Grade 10 Lessons
Grade 10 Lessons
GRADE 10
GEOGRAPHY
CURRICULUM AND ASSESSMENT POLICY STATEMENT
LESSON PLAN
PREFACE
This support document serves to assist Geography teachers and learners on how to deal
with curriculum gaps and learning losses as a result of the impact of COVID – 19 in 2020. It
also captures the challenging topics in the Grade 10 work. The lesson plans should be used
in conjunction with the 2021 Recovery Teaching Plan. Activities should serve as a guide to
assess the topics dealt with in this document. It covers the following:
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LESSON PLAN
Atmosphere, Air, Atmospheric pressure ,Thermosphere ,Ozone, Ozone layer, Chlorofluorocarbons (CFCs),
RELATED CONCEPTS: Hydrofluorocarbons (HFCs)
Confusion in differentiating layers and zones of separation between layers of the atmosphere
(e.g. mesosphere and mesopause).
Confusion between the variable gases and permanent gases
ERRORS AND MISCONCEPTIONS:
Confusion on differentiating between weather and climate (e.g. daily observation of cloud
cover perceived as climate)
.
DATE STARTED: DATE COMPLETED:
Learners should be able to :
Define the atmosphere
LESSON Explain the importance of the atmosphere
OBJECTIVES Identify the layer in which weather conditions occurs
Identify the gases that make up the atmosphere
Explain the importance of the ozone layer
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LESSON PLAN
To explain what ozone is, the importance of ozone, factors that contribute to ozone depletion, effect of
ozone depletion
On human and environment.
Discuss the strategies to reduce ozone depletion.
Methodology:
Brainstorm around the composition and the structure of the atmosphere using the simple language
Definition of concepts related to the composition and the structure of the atmosphere
Importance of the atmosphere with learners explain and clarify the importance of the atmosphere in sustaining life on Earth
Learners annotate (label) a sketch representing the structure of the atmosphere on worksheet provided
Learners view satellite images of atmosphere and the ozone depletion using overhead projectors, data projectors and pictures
Using case studies to read and interpret the ozone depletion and its effecting selected areas of the Earth e.g. Antarctica
RESOURCES
TEACHER ACTIVITIES LEARNER ACTIVITIES
NEEDED
Define atmosphere Textbooks
Introduction Map of South
Baseline assessment: Description of the importance of
Africa
Introduce the topic (atmosphere, the composition, the structure and the atmosphere Working guide
the importance of the atmosphere) Past Exam
I Indication of the atmosphere on
question papers
Main Body (Lesson presentation) the globe (thin blue layer) Newspapers,
Defining what is atmosphere
Discussing the composition, structure of the atmosphere, the Provide visible characteristics of websites,
importance of the atmosphere and the different layers of the layers of the atmosphere through
atmosphere
diagrams/ chart/ graph
Discuss the importance of ozone, causes of ozone depletion and
strategies to reduce the impact of ozone depletion
Unpacking the different gases that make the highest and lowest
proportions in the atmosphere
Conclusion
chalkboard summary
Assessment taken from the guide provided
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LESSON PLAN
COMPOSITION AND STRUCTURE OF THE ATMOSPHERE
Atmosphere is composed mostly of gasses, but it also contains some liquids and particles.
Permanent gasses refers to the gasses that do not change in their proportion on the
atmosphere. Those gasses are Nitrogen (78%) Oxygen (21) and Argon (0, 9 %)
Variable gasses are those gasses that can chance their proportion from time to time and
from place to place. Common examples of variable gasses are carbon dioxide and water
vapour
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There are four layers that make atmosphere and those are:
Troposphere -The lower atmosphere with the densest layer of air. Temperature
decreases with altitude.
Stratosphere -The second layer of atmosphere above earth containing ozone.
Temperature increases with altitude.
Mesosphere – The third layer of atmosphere where meteors burn up. Temperature
decreases with altitude.
Thermosphere -The fourth and furthest layer of the atmosphere where
temperature increases with altitude
What is an inversion?
Inversion refers to an increase temperature with the increase in altitude
The two layers of the atmosphere where inversion occurs are
STRATOSPHERE AND THERMOSPHERE
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LESSON PLAN
GRADE 10
SUBJECT GEOGRAPHY WEEK 2-3 TOPIC HEATING OF THE ATMOSPHERE
Processes associated with heating of the atmosphere
Factors that affect the temperatures of different places around the world – latitude, altitude, ocean currents and
distance from oceans.
SUBTOPICS:
Heating of the atmosphere
Processes associated with the heating of the atmosphere: insolation, reflection, scattering, absorption, radiation,
conduction and convection
Insolation, absorption, reflection, scattering, convection, conduction terrestrial radiation, albedo ,solar
RELATED CONCEPTS: content , Altitude, temperature inversion, Global warming ,Aspect,
Terrestrial radiation, Conduction, Latent heat, Albedo, Greenhouse gases, Greenhouse effect
PRIOR/BACKGROUND KNOWLEDGE: Heat transfer (NS Grade 7)
Confusion in differentiating latitude and altitude
Confusion between temperature inversion and the relationship between temperature and
ERRORS AND MISCONCEPTIONS: latitude (e.g. the higher you go the colder it becomes)
Confusion on the differentiation of chlorofluorocarbons and hydrofluorocarbons
Difficulty in understanding greenhouse gases and greenhouse effect
DATE STARTED: DATE COMPLETED:
Learners should be able to:
Identify processes associated with the heating of the atmosphere when presented on the diagram
Explain how factors affecting temperature of different places around the world operate
differentiate between greenhouse gases and greenhouse effect
LESSON
The greenhouse gases and the main greenhouse gases
OBJECTIVES
What is global warming, causes of global warming and consequences of global warming
Strategies to reduce the impact of global warming and climate change
The factors affecting temperatures of different places around the world.
Methodology:
• Brainstorm around heating of the atmosphere using simple language and definition of concepts related to heating of the atmosphere.
• Processes associated with the heating of the atmosphere: - demonstrating insolation and scattering by using a globe and a torch
-demonstrating reflection using a torch and a mirror,demonstrating absorption using a torch, an A4 paper and a globe,demonstrating
conduction, convection and radiation using apparatus such as Bunsen burner and a pot
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• Factors that affect the temperature of different places around the world- using a torch and a globe to demonstrate variation of
insolation in different parts of the world (latitudes), Use of diagrams/ illustrations to show temperature differences in different
altitudes
• Demonstrating the different ocean currents using the world map (atlases)
• Learners view satellite images of the atmosphere and ozone depletion using overhead projectors, data projectors.
RESOURCES
TEACHER ACTIVITIES LEARNER ACTIVITIES
NEEDED
Introduction Definition of related concepts e.g.
Baseline assessment: latitude, altitude, ocean currents
Introducing processes associated with heating of the atmosphere Demonstrate using a torch and a
i.e. latitudes, altitudes, distance from the ocean, ocean currents, globe how temperature differ in Textbooks
aspect different places of the world Map of South
Explain the difference between the greenhouse gases and the Explanation through illustrations Africa
greenhouse effect how altitude and latitude influence Working guide
The teacher lists greenhouse gases and their importance on the temperature of ocean currents Past Exam
atmosphere Explanation and demonstration question papers
using a map/ globe how ocean Newspapers,
Main Body (Lesson presentation) currents influence temperature of websites,
Discussing with the learners how latitudes, altitudes, distance from different places, as well as
the ocean, ocean currents, aspect affect temperatures of the influence of the distance from the
different places around the world. ocean
Using local examples to discuss the factors affecting temperatures Description of the general
of the different places around the world causes of ozone depletion
Discuss with learners the factors that affect temperatures of different Identification of the effects of
places around the world i.e. latitudes, altitudes, ocean currents, ozone depletion from a case
distance from the ocean and aspect. study
Discuss the greenhouse gases, their importance and how they Description of the causes and
contribute to global warming effects of ozone depletion
Explain the impact of climate change on people and environment Discussion on the ways to reduce
Conclusion ozone depletion
chalkboard summary
Assessment taken guide provided
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LESSON PLAN
INSOLATION
Refers to the heat energy emitted direct from the sun, the concept insolation has been
derived from the Incoming Solar Radiation. Approximately 51% out of 100% of
insolation reach the Earth’s surface, and it is referred to Solar content.
Most of the insolation is lost before reaching the Earth’s surface due to the following
processes:
Absorption, Scattering, and reflection
Absorption- most of the Heat energy is absorbed by clouds and dust before it
reaches the atmosphere
Scattering refers to split up of insolation by small dust particles and gases
deflecting into different direction.
Reflection occurs when sunrays striking the earth are redirected back to the
space usually by clouds
Albedo refers to the percentage of light reflected back to a space. Clouds and
grass can reflect large percentage of sunray hence we say they have high
Albedo in contrast with concrete surfaces the reflect little heat and we say they
have low Albedo
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LESSON PLAN
LATITUDES
(Google images)
Places closer to the equator are warmer than places further away from the equator. The sun
heats the equator at a direct angle while Polar Regions receive indirect sunrays.
ALTITUDE
Normally the temperature decreases with an increase in high. Places in upper altitude are
colder than places in lower altitude. That is why some taller mountains are covered by ice
caps.
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Places inland have hotter summers and colder winters. This is caused by the fact that land
heats up quickly and cools up quickly as well.
Places closer to the ocean have cooler summers and warmer winters. This is caused by the
fact that ocean water heats up slowly and releases heat slowly as well
SLOPE ASPECT
Aspect refers to the angle in which the sun’s rays strike a slope.
Slopes facing the equator are warmer than slope facing poles. Slopes facing the equator
receive more sunrays than slopes facing poles
In the southern hemisphere the north facing slopes are warmer than south facing slopes.
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LESSON PLAN
OCEAN CURRENTS
Google image.
BENGUELA CURRENT transfers cold temperature from the south pole to the equator in the
west coast. AGULHAS CURRENT transfers heat from the equator to the South Pole.
GREENHOUSE EFFECT
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LESSON PLAN
Greenhouse effect is the ability of the atmosphere to trap the heat and remain warm
What are the greenhouse gasses?
Greenhouse gasses refer to the gasses that trap long wave radiation and increase the
temperature on the atmosphere.
Long wave radiation/ terrestrial radiation refer to the heat released from the earth usually
at night.
Examples of greenhouse gasses
MAIN GREENHOUSE GASES Carbon dioxide
Water vapour
OTHER GREENHOUSE GASES Methane
Carbon monoxide
Ozone
Sulphur dioxide and CFCs
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RESOURCES
TEACHER ACTIVITIES LEARNER ACTIVITIES
NEEDED
Introduction Discuss the processes of the water Textbooks
Baseline assessment:
cycle Map of South
Introduce the lesson by explaining how the water cycle occurs, with all the Africa
processes i.e evaporation, condensation and precipitation. Identify processes from the textbook Working guide
Write summary notes and class Past Exam
Main Body (Lesson presentation) question papers
Using the illustration of the diagram show and explain how activities Newspapers,
evaporation,condensation and precipitation occurs.
websites,
Conclusion
chalkboard summary
Assessment taken from the guide provided
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Types of precipitation
There three types of rainfall. Those are convectional rainfall, frontal rainfall, , and
orographic rainfall
CONVECTIONAL RAINFALL
• Occurs when there is intense heating of the Earth’s surface especially during summer. •
Evaporation takes place and moist air rises and cools. • Convectional rain occurs in areas with
high temperatures. • Common in summer rainfall areas in the South African interior.
OROGRAPHIC RAINFALL
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LESSON PLAN
FRONTAL RAINFALL
Frontal rain is formed when cold air masses converge with warm air masses. Cold air masses
do no mix with warm air masses hence they are separated by a boundary called front. Warm
air overrides the cold air is it has low density, warm air rises and condenses forming frontal
rain. Cold air masses with high density under rides the warm air.
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RESOURCES
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RELATED CONCEPTS: Humidity, Relative humidity, Saturated air, Dew point temperature, Frost
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LESSON PLAN
Discuss the mechanism behind the formation of convectional rain, Identification of the different types
frontal rain and orographic or relief rain. of clouds using pictures/chart
Use the map to identify the places that are frequented by each type Outdoor observation of the
of rainfall. distribution of clouds, identifying
Conclusion type, shape and possible weather
chalkboard summary notes Identification of the forms of
Assessment taken from the guide provided. precipitation using pictures
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Cirrus
Cirrostratus
Altocumulus
Stratus
Cumulus
Cumulonimbus
nimbostratus
• Precipitation – any form (could be liquid in the form of rain or solid in the form
of snow/ hail) of water coming from cloud
• Snow
• Rain
• Hail
• Frost
• Dew
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LESSON PLAN
Heat transfer (NS Grade 7) Composition of the atmosphere, Cloud names and associated weather
PRIOR/BACKGROUND KNOWLEDGE: conditions , Different forms of precipitation- hail, snow, rain, dew and frost.
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LESSON PLAN
Display of synoptic weather map and synoptic weather station information for the identification of all the features
on the map
Definition of related concepts e.g. GIS
Displaying pictures showing different components of GIS and ask them to identify each component.
Explanation of GIS and how an ordinary computer differs from a GIS computer
Outlining reasons for the development of GIS
METHODOLOGY Enumeration of Advantages and disadvantages of GIS over paper maps
Explanation of remote Sensing
Explanation on how remote sensing works
Distribution of pictures (satellite image and aerial view photograph)
Enumeration of the advantages and disadvantages of remote sensing
RESOURCES
TEACHER ACTIVITIES LEARNER ACTIVITIES
NEEDED
Displaying a synoptic weather Textbooks
map for the analysis and Map of South
Introduction
interpretation of weather Africa
Baseline assessment:
information Working guide
Definition of related concepts e.g. Past Exam
Brainstorm around different types of clouds
GIS question papers
Introduce different form of precipitation
A displayed computer to identify News papers,
Main Body (Lesson presentation) components (hardware) websites,
Name and dicuss different type of clouds such as cumulonimbus Explanation on how a GIS differs
and nimbostratus from it
Discuss hail, snow, dew, frost with learners Display of pictures showing
components of a GIS
Discuss the mechanism behind the formation of convectional rain,
frontal rain and orographic or relief rain. Discussion on the reasons for the
development of a GIS
Use the map to identify the places that are frequented by each type
of rainfall. Discussion on the concept of
Conclusion remote sensing and how remote
sensing works
chalkboard summary notes
Assessment taken from the guide provided. Discussion on the advantages
and disadvantages : GIS and
Remote sensing
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LESSON PLAN
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LESSON PLAN
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LESSON PLAN
It is a computer technology used to capture, store, analyse, manipulate and display geographic
data.
Remote sensing means the process of capturing data from distance. Data captured by
satellites orbiting the earth is then directed receiving station located on earth.
GIS is able to collect data even in spaces where humans cannot reach
It can identify changes that are taking place of time. Some those changes people cannot see
with their eyes. GIS is useful to all business such as farming.
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LESSON PLAN
Changes in the position of continents over time; plate tectonics-an explanation for the movement of continents
RELATED CONCEPTS: Geomorphology, Geological time , Crust, Mantle, Core ,Magma, Lava , Rock Volcanism , Igneous Rock, Sediments,
Fossils, Sedimentary Rocks, Strata, Bedding Plane, Metamorphic Rock, Continental drift, Fossils, Tectonic plate, Plate
Boundary, Convergent Plate Boundary, Divergent Plate Boundary, Transform Plate Boundary, Constructive Plate
Boundary, Destructive Plate Boundary
PRIOR/BACKGROUND KNOWLEDGE: Grade 7: the structure of the Earth
ERRORS AND MISCONCEPTIONS: Confusion between different type of plate tectonic concepts.
Methodology:
Brainstorm around the structure of the Earth using simple language.
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LESSON PLAN
Annotation (label) a sketch representing the structure of the Earth on worksheets provided.
Demonstration of the structure of the Earth using OVH /chart/satellite Classify the types of rocks Satellite images
photographs brought to class
Internet
Questioning learners to label the layers of the structure of the earth on a Attempt an activity given to them
given boiled egg Globe
Assign learners to classify the types of rocks brought in class Rock pieces (types of
rocks)
Write the learners responses on the board and discuss them.
Atlases/world map
Summarise the learners’ responses and write the correct answers to the
misconceptions Chalk board
Conclusion Charts
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LESSON PLAN
GRADE 10 SUMMARY NOTES [TERM 2] TOPIC: STRUCTURE OF THE EARTH /PLATE TECTONICS
RELATED CONCEPTS
• Geomorphology- The study of the earth’s physical features and processes that formed them.
• Geological time – Number of years in the past that rocks and landforms were formed.
• Crust – the outer layer of the Earth, formed of solid rock.
• Mantle – Layer of the earth found between the crust and the core composed of soft rocks.
• Core – The inner most layer of the Earth composed soft and solid rocks.
• Magma – Liquid rock inside the Earth.
• Lava – Magma that comes out onto the Earth’s surface.
• Rock – It is a mixture of minerals.
• Volcanism – Transfer of magma within or onto the surface.
• Igneous Rock – Forms when Magma cools and solidifies.
• Sediments – Pieces of rocks, clay and other substances from eroded rocks.
• Fossils – Remains of dead plants or animals preserved in rocks.
• Sedimentary Rocks – Rocks which from layers of compressed sediments.
• Strata – Layers of rocks
• Bedding Plane – Plane separating layers of rocks.
• Metamorphic Rock – Rocks that form when igneous or sedimentary rock change due to extreme heat and pressure.
● Continental drift – Is a theory that continents were once one landmass, but they have drifted apart overtime.
● Fossils – Remains of dead plants or animals preserved in rocks.
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● Tectonic plate – A section of the Earth’s crust which can move on the mantle.
● Plate Boundary – The edge of a tectonic plate.
● Convergent Plate Boundary – A plate boundary where plates are moving towards each other.
● Divergent Plate Boundary – A boundary where plates are moving apart from each other.
● Transform Plate Boundary – Where plates slide or grind past each other.
● Constructive Plate Boundary – A plate boundary where new land is forming.
● Destructive Plate Boundary – A plate boundary where is being destroyed.
EARTH’S STRUCTURE
All three forms of matter – solids, liquids and gases – make up the Earth.
The Earth is made up of four distinct layers, a solid outer crust, a solid mantle, a liquid
Continental crust
The crust is the outermost layer of solid rock, on which we live. It is thicker under the
The crust is broken into smaller segments, called plates, which float on the mantle.
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Mantle
The mantle is beneath the crust. TYPES OF ROCKS
It is 2 900 km thick, consisting of hot and plastic but solid rock. Temperatures may
reach 5 000°C.
The Moho discontinuity is the boundary between the crust and the mantle.
Outer core
The outer core layer is very dense but liquid due to extremely high temperatures.
It is 2 250 km thick.
Inner core
The inner core is extremely hot.
It is 1200 km thick.
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CHANGES IN THE POSITION OF CONTINENTS OVER TIME; PLATE TECTONICS-AN EXPLANATION FOR THE MOVEMENT OF CONTINENTS
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RELATED CONCEPTS: Faulting, Folding, Anticline, Overfold, Limb, Symmetrical fold, Asymmetrical fold, Overthrust fold, Fault line,
Normal fault, Reverse (thrust) fault, Transform / tear / strike-slip fault, Fault scarp
PRIOR/BACKGROUND KNOWLEDGE: Grade 7: Plate tectonics
ERRORS AND MISCONCEPTIONS: Confusion between folding and faulting.
Struggling to differentiate types of folds and faults.
DATE STARTED: DATE COMPLETED:
LESSON At the end of this lesson the learner must be able to:
OBJECTIVES Define related concepts
Understand the processes of folding and faulting as well as related landforms
Methodology:
Brainstorming around folding and faulting using simple language
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Different types of faults and their uses- make use of square boxes to illustrate different types of faults
Landforms associated with faulting, e.g. rift valleys and block mountains- Ask leaners to identify the different landforms (rift valley, block
mountain) making use of square boxes
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RELATED CONCEPTS
• Faulting: cracking of rock layers when they are pushed or pulled apart by disturbances in the earth’s crust.
• Folding: is the bending of rock layers when they are pushed together by disturbances in the earth’s crust.
• Syncline: downward bend of a folded rock
• Anticline: upward bend of folded rock
• Overfold: is a fold where one limb of fold is steeper than the other.
• Limb: the side of the fold
• Symmetrical fold: is the fold that have limps of equal angles
• Asymmetrical fold: is the fold that have limps of different angles.
• Overthrust fold: when one limb is pushed forward over the other limb
• Fault line: the line along the surface of Earth where fault occurs.
• Normal fault: a crack that forms when rock is under tension; on block of rock drops down.
• Reverse (thrust) fault: a crack that forms when rock is compressed, one block is pushed up.
• Transform / tear / strike-slip fault: a crack that forms when rock is sheared and one block slides sideways past the other.
• Fault scarp: a steep slope which forms along a fault line when rocks slide up or down
FOLDING
FORMATION OF FOLDS
Sediments laid down in horizontal layers form sedimentary rocks.
Folds form when tectonic plates push together, placing the rock layers under tremendous pressure.
The rock layers compress and form fold features. These range from simple folds to heavily compressed folds, which also feature fractured
rock.
Fold mountains are normally formed on the edges of colliding plates. For instance, the colliding Indian and Eurasian plates form the
Himalaya mountains
TYPES OF FOLDS
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Overthrust fold
Also called a Nappe.
Pressure is very great.
Fold breaks/fractures – faulting occurs.
One limb is pushed forward over the other limb.
Recumbent fold
Occurs under extreme pressure.
Result is the limbs become nearly horizontal.
Overfold
Similar to an anticline fold.
Except that the one limb is more steeply inclined than the other.
Monocline
Is the simplest fold.
Step-like fold in rock strata.
Consists of an area of steeply sloping rock strata in an area of otherwise gently sloping
rock strata.
Fold mountains
Alps, Rockies, Himalayas, Cape Fold Belt mountains in South Africa, Atlas in north Africa,
Mount Everest (8 850 m above sea level).
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Cape Fold Belt mountains – 23 ranges. Highest peak 2 325 m above sea level. Older than the
Alps and Himalayas.
FAULTING
CAUSE OF FAULTS
Under great pressure, rocks can crack or fracture.
One section of rock may then slide alongside or over another. The fracture is called a
fault.
Faulting can be caused by either lateral (sideways) or vertical (up and down) forces.
The forces may be caused by tension (rock layers being stretched or pulled apart) or
compression (the rocks being squeezed or pushed together).
A normal fault is caused by tension.
If one part of the crust is being compressed, then another part is under tension (being
stretched).
Rocks under tension usually fault.
Rocks under compression may fault or fold – softer rocks will fold, but harder rocks
that are brittle, will fault.
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VOLCANOES
Brainstorm around volcanoes using simple English language.
Definition of concepts related to volcanoes.
Types of volcanoes: - Explain and clarify the types of volcanoes i.e. extrusive, intrusive, active, dormant and extinct.
Structure of the volcanoes: Explain the structure of the volcano by means of the diagram and also using photos to explain volcanic landforms.
Impact of volcanoes on people and the environment (Positive and negative): Discuss with learners the impact of volcanoes on people and the
environment.
Case studies of different volcanic eruptions: Engaging learners in a discussion by means of reading the case study on volcanic eruption.
Conduct an experiment to illustrate volcanic eruption (enrichment).
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LESSON PLAN
VOLCANOES:
Define the concept of a volcano and volcanism.
List the different types of volcanoes (including intrusive and
extrusive).
Use illustrations(diagrams) to show different structures of
volcanoes.
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LESSON PLAN
Discuss with learners the impact (positive and negative) of Refer to the summary notes/ take
volcanoes on people and environment through case studies. down summary notes on the board.
Discussing strategies that can be adopted to reduce the View and interpret the illustrations
impact of volcanoes on people and environment. showing types of volcanoes.
Label the diagrams.
MAPWORK SKILLS INTERGRATION Read and analyse the impact of
Use atlas index to locate places where earthquakes, volcanoes from the given case
tsunamis and volcanoes occur. study.
Explain the importance of GIS in predicting, monitoring and Refer to the summary notes/ take
mitigating the occurrence/impact of earthquakes, tsunamis down summary notes on the board.
and volcanoes.
Conclusion
Recap of the entire lesson and emphasis on the most
important/key concepts.
Handing out of the assessment taken from the working guide Classwork/Homework
below.
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RELATED CONCEPTS: Lines of longitude, Lines of latitudes, Co-ordinates, Cardinal points, Grid Referencing
Map Scale
PRIOR/BACKGROUND KNOWLEDGE: Grade 8: SS-Maps and globes
Grade 9: Orthophoto maps
ERRORS AND MISCONCEPTIONS: Confusion in differentiating latitudes and longitudes
Struggling to locate exact position of features (determining seconds)
DATE STARTED: DATE COMPLETED:
LESSON At the end of this lesson the learner must be able to:
OBJECTIVES Define related concepts
Determine the exact location of a geographical feature on a map
Differentiate between types of scales
Methodology:
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Conclusion
Summarise the lesson and refer learners to an activity
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RELATED CONCEPTS
Lines of longitude – imaginary lines that run from north to south. Also called meridians.
Lines of latitudes – imaginary lines that run from east to west. Also called parallels.
Co-ordinates – exact position using the lines of latitude and longitudes.
Cardinal points – compass point that indicate direction
Grid Referencing - Refers to the location of places using degrees, minutes and seconds.
Map Scale -the relationship (or ratio) between distance on a map and the corresponding distance on the ground
LOCATING EXACT LOCATIONS
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50 ʹ ʹ
=25°13 ʹ 50 ʹ ʹ S
15 ʹ ʹ
30°1911511E
Co-ordinates: 25°13 ʹ 50 ʹ ʹ S, 30°19115 ʹ ʹ E
SCALE
Scale is the comparison between the distance on a map and the associated or corresponding distance on the earth’s surface.
Scale can be represented in three ways:
Ratio scale or Representative Fraction for example, 1 : 50 000 or 1/50 000
Word scale or Statement Scale, for example, one centimetre on the map represents fifty thousand centimetres in reality.
Linear scale or Line scale, for example, a line marked off in centimetre markings, showing what unit of measurement each centimetre
represents on the ground.
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METHODOLOGY:
Learners will be asked to define the term Population density and also to account for reason of people being
densely populated in certain part of the world (geographical area).
The teacher will give learners a diagram or an atlas of global population density
Learners will be required to brainstorm on factors that affect the distribution and density of the world’s population.
Educator will be expected to give a clear explanation how factors such as climate, Water, Soil, Relief etc.
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LESSON • Brain storming- unpacking a topic in simple language (factors influencing population indicators)
OBJECTIVES
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• Graphs – Showing the relationship between population indicators (e.g. deaths and births) as well as the
relationship between gender and age (population pyramid)
• Cartoons – reading, analysing and interpreting cartoons i.e. factors affecting fertility rate
METHODOLOGY:
Recap on population distribution and integrate introduction with previous knowledge from lower grades.
Population indicators:
demonstrating relationship between population indicators using line graphs and tables
Factors that affect birth rate and death rate – in LEDCs and MEDCs
Factors that affect fertility rate, life expectancy and natural increase
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Population pyramids
Demonstration through comparative population pyramids for developing and developed countries, the relationship
between age and gender
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ERRORS AND Confusion with the concept of diminishing population and exponential growth
MISCONCEPTIONS Difficulty in understanding the stages of the demographic transition model
: Applying geographical knowledge in the analysis of a cartoon
METHODOLOGY:
Recap on population structure and integrate previous knowledge from lower grades with introductory
LESSON
statement
OBJECTIVES
Refer to graph showing world population growth over time
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RESOURCES
TEACHER ACTIVITIES LEARNER ACTIVITIES
NEEDED
.
Charts/ diagrams
Interpretation of graphs
Cartoon images
(line graph- trend on
Google
Teacher will provide graphs reflecting/indicating world’s population/ world’s population/
demographic transition model) Textbooks
demographic transition
Case study-managing population growth Chalkboard
model)
Case study-managing
population growth
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METHODOLOGY:
• Recap on population growth and link previous content from lower grades with introductory statement
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SUB TOPICS Satellite images, Map skills, Map referencing, Conventional signs, True bearing, Magnetic bearing and Cross
section
• GIS – Is a system for capturing storing analysing and displaying Geographical data.
• Data – It is facts about reality that has been observed and measured.
• Information – It is data that is stringed together.
• Spatial data – It refers to the position of an object.
• Attribute data – It refers to the data that describes the characteristics of spatial data.
• Vector data – It refers to the representation of an area using points, lines and polygons.
• Raster data – It refers to the representation of an area using grid cells referred to as pixels.
• Resolution – It refers to the degree of clarity of an image.
RELATED CONCEPTS • Spatial resolution – It refers to the detail with which a map shows a location and shape of geographical
feature.
• Spectral resolution – It refers to the different kinds of information that can be collected.
• Remote sensing – It refers to the capturing of data on objects from a distance.
• Data integration – Combining of different types of data on a single map.
• Buffering – It refers to a line used to demarcate an area around a spatial feature.
• Map referencing – Identifying a point on the surface of the earth by relating it to information appearing on a
map.
• True bearing – It is an angle measured from the true north.
• Magnetic bearing – It is an angle measured from the magnetic north.
Population (Grade 6)
PRIOR/BACKGROUND
Population growth and change-focus SA and world (Grade 7)
KNOWLEDGE:
Recap from previous knowledge (grade 9)
ERRORS AND
True bearing – difficulty on the use of a protector
MISCONCEPTIONS:
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METHODOLOGY:
Learners will be asked to define Geographical Information System.
Learners will be asked to mention the components of GIS.
Learners will explain the importance of GIS.
Learners will give the differences between terms e.g.
Spatial and Attribute data, Vector and Raster data, Spatial and Spectral resolution
Learners will be asked to identify features on a map using the conventional sings.
Learners will give direction using the cardinal points.
Learners will calculate the magnetic bearing starting from finding True bearing and calculation of magnetic
declination.
• Lesson should be taught using simple English as a medium of instruction
LESSON OBJECTIVES
• Geographical terms should be defined using geographical terminology.
• The use of correct geographical term when explaining.
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ADDITIONAL NOTES
POPULATION GEOGRAPHY: Distribution and density, Structure, Growth &
Movements
• Population distribution describes how people are spread out on the Earth.
• Population density is the measurement of how many people there are in an area.
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• For most of human history the world’s population remained steady. It took until 1800 for it
to reach one billion. Today the world’s population is over six billion.
• This rapid growth in world population is called the population explosion and is the result of
reduced death rates due to improvements in medicine.
• Global population growth is now beginning to slow. It is predicted the population will
stabilise at 10, 4 billion in 2200.
• Population growth is not spread equally between countries – 95% of growth is in LEDCs.
• The following diagram represents the difference in growth rate between developed
(MEDCs) and developing (LEDCs) countries.
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• The demographic transition model shows how changes in birth rates and death rates affect
population growth in countries at different stages of development.
• The model may be used to explain population change in five stages (see diagram below).
• MEDCs (more economically developed countries) are entering a fifth stage where death
rates exceed birth rates and populations are falling.
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• Healthcare – reducing the infant mortality rate by providing primary health care facilities.
• Policies / Law – e.g. rules limiting the number of children (China: One child policy)
POPULATION MOVEMENTS
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• Social factors – the desire to live a better life, housing, environment, improved living
conditions, improved services, facilities, activities, relationships.
• Political factors – people move because they are unhappy with the political system, mainly
a push factor.
• Religious factors – people may move to avoid being persecuted because of their religion.
Move to where they can practise their religious beliefs.
• Physical factors – people may move to avoid physical dangers, a harsh climate or infertile
soil.
Seasonal movements
• Transhumance is the seasonal movement of people with their livestock over relatively short
distances, usually to higher pastures in summer and to lower valleys in winter.
• The traditional economy of the Basotho in Lesotho – seasonal migration between the
valleys and high plateaus of the Maluti mountains to increase the number of cattle.
Daily movements
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Temporary movements
• People stay in a place temporarily – for a short time only. Migrant labourers move to
another area temporarily to seek employment.
• Many migrant labourers are men who return home with their savings or later have their
family join them.
• Refugees who leave for political reasons may migrate temporarily to another area either
temporarily or permanently when lives are in danger. The Rwandan civil war in early 1990s
created more than 1,5 million refugees.
• Some people's beliefs (religion, political) may differ with the current status quo.
• Tourism, short contract work, business travel, conferences and conventions are also
examples of temporary movements.
• Refugees are people who have been forced to leave their home country because of war,
persecution or natural disaster. The United Nations estimates there are over 13 million
refugees spread throughout 140 countries.
• Perceptions people have of immigrants taking away jobs that only citizens are entitled to,
especially where jobs are in short supply.
• Foreign traditions and practices that are different from those of local people.
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RELATED Lake; Hydro-electricity; Water transfer scheme/ inter-basin transfer scheme; Free basic water, sustainability, alien
CONCEPTS vegetation, desalination
PRIOR/
Ways in which we use water?
BACKGROUND
KNOWLEDGE: What causes a place to have too much or too little water?
ERRORS AND
MISCONCEPTION Physical and human factors
S
LESSON Methodology:
OBJECTIVES
Explanation and supply of terminology list
Give an overview of topics and concepts to be covered using a mind map
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2. Physical factors
Rainfall
Alien vegetation
Climate change
Conclusion
Summary
Learners supplied with possible answers to the definitions or
terminology
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GRADE 10 SUBJECT Geography WEEK 36 TOPIC FLOODS
Floods – sudden overflow of water which covers land that is usually dry
Hydrograph – a graph showing a rivers discharge over time
Discharge’- amount of water across the width of a river flowing past a given point.
Drainage basin- total area drained by a river system.
Source- where a river begins
Tributary- a rivulet (small river) entering the main river
RELATED Watershed – high-lying area separating two drainage basins
CONCEPTS Mouth- where a river enters the sea/ocean
El Nino- a warm current which replaces the normal cold current on the west coast of South America every few years,
bringing drier conditions to South America and Africa
La Nina- a cold current which normally flows off the west coast of South America, bringing more rain to South America
and Africa
PRIOR/
Causes of floods
BACKGROUND
KNOWLEDGE: When do floods occur?
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Types of floods
Coastal floods/ river floods
Effects of river floods
Destroy crops
Drown people and livestock
Wash away top soil
Damage homes
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Charecteristics of floods
Using hydrographs to identify the characteristics of floods
River discharge rises soon after the rain storm put water
into the river drainage basin
The peak of the hydrograph shows the highest flow in cubic
meiters per second.
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