichens, crowberry, dwarf birch, Arctic poppy, anemone\n - Economic Activities: Hunting (Eskimos), fishing during summer\n\n## Temperate Climates\n\n- Western Warm Temperate (Mediterranean Climate):\n - Geographic Location: 30^\circ\text{–}45^\circ\text{ North and South} (Mediterranean basin, North Africa [Tunisia, Morocco, Libya], SW South Africa, Central Chile, California, France, Spain, Italy)\n - Key Features:\n - Hot, dry summers\n - Mild, wet winters (600\text{–}800\,\text{mm} rainfall)\n - Prominent local wind systems (Sirocco wind, Mistral wind)\n - Vegetation: Oak, cedar, grapevines, coniferous trees (pine, fir), acacia, laurel, rosemary, maquis scrub, grasses\n - Economic Activities: Viticulture (grape cultivation), fruit orchard farming, wheat and rice farming, pulp and paper manufacturing\n- Eastern Warm Temperate (China Type Climate):\n - Geographic Location: 20^\circ\text{–}40^\circ\text{ North and South} (Eastern margins of China, Japan, USA, Mexico, Australia, South Africa)\n - Key Features: Warm wet summers and cool dry winters\n- Western Cool Temperate (British Type Climate):\n - Geographic Location: 45^\circ\text{–}60^\circ\text{ North and South} (United Kingdom, Western Europe)\n - Key Features:\n - Warm summers and mild winters\n - Rainfall distributed evenly throughout the entire year\n - Vegetation: Deciduous trees (oak, elm, birch, beech, eucalyptus)\n - Economic Activities: Arable and market garden farming, mixed livestock farming\n- Eastern Cool Temperate (Laurentian Type Climate):\n - Geographic Location: 40^\circ\text{–}50^\circ\text{ North and South} (North-Eastern Canada, North-Eastern USA / North America)\n - Key Features:\n - Cold dry winters and warm wet summers\n - Vegetation: Coniferous trees (spruce, fir) mixed with deciduous trees (maple, birch, beech, oak)\n\n## Systems of Climate Classification\n\n- Greek Climate Classification System (Aristotle):\n - Basis: Based exclusively on temperature parameters.\n - Temperature Zones:\n - Torrid Zone: Hot central equatorial band\n - Temperate Zone: Moderate middle latitude zones\n - Frigid Zone: Extremely cold polar zones\n\n\n\n- Köppen's Climate Classification System:\n - Basis: Quantitative system using letter codes based on monthly temperature and precipitation values.\n - Primary Climate Groups:\n - Group A: Tropical moist climates (Hot and wet rain forests & Savannas)\n - Group B: Dry climates (Steppe / Semi-arid and Arid Deserts)\n - Group C: Warm temperate / Mild humid mid-latitude climates\n - Group D: Cold snowy forest climates / Severe mid-latitude winters\n - Group E: Polar / Frigid climates (Tundra and Ice Cap)\n\n## Review Questions\n\n- 1. Discuss the characteristics of Mediterranean climate.\n- 2. Oak and cedar are good examples of commercial trees common in the \_\_\_\_\_\_\_\_\_\_ climate.\n- 3. Differentiate between hot and cold desert climates.\n- 4. Highlight three differences between polar cold climate and tundra cold climate.\n- 5. What are the differences between Equatorial and Sudan climates?\n- 67 hot deserts and the country or region where they are located.\n- 7. Explain why rainfall is heavy in equatorial regions.\n- 8. Describe the main features of the tropical savanna.\n- 9. State two countries in which tropical savanna climate is found.\n- 10. Explain why temperature remains low throughout the year in polar regions.\n- 11. Describe the vegetation of the savanna region.\n- 12. Describe the vegetation of the equatorial climate.\n- 13. Equatorial hot climate is experienced in which regions of the world.\n- 14. Describe the temperature of a typical hot desert during the day and at night.\n- 15. Equatorial hot climate supports plantation farming. Why?\n- 16. Why is wildlife conservation for tourism popular in Sudan climate?\n- 17. What does Campos mean?\n- 18. Differentiate between Mediterranean climate and China type.\n- 19. Describe the Greek system of classification in detail.\n- 20. Describe Koppen's system of classification.\n- 214 advantages of Koppen's classification over Greek's system.\n\n## Reference\n\n- Essential Geography for Senior Secondary Schools by O.A. Iwena, pages 268\text{–}283$.
Week 10: Environmental Resources
Meaning and Types of Environmental Resources
Meaning of Resources: Materials, substances, or components found naturally within the environment that are valuable and useful to humans for satisfying basic needs.
Categories of Resources:
Atmospheric Resources: Air, wind, solar radiation, ozone layer, water vapour, precipitation/rain.
Water Resources: All surface and subsurface water systems including aquatic organisms and dissolved minerals.
Forest Resources: Natural flora, timber, vegetation cover, and associated wild fauna.
Human Resources: Human labor force, intelligence, skill, and technology.
Mineral Resources: Non-renewable subsoil metallic, non-metallic, and fuel deposits.

Renewable and Non-Renewable Resources
Renewable Resources:
Definition: Natural resources that replenish or replace themselves naturally through natural cycles within a relatively short period.
Examples: Solar energy, wind energy, flowing water / tidal energy, soil, plants / forests, animals.
Characteristics:
Naturally restored after utilization
Highly sustainable if managed correctly
Inexhaustible under normal environmental cycles
Environmentally friendly
Dependent on continuous ecological systems
Advantages:
Do not get easily exhausted
Minimal carbon footprint / eco-friendly
Reduces global pollution
Ensures long-term sustainability
Cost-effective long-term operation
Disadvantages:
Intermittent supply dependent on short-term weather
High initial installation costs
Vulnerable to depletion if mismanaged (e.g., deforestation)
Non-Renewable Resources:
Definition: Natural resources that exist in fixed finite quantities and cannot be replaced once exhausted, or require millions of years to form.
Categories & Examples:
Fossil Fuels: Crude petroleum oil, coal, natural gas
Metallic Minerals: Iron ore, copper, aluminum, gold, tin, bauxite
Non-Metallic Minerals: Salt, phosphates
Nuclear Fuels: Uranium
Characteristics:
Finite and limited in total supply
Takes millions of geological years to form
Highly exhaustible
Irreplaceable once consumed
Causes environmental pollution during extraction and usage
Advantages:
Exceptionally high energy output
Reliable and continuous supply independent of weather
Established transport and storage infrastructure
Primary raw materials driving global heavy industry
Disadvantages:
Subject to total depletion
Causes atmospheric pollution and environmental degradation
Drives anthropogenic climate change
Price volatility and expensive long-term environmental costs
Mining damages ecosystems and causes land degradation
Resource Conservation Methods
Afforestation and reforestation (planting trees)
Recycling scrap metals, plastics, and glass
Waste minimization and industrial reduction
Transitioning to sustainable alternative energy sources (solar, wind, hydro)
Enforcing strict government environmental legislation and regulations
Review Questions
. Define resources.
. What are renewable resources?
. Give four examples of renewable resources.
. Explain two characteristics of renewable resources.
. State two advantages of renewable resources.
. Mention two disadvantages of renewable resources.
. Define non-renewable resources.
. Give four examples of non-renewable resources.
. Explain how fossil fuels are formed.
. State three characteristics of non-renewable resources.
. Mention three advantages of non-renewable resources.
. Outline three disadvantages of non-renewable resources.
. Differentiate between renewable and non-renewable resources.
. Explain the term conservation of resources.
. List four methods of conserving resources.
. Why are non-renewable resources considered exhaustible?
. Explain why solar energy is renewable.
. Describe two environmental effects of using fossil fuels.
. State two examples of mineral resources.
. Explain the importance of renewable resources to future generations.
Reference
Essential Geography for Senior Secondary Schools by O.A. Iwena, pages .