1. Maps and Map Skills

2. Kinds of Maps General Reference Maps
Provide the reader general information about an area or place.
Thematic Maps
Provide more specific information about an area or place than general reference maps.

3. General reference

4. Thematic Map

5. Maps are important tools for geographers.
A globe is a better model of Earth than a map, but a globe has disadvantages that a map does not have

6. Reading Maps Map Parts Title Legend or Key Grid System Direction Scale
Map orientation – This has to do with direction

7. Compass
Title
Scale

8. Grid System

9. Large Scale and Small Scale Maps
A large-scale map shows a small area such as a neighborhood street in great detail.
A small-scale map shows a large area such as a country or a continent in comparatively lesser detail.
Small Area = Large Scale
Large Area = Small Scale

10. Small Area = Large Scale Large Area = Small Scale

11. Compass
Is used to orient a map toward north

12. Latitude and Longitude

13. Latitude
The set of lines crossing the Earth’s surface horizontally, Circling east and west.
Each line of latitude is always an equal distance from the next.
They are also known as parallels. All latitude lines are parallel to each other.

14. Longitude
A set of lines that run vertically along Earth’s surface from the North Pole to the South Pole

15. Global Grid
When lines of latitude and longitude cross a grid is formed. The grid is used to located certain places on earth

16. Each line has an Identifying number called degrees, or parts of a circle. (410 )
Degrees, can be further divided into minutes, or parts of a degree. There are 60 minutes, or parts of a degree. (10’)
Minutes can be divided into even smaller parts called seconds. There are 60 seconds in each minute. (10”)
41010’10”
410
Degrees
Minutes
10’
Seconds
10”

17. Direction
The other part needed to locate places on Earth is direction.
Cardinal directions are: north, south, east, and west.
Intermediate directions are: northeast, southeast, northwest, and southwest. They are located midway between the cardinal directions.

18. Using Latitude & Longitude to Locate Places
Lines of latitude are numbered based on how far north or south they are from an imaginary line called the equator
This line circles the Earth exactly halfway between the NP and SP.
The equator’s latitude degree is 00. There are 90 degrees between it and each of the poles.
Area between the equator and NP is “north” latitude (220N)
Area between the equator and SP is “south” latitude (220S)

20. This line is called the Prime Meridian.
Lines of longitude are numbered based on how far east or west they are from another imaginary line.
This line is called the Prime Meridian.
Prime Meridian’s longitude degree is 00.
There are 1800 of longitude east of the PM and 1800 degrees west of it.
Area east of the PM is known as “east” longitude. (1200E)
Area west of the PM is known as “west” longitude. (1200W)

22. Prime Meridian & International Date Line
The prime meridian does not circle the globe as the equator does.
The PM runs from the NP to SP
At 1800 on the other side of the globe the meridian is called the international date line.

23. Hemispheres
The earth can be divided into halves. Each of these halves is called a hemisphere.

24. Hemispheres at the Equator
The ½ north of the equator is called the northern hemisphere
The ½ south of the equator is called the southern hemisphere

25. Hemispheres at Prime Meridian and International Date Line
Earth can also be divided into hemispheres at the circle formed by the prime meridian and International date line
The ½ east of the prime meridian is called the eastern hemisphere.
The ½ west of the prime meridian is called the western hemisphere.

27. Making Maps Gathering Information Problem of Distortion Map Properties
Map Projections
Cartographers (Mapmakers)

28. Gathering Information
Surveying
Aerial Photography (Air Planes)
Remote Sensing (Satellites)

29. Problem of Distortion
Features are stretched to put Earth’s information onto a map.

30. Map Properties No map can have all of the properties at once
Equal areas
Conformality
Consistent Scale
True-Compass Directions

31. Equal areas
Places shown have the same proportions as they do on Earth.
Example: Greenland 1/8 land area of S. America

32. Conformality Having correct shapes. Shows true shapes.
Can show larger areas as closely as possible to their true shapes

33. Consistent Scale Uses the same scale for all parts of the map.
Shows the true distances between places on Earth
In most Cases maps showing large areas cannot be consistent-scale maps.

34. •True-Compass Direction
Parallels and meridians appear as straight lines.
By following these lines you will be following the cardinal directions of N,S,E,&W.
Straight line between two points on map determines exact directions and set course. (Navigators use these maps)

35. Map Projections Cylindrical Projections Conic Projections
Flat Plane Projections
Gnomonic Projection
Robinson Projection
Goode’s Interrupted

36. Cylindrical Projections
Straight lines of latitude and Longitude are Perpendicular
Little distortion near the equator
Best Known:
Mercator –
conformal and true-compass direction map, but distortion near poles makes size of land and water areas inaccurate. Land shapes correct – areas distorted – valuable to navigator

37. Cylindrical

38. Conic Projections Cannot map the entire world.
Used for middle latitudes between 300 and 600 north latitudes, and between 300 and 600 south latitudes
Best Known:
Lambert Conformal Conical
Important because it shows the true shapes of areas.
Albers Equal Area Conical
Consistent scale and is used when the size of land and water areas must be accurate. (military and engineering maps)

39. Conic

40. Albers Equal Area Conical

41. Flat Plane Projections
Used to map areas of the North and South poles. Areas near that point show little distortion
Farther away from the point the greater the distortion of area, shape, and scale.
Shows no more that ½ of the Earth at one time.
Also called Azimuthal Projection

42. Flat Plane Map

43. Gnomonic Projection
Circles of latitude lines and straight longitude lines form a wheel-like pattern.
Especially useful to navigators because the shortest distance between two places on the map is found by drawing a straight line between them {this line is actually a part of a great circle – any imaginary line that circles Earth and divides it into 2 equal parts
Navigators use these along with true-compass direction maps to make their travel plans.

44. Gnomonic Projection

45. Robinson Projection Equal areas – shown with high degree of accuracy
Conformal except near edges of map where distortion increases
Valuable for showing entire world.

46. Goode’s Interrupted High degree of accuracy in area and shape
Distorted direction and scale.
Valuable for showing Land masses.

47. Points to Remember
The projection one chooses to use depends on the information one wants.
All Maps are projections – they transfer Earth’s features from the globe to a flat surface (map).
When large areas of Earth are mapped, distortion is more serious.
When mapping small areas like cities, distortion is not usually evident.