SlideShare a Scribd company logo
1 of 63
Mapwork
Otavi
Characteristic of a map
ā€¢ Scale
ā€¢ Title
ā€¢ Legend/ Key/ Reference
ā€¢ Direction
Types of Scale
Word Scale :
2 cm on the map represents 1 km on the ground or in
reality
Ratio Scale : 1: 50 000
Fraction scale:
1
50 0000
Linear Scale:
Determining size of the scale
ā€¢ When determining size of ratio scale, you look at
how big is the number after the colon (:). If the
number is bigger than its shows a small scale but
if the number is smaller then it indicates big
scale.
ā€¢ The number show how much detail and
information is indicated by the map. The bigger
the number the more information covered but
less detail, while smaller number means less
information but detailed
ā€¢ Example, 1 : 50 000 is a small scale while
1 : 25 000 is a large scale
Measuring and calculating
distance on the map
1. Measure distance on map in cm.
2. When measuring a curve line you use a strip of
paper and when measuring a straight line use a
ruler.
3. Apply formula
Distance on map
unit asked (m or km)
Ɨ Scale
4. Unit asked in m divide by 100 and in Km divide
by 100 0000
Example How to calculate distance
For instance, the distance measured on the map between
two points is 5cm and the map scale 1: 50 000
ā€¢ To kilometer (Km)
5cm
100 000 Ɨ 50 000 = 2.5 Km
1
2 x 5cm= 2.5 Km
ā€¢ To meter (m)
5cm
100 Ɨ 50 000 = 2500 m
Converting scales to Another
(a) Ratio to fraction (Ratio scale, 1 : 50 000)
Expressed as a Normal fractional scale.
1
50 000
Express scale as half a fractional scale.
1
50 000 š‘„
1
2 =
1
100 000
Express scale as a double fractional scale.
1
50 000 š‘„ 2 =
1
25 000
(b) Ratio to word scale (Ratio Scale,1:50 000)
1:50 000
1cm=50 000 cm
1cm=
50 000
100 000
1cm = 0.5km
1cm on the map represent 0.5km on the ground
or
1cm on the map represents 50 000 cm on the
ground.
2cm on the map represents 1km on the ground.
(c) From word scale to ratio scale.
word scale: 2cm on the map represent 1km on the ground
2cm=1km
2cm= 1km x 100 000
2cm=100 000cm
2š‘š‘š
2
=
100 000cm
2
1cm=50 000cm
1:50 000
(d) From linear to word scale to ratio scale
First measure the segment of the scale in cm, e.g.
you get 2cm.
To Word scale
2cm= 1000 m
2cm on the map represents 1000m on the ground
2cm
To Ratio scale
2cm= 1000 m
2cm= 1000 x 100
2cm/2=100 000/2
1cm=50 000 cm
1: 50 000
Determining Height
ā€¢ Height on the map is represented in metres (m)
Height on a topographic map is presented by:
ļƒ¼Spot Height e.g. 1170
ļƒ¼Trigonometrical Beacon e.g. 330
1274
ļƒ¼ Contour lines
Calculating gradient
ā€¢ Gradient refers to how steep is the slope
ā€¢ A gradient of 1: 5 is steeper than the gradient
of 1:50.
ā€¢ Reason: A gradient of 1:5 has to cover less
distance on the actual ground for 1 unit
increase in height While a gradient of 1:50 has
to cover more distance on the actual ground
for 1 unit increase in height.
How is gradient calculated
ā€¢ Gradient=
Vertical interval (VI)
Horizontal interval (HI)
ā€¢ VI= Highest height ā€“ Lowest Height
ā€¢ HI =
Distance on the map
100 x Scale of the map
Example
Calculate the gradient between spot height
1174 and spot height 1274, on a topographic
map if the distance between them is 4cm. The
map scale is 1: 50 000.
VI = highest ā€“ lowest
VI=1274m - 1174m
VI= 100m
ā€¢ HI=
Distance on the map
100 x Scale
ā€¢ HI=
4š‘š‘š
100 x 50 000
ā€¢ HI= 2000 m
ā€¢ Gradient=
Vertical interval (VI)
Horizontal interval (HI)
ā€¢ Gradient=
100 Ć·
2000 Ć·
100
100
ā€¢ Gradient =
1
20
ā€¢ Gradient= 1:20 (Change fractional scale into
ratio scale)
Direction
ā€¢ Make use of sixteen compass directions.
Direction Web Cross
How to get direction
ā€¢ Step 1: Connect the two features involved with
a light pencil
ā€¢ Step 2: Draw a true north line on the starting
feature
ā€¢ Step 3 : Draw a neat cross, on the starting point
ā€¢ Step 4 : find the direction using the neat cross
Example
Find the direction of B from A.
ā€¢ Mark the North line on
starting point at A
ā€¢ Draw a direction neat cross,
on the starting point (at A)
A
B
x
x
ā€¢ Draw the line connecting A
to B.
N
NE
E
SE
S
NW
SW
ā€¢Direction of B from A is
South East (SE)
Bearings
Rules:
ā€¢ Are always written in three figures (e.g.
040Ā° instead of 40Ā°)
ā€¢ Always measure the angle clockwise from
the True North
Matching compass pointsā€¦
360Ā°
000Ā°
023Ā°
045Ā°
068Ā°
090Ā°
113Ā°
225Ā°
158Ā°
180Ā°
338Ā°
315Ā°
293Ā°
270Ā°
248Ā°
135Ā°
203Ā°
Measuring bearingsā€¦
Find the bearing of B from A.
ā€¢ Mark the North line on at A
(if there isnā€™t a North line
draw one in)
ā€¢ Place your protractor over
the north line with 0Ā° at the
top (true north).
A
B
x
x
ā€¢ Draw the line connecting A
to B.
Measuring bearingsā€¦
Find the bearing of B from A.
ā€¢Measure the angle clockwise
from the North line to B
ā€¢ Give the answer as a three-
figure bearing
The bearing of B from A is 134Ā°.
A
B
Measuring bearingsā€¦
Find the bearing of A from B.
ā€¢ Mark the North line on at B
(if there isnā€™t a North line
draw one in)
ā€¢ Measure the angle
clockwise from the North line
to A
A
B
x
x
ā€¢ Draw the line connecting B
to A.
Measuring bearingsā€¦
Find the bearing of A from B.
ā€¢ Place your protractor over
the north line with 0Ā° at the
bottom.
ā€¢ The angle has gone past
180Ā° so you will need to add
your measurement to 180Ā°
A
B
x
x
ā€¢ Because you are measuring
clockwise you need to
measure the exterior angle.
Measuring bearingsā€¦
Find the bearing of A from B.
ā€¢ The measurement from the
bottom 0Ā° is 135Ā°.
The bearing of A from B is 313Ā°.
A
B
x
x
ā€¢ 133Ā° + 180Ā° = 313Ā°.
135 Ā°
Determining location
ā€¢ Involves using Latitude and longitude
ā€¢ Latitude are line that runs from the west to the east
while Longitude lines that runs from north to the
south
Symbols used
ā€¢ Degrees(Ā°), minutes (ā€˜) and seconds (ā€œ).
How to write Location( coordinates)
ā€¢ In Southern Hemisphere we first write the latitude
degree, minutes, seconds reading follow by south
direction.
ā€¢ Then followed by the longitude degree, minutes,
second reading followed by the east direction.
ā€¢ 24Ā°51ā€™45ā€™ā€™S29Ā°15ā€™30ā€™ā€™E
Examples how to determine location?
Find location of A (see next slide)
a) In Degree and Minutes
ā€¢ Latitude reading will be 17Ėš23 Ģ’S
ā€¢ Longitude reading will be 19Ėš38 Ģ’E
ā€¢ Therefore the Location will be
17Ėš23 Ģ’S 19Ėš38 Ģ’E
b) Degrees, Minutes and Second
For you to do this you need a ruler and
calculator.
See examples below
A
ā€¢ Firstly connect latitudes
and longitudes lines to
make a grid
ā€¢ For latitude seconds
measure from first
latitude to the second
latitude line in mm (b).
ā€¢ Measure from first
latitude to the point in
mm (a).
ā€¢ Use formalar
š‘Ž
š‘
x 60ā€
ā€¢ The final answer you
add it to degrees and
minutes of latitude
A
ā€¢ Firstly connect latitudes
and longitudes lines to
make a grid
ā€¢ For longitude seconds
measure from first
longitude to the second
longitude line in mm (b).
ā€¢ Measure from first
longitude to the point in
mm (a).
ā€¢ Use formalar
š‘Ž
š‘
x 60ā€
ā€¢ The final answer you
get add it to degrees
and minutes of
longitude
How to read other features on the map
Relief
ā€¢ Look for region uplands and lowlands
ā€¢ State the highest point and the lowest point,
ā€¢ Recognize landform features such as Plateau,
Valley.
ā€¢ Look for identifiable slopes ā€“ convex, concave,
steeper or Gentle.
Type of slopes on the map
Gentle : Steep
Terraced : Vertical
Convex : Concave
Terraced Slope
Flat Topped hill
Conical hill/Pointed butte
Spur
Valley
Saddle
Drainage
ā€¢ Describe drainage density of river (High, Low or
Medium) depending on number of streams
forming a drainage
ā€¢ Identify the drainage patterns (trellis, dendritic,
radial, etc.)
ā€¢ Recognize if the rivers are perennial or not
ā€¢ Recognizable features of the river (waterfalls,
rapids, braiding, meander, islands, ox bow lakes,
etc)
ā€¢ Identify stage of river courses (upper, middle or
lower)
Drainage Patterns
Dendritric Pattern
Deranged Pattern
Parallel Pattern
Rectangular Pattern
Trellis Pattern
Radial Pattern
Drainage Density
Land use
A useful method is to consider economic activities:
Primary economic activities
a) Farming
ā€¢ Type of farming: Arable Farming (Crop Farming)
or Pastoral Farming (livestock Farming)
ā€¢ For Arable farming look out for cultivation,
irrigation furrows, canals and pipelines, farm
dams and Silos.
ā€¢ For Livestock look out for kraals, windmills and
dipping tanks
b) Mining
ā€¢ Open cast mining
ā€¢ Look for name of the mine, Opencast mine, service
railways, mine dump, excavations and diggings.
c) Forestry
ā€¢ Look out for plantations and forests names
d) Fishing
ā€¢ Look out for coastal quays and harbours
Secondary economic activity
industry (look for industrial location factors,
market, raw material, power and water, labour, flat
land and transport).
Tertiary economic activity
Look for services facilities indicated next to each
service
ā€¢ Education (School, University and Colleges)
ā€¢ Recreation ( Caravan Park, Rec, Golf Course)
ā€¢ Health /Medical service (Clinic and Hospitals)
ā€¢ Shopping( Shops, Supermarkets and Store)
Transport and communication
ā€¢ Railways
ā€¢ Main Roads
ā€¢ Secondary roads
ā€¢ Landing Strips/ Airports
ā€¢ Hiking and Trail
Road Patterns/Street Patterns
Photographs
ā€¢ Horizontal photographs
ā€¢ High oblique
ā€¢ Low oblique
ā€¢ Vertical /aerial photographs
Horizontal photographs
ā€¢ Advantages
ā€¢ The photograph shows a lot of detail
ā€¢ Disadvantages
ā€¢ Shows a small area
ā€¢ Objects in the foreground block out objects in
the background
ā€¢ Objects in the foreground appear larger than
objects in the background
ā€¢ Cannot use them for map drawing
GROUND-LEVEL PHOTOGRAPH
ļƒ˜Taken at ground-level, as you would normally
see things.
High oblique photographs
ā€¢ Taken from a high vantage point such as top of a
building.
ā€¢ The horizon is visible
Advantages
ā€¢ Covers a larger area
ā€¢ Shows a lot of information
Disadvantages
ā€¢ Less detail in the foreground
ā€¢ Objects in the foreground block out objects in the
background
HIGH OBLIQUE PHOTOGRAPH
ļƒ˜Taken from a high point (building), horizon is
visible.
Low oblique photographs
ā€¢ These photographs are taken from a airplane at a
angle.
ā€¢ Horizon is not visible
ā€¢ Advantages
ā€¢ They show a larger area
ā€¢ Shows much more information
ā€¢ Disadvantages
ā€¢ Objects in the foreground block out objects in the
background
ā€¢ Objects in the foreground appear larger than
objects in the background
LOW OBLIQUE PHOTOGRAPH
ļƒ˜Taken from an aero plane, horizon not visible.
Vertical photographs
ā€¢ Taken from a airplane but the camera is tilted
vertically down.
ā€¢ Advantage
ā€¢ No hidden areas
ā€¢ Shows a lot of information
ā€¢ Used to draw maps
ā€¢ Disadvantages
ā€¢ Height and surface slopes are not easy to identify
ā€¢ A lot of experience is needed to obtain
information from these photographs
Other Graphical analysis
Know how to read and complete the graphs below
ā€¢ Bar graphs
ā€¢ Line graphs
ā€¢ Pie Chart
ā€¢ Divided Bar graph
ā€¢ Triangular graph
ā€¢ Wind rose

More Related Content

What's hot

Scale and distance
Scale and distanceScale and distance
Scale and distanceSteven Heath
Ā 
Topographic maps presentation_mine
Topographic maps presentation_mineTopographic maps presentation_mine
Topographic maps presentation_minemisterbatroms
Ā 
Map Projections
Map ProjectionsMap Projections
Map ProjectionsJohn Reiser
Ā 
Map Reading and Interpretation
Map Reading and InterpretationMap Reading and Interpretation
Map Reading and InterpretationYonas Gemeda
Ā 
Methods of representing physiographic features
Methods of representing physiographic featuresMethods of representing physiographic features
Methods of representing physiographic featuresvenkatesh sambandan
Ā 
shape of earth
shape of earthshape of earth
shape of earthHafsa Naeem
Ā 
Types Drainage pattern presentation
Types Drainage pattern presentationTypes Drainage pattern presentation
Types Drainage pattern presentationKamrul Islam Karim
Ā 
Morphology of ocean floor
Morphology of ocean floorMorphology of ocean floor
Morphology of ocean floorPramoda Raj
Ā 
Numbering system of topographical map
Numbering system of topographical mapNumbering system of topographical map
Numbering system of topographical mapMithun Ray
Ā 
Gradient CSEC Geography
Gradient  CSEC GeographyGradient  CSEC Geography
Gradient CSEC Geographyry_moore
Ā 
Toposheet interpretation
Toposheet interpretationToposheet interpretation
Toposheet interpretationPramod Hanamgond
Ā 
Basic topographic mapping
Basic topographic mappingBasic topographic mapping
Basic topographic mappingBhok Millare
Ā 
Map projection
Map projectionMap projection
Map projectionkaslinsas
Ā 
Introduction to spatial interaction modelling
Introduction to spatial interaction modellingIntroduction to spatial interaction modelling
Introduction to spatial interaction modellingUniversity of Southampton
Ā 
Evolution of Geographical Thought
Evolution of Geographical Thought Evolution of Geographical Thought
Evolution of Geographical Thought Namdev Telore
Ā 
Family of cylindrical map projection
Family of cylindrical map projectionFamily of cylindrical map projection
Family of cylindrical map projectionNasir Mughal
Ā 
Coordinate systems
Coordinate systemsCoordinate systems
Coordinate systemsSaad Raja
Ā 

What's hot (20)

Scale and distance
Scale and distanceScale and distance
Scale and distance
Ā 
Topographic maps presentation_mine
Topographic maps presentation_mineTopographic maps presentation_mine
Topographic maps presentation_mine
Ā 
Map Projections
Map ProjectionsMap Projections
Map Projections
Ā 
Map Reading and Interpretation
Map Reading and InterpretationMap Reading and Interpretation
Map Reading and Interpretation
Ā 
Methods of representing physiographic features
Methods of representing physiographic featuresMethods of representing physiographic features
Methods of representing physiographic features
Ā 
shape of earth
shape of earthshape of earth
shape of earth
Ā 
Types Drainage pattern presentation
Types Drainage pattern presentationTypes Drainage pattern presentation
Types Drainage pattern presentation
Ā 
Morphology of ocean floor
Morphology of ocean floorMorphology of ocean floor
Morphology of ocean floor
Ā 
Numbering system of topographical map
Numbering system of topographical mapNumbering system of topographical map
Numbering system of topographical map
Ā 
Gradient CSEC Geography
Gradient  CSEC GeographyGradient  CSEC Geography
Gradient CSEC Geography
Ā 
Coordinate systems
Coordinate systemsCoordinate systems
Coordinate systems
Ā 
Toposheet interpretation
Toposheet interpretationToposheet interpretation
Toposheet interpretation
Ā 
Topography powerpoint
Topography powerpointTopography powerpoint
Topography powerpoint
Ā 
Basic topographic mapping
Basic topographic mappingBasic topographic mapping
Basic topographic mapping
Ā 
Geological Map.ppt
Geological Map.pptGeological Map.ppt
Geological Map.ppt
Ā 
Map projection
Map projectionMap projection
Map projection
Ā 
Introduction to spatial interaction modelling
Introduction to spatial interaction modellingIntroduction to spatial interaction modelling
Introduction to spatial interaction modelling
Ā 
Evolution of Geographical Thought
Evolution of Geographical Thought Evolution of Geographical Thought
Evolution of Geographical Thought
Ā 
Family of cylindrical map projection
Family of cylindrical map projectionFamily of cylindrical map projection
Family of cylindrical map projection
Ā 
Coordinate systems
Coordinate systemsCoordinate systems
Coordinate systems
Ā 

Similar to Mapwork skills.pptx

geographic techniques.ppt
geographic techniques.pptgeographic techniques.ppt
geographic techniques.pptssuser2350ae
Ā 
Social Science Grade 8 Maps and Globes.pptx
Social Science Grade 8 Maps and Globes.pptxSocial Science Grade 8 Maps and Globes.pptx
Social Science Grade 8 Maps and Globes.pptxAntonHartman
Ā 
Determination of strike and dip and geological cross section
Determination of strike and dip and geological cross section Determination of strike and dip and geological cross section
Determination of strike and dip and geological cross section Aditya Mistry
Ā 
Maps-and-map-interpretation.pdf
Maps-and-map-interpretation.pdfMaps-and-map-interpretation.pdf
Maps-and-map-interpretation.pdfshucaybcabdi
Ā 
Chapter 3 gateway 123 combined
Chapter 3 gateway 123 combinedChapter 3 gateway 123 combined
Chapter 3 gateway 123 combinedMissST
Ā 
Chapter 3 gateway 123
Chapter 3 gateway 123Chapter 3 gateway 123
Chapter 3 gateway 123MissST
Ā 
Chapter 2 - Topo Map Reading
Chapter 2 - Topo Map ReadingChapter 2 - Topo Map Reading
Chapter 2 - Topo Map ReadingGeographyByTian
Ā 
LS GE Slides - Map Reading
LS GE Slides - Map ReadingLS GE Slides - Map Reading
LS GE Slides - Map ReadingLEEENNA
Ā 
Contour lines by sk
Contour lines by skContour lines by sk
Contour lines by skSalman Khan
Ā 
contourlines-161212065738.pdf
contourlines-161212065738.pdfcontourlines-161212065738.pdf
contourlines-161212065738.pdfshucaybcabdi
Ā 
ContourLines (4).ppt
ContourLines (4).pptContourLines (4).ppt
ContourLines (4).pptnokwandaNyandeni
Ā 
Brief ContourLines power point for surveying engineering
Brief ContourLines power point for surveying engineeringBrief ContourLines power point for surveying engineering
Brief ContourLines power point for surveying engineeringdejenemulu
Ā 
ContourLines.ppt
ContourLines.pptContourLines.ppt
ContourLines.pptFahadZareef1
Ā 
topographicmapsnotes-130930200052-phpapp01.pdf
topographicmapsnotes-130930200052-phpapp01.pdftopographicmapsnotes-130930200052-phpapp01.pdf
topographicmapsnotes-130930200052-phpapp01.pdfshucaybcabdi
Ā 
Drawing tools unit 1
Drawing tools unit 1Drawing tools unit 1
Drawing tools unit 1Rai University
Ā 
GI - Map skills and hypothesis
GI - Map skills and hypothesisGI - Map skills and hypothesis
GI - Map skills and hypothesisMissST
Ā 
7_UELSurveyingMeasurement.pdf
7_UELSurveyingMeasurement.pdf7_UELSurveyingMeasurement.pdf
7_UELSurveyingMeasurement.pdfYusufAhmed331510
Ā 
Secondary 1 Geography-Topographic Map
Secondary 1 Geography-Topographic MapSecondary 1 Geography-Topographic Map
Secondary 1 Geography-Topographic MapMarioSonic54
Ā 

Similar to Mapwork skills.pptx (20)

geographic techniques.ppt
geographic techniques.pptgeographic techniques.ppt
geographic techniques.ppt
Ā 
Social Science Grade 8 Maps and Globes.pptx
Social Science Grade 8 Maps and Globes.pptxSocial Science Grade 8 Maps and Globes.pptx
Social Science Grade 8 Maps and Globes.pptx
Ā 
Determination of strike and dip and geological cross section
Determination of strike and dip and geological cross section Determination of strike and dip and geological cross section
Determination of strike and dip and geological cross section
Ā 
Maps-and-map-interpretation.pdf
Maps-and-map-interpretation.pdfMaps-and-map-interpretation.pdf
Maps-and-map-interpretation.pdf
Ā 
Mapping .pptx
Mapping .pptxMapping .pptx
Mapping .pptx
Ā 
Chapter 3 gateway 123 combined
Chapter 3 gateway 123 combinedChapter 3 gateway 123 combined
Chapter 3 gateway 123 combined
Ā 
Chapter 3 gateway 123
Chapter 3 gateway 123Chapter 3 gateway 123
Chapter 3 gateway 123
Ā 
Chapter 2 - Topo Map Reading
Chapter 2 - Topo Map ReadingChapter 2 - Topo Map Reading
Chapter 2 - Topo Map Reading
Ā 
LS GE Slides - Map Reading
LS GE Slides - Map ReadingLS GE Slides - Map Reading
LS GE Slides - Map Reading
Ā 
Contour lines by sk
Contour lines by skContour lines by sk
Contour lines by sk
Ā 
contourlines-161212065738.pdf
contourlines-161212065738.pdfcontourlines-161212065738.pdf
contourlines-161212065738.pdf
Ā 
Area_Contour.ppt
Area_Contour.pptArea_Contour.ppt
Area_Contour.ppt
Ā 
ContourLines (4).ppt
ContourLines (4).pptContourLines (4).ppt
ContourLines (4).ppt
Ā 
Brief ContourLines power point for surveying engineering
Brief ContourLines power point for surveying engineeringBrief ContourLines power point for surveying engineering
Brief ContourLines power point for surveying engineering
Ā 
ContourLines.ppt
ContourLines.pptContourLines.ppt
ContourLines.ppt
Ā 
topographicmapsnotes-130930200052-phpapp01.pdf
topographicmapsnotes-130930200052-phpapp01.pdftopographicmapsnotes-130930200052-phpapp01.pdf
topographicmapsnotes-130930200052-phpapp01.pdf
Ā 
Drawing tools unit 1
Drawing tools unit 1Drawing tools unit 1
Drawing tools unit 1
Ā 
GI - Map skills and hypothesis
GI - Map skills and hypothesisGI - Map skills and hypothesis
GI - Map skills and hypothesis
Ā 
7_UELSurveyingMeasurement.pdf
7_UELSurveyingMeasurement.pdf7_UELSurveyingMeasurement.pdf
7_UELSurveyingMeasurement.pdf
Ā 
Secondary 1 Geography-Topographic Map
Secondary 1 Geography-Topographic MapSecondary 1 Geography-Topographic Map
Secondary 1 Geography-Topographic Map
Ā 

Recently uploaded

Separation of Lanthanides/ Lanthanides and Actinides
Separation of Lanthanides/ Lanthanides and ActinidesSeparation of Lanthanides/ Lanthanides and Actinides
Separation of Lanthanides/ Lanthanides and ActinidesFatimaKhan178732
Ā 
Hybridoma Technology ( Production , Purification , and Application )
Hybridoma Technology  ( Production , Purification , and Application  ) Hybridoma Technology  ( Production , Purification , and Application  )
Hybridoma Technology ( Production , Purification , and Application ) Sakshi Ghasle
Ā 
Incoming and Outgoing Shipments in 1 STEP Using Odoo 17
Incoming and Outgoing Shipments in 1 STEP Using Odoo 17Incoming and Outgoing Shipments in 1 STEP Using Odoo 17
Incoming and Outgoing Shipments in 1 STEP Using Odoo 17Celine George
Ā 
Industrial Policy - 1948, 1956, 1973, 1977, 1980, 1991
Industrial Policy - 1948, 1956, 1973, 1977, 1980, 1991Industrial Policy - 1948, 1956, 1973, 1977, 1980, 1991
Industrial Policy - 1948, 1956, 1973, 1977, 1980, 1991RKavithamani
Ā 
Alper Gobel In Media Res Media Component
Alper Gobel In Media Res Media ComponentAlper Gobel In Media Res Media Component
Alper Gobel In Media Res Media ComponentInMediaRes1
Ā 
How to Make a Pirate ship Primary Education.pptx
How to Make a Pirate ship Primary Education.pptxHow to Make a Pirate ship Primary Education.pptx
How to Make a Pirate ship Primary Education.pptxmanuelaromero2013
Ā 
Micromeritics - Fundamental and Derived Properties of Powders
Micromeritics - Fundamental and Derived Properties of PowdersMicromeritics - Fundamental and Derived Properties of Powders
Micromeritics - Fundamental and Derived Properties of PowdersChitralekhaTherkar
Ā 
Presiding Officer Training module 2024 lok sabha elections
Presiding Officer Training module 2024 lok sabha electionsPresiding Officer Training module 2024 lok sabha elections
Presiding Officer Training module 2024 lok sabha electionsanshu789521
Ā 
Science 7 - LAND and SEA BREEZE and its Characteristics
Science 7 - LAND and SEA BREEZE and its CharacteristicsScience 7 - LAND and SEA BREEZE and its Characteristics
Science 7 - LAND and SEA BREEZE and its CharacteristicsKarinaGenton
Ā 
Concept of Vouching. B.Com(Hons) /B.Compdf
Concept of Vouching. B.Com(Hons) /B.CompdfConcept of Vouching. B.Com(Hons) /B.Compdf
Concept of Vouching. B.Com(Hons) /B.CompdfUmakantAnnand
Ā 
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Sapana Sha
Ā 
Grant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingGrant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingTechSoup
Ā 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactdawncurless
Ā 
Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)eniolaolutunde
Ā 
Arihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdfArihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdfchloefrazer622
Ā 
The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13Steve Thomason
Ā 
BASLIQ CURRENT LOOKBOOK LOOKBOOK(1) (1).pdf
BASLIQ CURRENT LOOKBOOK  LOOKBOOK(1) (1).pdfBASLIQ CURRENT LOOKBOOK  LOOKBOOK(1) (1).pdf
BASLIQ CURRENT LOOKBOOK LOOKBOOK(1) (1).pdfSoniaTolstoy
Ā 
_Math 4-Q4 Week 5.pptx Steps in Collecting Data
_Math 4-Q4 Week 5.pptx Steps in Collecting Data_Math 4-Q4 Week 5.pptx Steps in Collecting Data
_Math 4-Q4 Week 5.pptx Steps in Collecting DataJhengPantaleon
Ā 

Recently uploaded (20)

Separation of Lanthanides/ Lanthanides and Actinides
Separation of Lanthanides/ Lanthanides and ActinidesSeparation of Lanthanides/ Lanthanides and Actinides
Separation of Lanthanides/ Lanthanides and Actinides
Ā 
Hybridoma Technology ( Production , Purification , and Application )
Hybridoma Technology  ( Production , Purification , and Application  ) Hybridoma Technology  ( Production , Purification , and Application  )
Hybridoma Technology ( Production , Purification , and Application )
Ā 
Staff of Color (SOC) Retention Efforts DDSD
Staff of Color (SOC) Retention Efforts DDSDStaff of Color (SOC) Retention Efforts DDSD
Staff of Color (SOC) Retention Efforts DDSD
Ā 
Incoming and Outgoing Shipments in 1 STEP Using Odoo 17
Incoming and Outgoing Shipments in 1 STEP Using Odoo 17Incoming and Outgoing Shipments in 1 STEP Using Odoo 17
Incoming and Outgoing Shipments in 1 STEP Using Odoo 17
Ā 
Industrial Policy - 1948, 1956, 1973, 1977, 1980, 1991
Industrial Policy - 1948, 1956, 1973, 1977, 1980, 1991Industrial Policy - 1948, 1956, 1973, 1977, 1980, 1991
Industrial Policy - 1948, 1956, 1973, 1977, 1980, 1991
Ā 
Alper Gobel In Media Res Media Component
Alper Gobel In Media Res Media ComponentAlper Gobel In Media Res Media Component
Alper Gobel In Media Res Media Component
Ā 
How to Make a Pirate ship Primary Education.pptx
How to Make a Pirate ship Primary Education.pptxHow to Make a Pirate ship Primary Education.pptx
How to Make a Pirate ship Primary Education.pptx
Ā 
Micromeritics - Fundamental and Derived Properties of Powders
Micromeritics - Fundamental and Derived Properties of PowdersMicromeritics - Fundamental and Derived Properties of Powders
Micromeritics - Fundamental and Derived Properties of Powders
Ā 
Presiding Officer Training module 2024 lok sabha elections
Presiding Officer Training module 2024 lok sabha electionsPresiding Officer Training module 2024 lok sabha elections
Presiding Officer Training module 2024 lok sabha elections
Ā 
Science 7 - LAND and SEA BREEZE and its Characteristics
Science 7 - LAND and SEA BREEZE and its CharacteristicsScience 7 - LAND and SEA BREEZE and its Characteristics
Science 7 - LAND and SEA BREEZE and its Characteristics
Ā 
Concept of Vouching. B.Com(Hons) /B.Compdf
Concept of Vouching. B.Com(Hons) /B.CompdfConcept of Vouching. B.Com(Hons) /B.Compdf
Concept of Vouching. B.Com(Hons) /B.Compdf
Ā 
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Ā 
Grant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingGrant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy Consulting
Ā 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impact
Ā 
Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)
Ā 
Arihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdfArihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdf
Ā 
Model Call Girl in Tilak Nagar Delhi reach out to us at šŸ”9953056974šŸ”
Model Call Girl in Tilak Nagar Delhi reach out to us at šŸ”9953056974šŸ”Model Call Girl in Tilak Nagar Delhi reach out to us at šŸ”9953056974šŸ”
Model Call Girl in Tilak Nagar Delhi reach out to us at šŸ”9953056974šŸ”
Ā 
The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13
Ā 
BASLIQ CURRENT LOOKBOOK LOOKBOOK(1) (1).pdf
BASLIQ CURRENT LOOKBOOK  LOOKBOOK(1) (1).pdfBASLIQ CURRENT LOOKBOOK  LOOKBOOK(1) (1).pdf
BASLIQ CURRENT LOOKBOOK LOOKBOOK(1) (1).pdf
Ā 
_Math 4-Q4 Week 5.pptx Steps in Collecting Data
_Math 4-Q4 Week 5.pptx Steps in Collecting Data_Math 4-Q4 Week 5.pptx Steps in Collecting Data
_Math 4-Q4 Week 5.pptx Steps in Collecting Data
Ā 

Mapwork skills.pptx

  • 3. Characteristic of a map ā€¢ Scale ā€¢ Title ā€¢ Legend/ Key/ Reference ā€¢ Direction
  • 4. Types of Scale Word Scale : 2 cm on the map represents 1 km on the ground or in reality Ratio Scale : 1: 50 000 Fraction scale: 1 50 0000 Linear Scale:
  • 5. Determining size of the scale ā€¢ When determining size of ratio scale, you look at how big is the number after the colon (:). If the number is bigger than its shows a small scale but if the number is smaller then it indicates big scale. ā€¢ The number show how much detail and information is indicated by the map. The bigger the number the more information covered but less detail, while smaller number means less information but detailed ā€¢ Example, 1 : 50 000 is a small scale while 1 : 25 000 is a large scale
  • 6. Measuring and calculating distance on the map 1. Measure distance on map in cm. 2. When measuring a curve line you use a strip of paper and when measuring a straight line use a ruler. 3. Apply formula Distance on map unit asked (m or km) Ɨ Scale 4. Unit asked in m divide by 100 and in Km divide by 100 0000
  • 7. Example How to calculate distance For instance, the distance measured on the map between two points is 5cm and the map scale 1: 50 000 ā€¢ To kilometer (Km) 5cm 100 000 Ɨ 50 000 = 2.5 Km 1 2 x 5cm= 2.5 Km ā€¢ To meter (m) 5cm 100 Ɨ 50 000 = 2500 m
  • 8. Converting scales to Another (a) Ratio to fraction (Ratio scale, 1 : 50 000) Expressed as a Normal fractional scale. 1 50 000 Express scale as half a fractional scale. 1 50 000 š‘„ 1 2 = 1 100 000 Express scale as a double fractional scale. 1 50 000 š‘„ 2 = 1 25 000
  • 9. (b) Ratio to word scale (Ratio Scale,1:50 000) 1:50 000 1cm=50 000 cm 1cm= 50 000 100 000 1cm = 0.5km 1cm on the map represent 0.5km on the ground or 1cm on the map represents 50 000 cm on the ground. 2cm on the map represents 1km on the ground.
  • 10. (c) From word scale to ratio scale. word scale: 2cm on the map represent 1km on the ground 2cm=1km 2cm= 1km x 100 000 2cm=100 000cm 2š‘š‘š 2 = 100 000cm 2 1cm=50 000cm 1:50 000
  • 11. (d) From linear to word scale to ratio scale First measure the segment of the scale in cm, e.g. you get 2cm. To Word scale 2cm= 1000 m 2cm on the map represents 1000m on the ground 2cm
  • 12. To Ratio scale 2cm= 1000 m 2cm= 1000 x 100 2cm/2=100 000/2 1cm=50 000 cm 1: 50 000
  • 13. Determining Height ā€¢ Height on the map is represented in metres (m) Height on a topographic map is presented by: ļƒ¼Spot Height e.g. 1170 ļƒ¼Trigonometrical Beacon e.g. 330 1274 ļƒ¼ Contour lines
  • 14. Calculating gradient ā€¢ Gradient refers to how steep is the slope ā€¢ A gradient of 1: 5 is steeper than the gradient of 1:50. ā€¢ Reason: A gradient of 1:5 has to cover less distance on the actual ground for 1 unit increase in height While a gradient of 1:50 has to cover more distance on the actual ground for 1 unit increase in height.
  • 15. How is gradient calculated ā€¢ Gradient= Vertical interval (VI) Horizontal interval (HI) ā€¢ VI= Highest height ā€“ Lowest Height ā€¢ HI = Distance on the map 100 x Scale of the map
  • 16. Example Calculate the gradient between spot height 1174 and spot height 1274, on a topographic map if the distance between them is 4cm. The map scale is 1: 50 000. VI = highest ā€“ lowest VI=1274m - 1174m VI= 100m
  • 17. ā€¢ HI= Distance on the map 100 x Scale ā€¢ HI= 4š‘š‘š 100 x 50 000 ā€¢ HI= 2000 m
  • 18. ā€¢ Gradient= Vertical interval (VI) Horizontal interval (HI) ā€¢ Gradient= 100 Ć· 2000 Ć· 100 100 ā€¢ Gradient = 1 20 ā€¢ Gradient= 1:20 (Change fractional scale into ratio scale)
  • 19. Direction ā€¢ Make use of sixteen compass directions. Direction Web Cross
  • 20. How to get direction ā€¢ Step 1: Connect the two features involved with a light pencil ā€¢ Step 2: Draw a true north line on the starting feature ā€¢ Step 3 : Draw a neat cross, on the starting point ā€¢ Step 4 : find the direction using the neat cross
  • 21. Example Find the direction of B from A. ā€¢ Mark the North line on starting point at A ā€¢ Draw a direction neat cross, on the starting point (at A) A B x x ā€¢ Draw the line connecting A to B. N NE E SE S NW SW ā€¢Direction of B from A is South East (SE)
  • 22. Bearings Rules: ā€¢ Are always written in three figures (e.g. 040Ā° instead of 40Ā°) ā€¢ Always measure the angle clockwise from the True North
  • 24. Measuring bearingsā€¦ Find the bearing of B from A. ā€¢ Mark the North line on at A (if there isnā€™t a North line draw one in) ā€¢ Place your protractor over the north line with 0Ā° at the top (true north). A B x x ā€¢ Draw the line connecting A to B.
  • 25. Measuring bearingsā€¦ Find the bearing of B from A. ā€¢Measure the angle clockwise from the North line to B ā€¢ Give the answer as a three- figure bearing The bearing of B from A is 134Ā°. A B
  • 26. Measuring bearingsā€¦ Find the bearing of A from B. ā€¢ Mark the North line on at B (if there isnā€™t a North line draw one in) ā€¢ Measure the angle clockwise from the North line to A A B x x ā€¢ Draw the line connecting B to A.
  • 27. Measuring bearingsā€¦ Find the bearing of A from B. ā€¢ Place your protractor over the north line with 0Ā° at the bottom. ā€¢ The angle has gone past 180Ā° so you will need to add your measurement to 180Ā° A B x x ā€¢ Because you are measuring clockwise you need to measure the exterior angle.
  • 28. Measuring bearingsā€¦ Find the bearing of A from B. ā€¢ The measurement from the bottom 0Ā° is 135Ā°. The bearing of A from B is 313Ā°. A B x x ā€¢ 133Ā° + 180Ā° = 313Ā°. 135 Ā°
  • 29. Determining location ā€¢ Involves using Latitude and longitude ā€¢ Latitude are line that runs from the west to the east while Longitude lines that runs from north to the south Symbols used ā€¢ Degrees(Ā°), minutes (ā€˜) and seconds (ā€œ). How to write Location( coordinates) ā€¢ In Southern Hemisphere we first write the latitude degree, minutes, seconds reading follow by south direction. ā€¢ Then followed by the longitude degree, minutes, second reading followed by the east direction. ā€¢ 24Ā°51ā€™45ā€™ā€™S29Ā°15ā€™30ā€™ā€™E
  • 30.
  • 31. Examples how to determine location? Find location of A (see next slide) a) In Degree and Minutes ā€¢ Latitude reading will be 17Ėš23 Ģ’S ā€¢ Longitude reading will be 19Ėš38 Ģ’E ā€¢ Therefore the Location will be 17Ėš23 Ģ’S 19Ėš38 Ģ’E
  • 32. b) Degrees, Minutes and Second For you to do this you need a ruler and calculator. See examples below
  • 33. A ā€¢ Firstly connect latitudes and longitudes lines to make a grid ā€¢ For latitude seconds measure from first latitude to the second latitude line in mm (b). ā€¢ Measure from first latitude to the point in mm (a). ā€¢ Use formalar š‘Ž š‘ x 60ā€ ā€¢ The final answer you add it to degrees and minutes of latitude
  • 34. A ā€¢ Firstly connect latitudes and longitudes lines to make a grid ā€¢ For longitude seconds measure from first longitude to the second longitude line in mm (b). ā€¢ Measure from first longitude to the point in mm (a). ā€¢ Use formalar š‘Ž š‘ x 60ā€ ā€¢ The final answer you get add it to degrees and minutes of longitude
  • 35. How to read other features on the map Relief ā€¢ Look for region uplands and lowlands ā€¢ State the highest point and the lowest point, ā€¢ Recognize landform features such as Plateau, Valley. ā€¢ Look for identifiable slopes ā€“ convex, concave, steeper or Gentle.
  • 36. Type of slopes on the map Gentle : Steep
  • 42. Spur
  • 45. Drainage ā€¢ Describe drainage density of river (High, Low or Medium) depending on number of streams forming a drainage ā€¢ Identify the drainage patterns (trellis, dendritic, radial, etc.) ā€¢ Recognize if the rivers are perennial or not ā€¢ Recognizable features of the river (waterfalls, rapids, braiding, meander, islands, ox bow lakes, etc) ā€¢ Identify stage of river courses (upper, middle or lower)
  • 50. Land use A useful method is to consider economic activities: Primary economic activities a) Farming ā€¢ Type of farming: Arable Farming (Crop Farming) or Pastoral Farming (livestock Farming) ā€¢ For Arable farming look out for cultivation, irrigation furrows, canals and pipelines, farm dams and Silos. ā€¢ For Livestock look out for kraals, windmills and dipping tanks
  • 51. b) Mining ā€¢ Open cast mining ā€¢ Look for name of the mine, Opencast mine, service railways, mine dump, excavations and diggings. c) Forestry ā€¢ Look out for plantations and forests names d) Fishing ā€¢ Look out for coastal quays and harbours
  • 52. Secondary economic activity industry (look for industrial location factors, market, raw material, power and water, labour, flat land and transport). Tertiary economic activity Look for services facilities indicated next to each service ā€¢ Education (School, University and Colleges) ā€¢ Recreation ( Caravan Park, Rec, Golf Course) ā€¢ Health /Medical service (Clinic and Hospitals) ā€¢ Shopping( Shops, Supermarkets and Store)
  • 53. Transport and communication ā€¢ Railways ā€¢ Main Roads ā€¢ Secondary roads ā€¢ Landing Strips/ Airports ā€¢ Hiking and Trail
  • 55. Photographs ā€¢ Horizontal photographs ā€¢ High oblique ā€¢ Low oblique ā€¢ Vertical /aerial photographs
  • 56. Horizontal photographs ā€¢ Advantages ā€¢ The photograph shows a lot of detail ā€¢ Disadvantages ā€¢ Shows a small area ā€¢ Objects in the foreground block out objects in the background ā€¢ Objects in the foreground appear larger than objects in the background ā€¢ Cannot use them for map drawing
  • 57. GROUND-LEVEL PHOTOGRAPH ļƒ˜Taken at ground-level, as you would normally see things.
  • 58. High oblique photographs ā€¢ Taken from a high vantage point such as top of a building. ā€¢ The horizon is visible Advantages ā€¢ Covers a larger area ā€¢ Shows a lot of information Disadvantages ā€¢ Less detail in the foreground ā€¢ Objects in the foreground block out objects in the background
  • 59. HIGH OBLIQUE PHOTOGRAPH ļƒ˜Taken from a high point (building), horizon is visible.
  • 60. Low oblique photographs ā€¢ These photographs are taken from a airplane at a angle. ā€¢ Horizon is not visible ā€¢ Advantages ā€¢ They show a larger area ā€¢ Shows much more information ā€¢ Disadvantages ā€¢ Objects in the foreground block out objects in the background ā€¢ Objects in the foreground appear larger than objects in the background
  • 61. LOW OBLIQUE PHOTOGRAPH ļƒ˜Taken from an aero plane, horizon not visible.
  • 62. Vertical photographs ā€¢ Taken from a airplane but the camera is tilted vertically down. ā€¢ Advantage ā€¢ No hidden areas ā€¢ Shows a lot of information ā€¢ Used to draw maps ā€¢ Disadvantages ā€¢ Height and surface slopes are not easy to identify ā€¢ A lot of experience is needed to obtain information from these photographs
  • 63. Other Graphical analysis Know how to read and complete the graphs below ā€¢ Bar graphs ā€¢ Line graphs ā€¢ Pie Chart ā€¢ Divided Bar graph ā€¢ Triangular graph ā€¢ Wind rose