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Maps—The Geographer’s
       Tool
  Cartography: The art and
   science of making maps
A 2-D View of a 3-D World
Maps Illustrate and Reinforce Our
Ideas about the World Around Us
Maps Illustrate and Reinforce Our
    Ideas about the World Around Us
   What we see, what we don’t see,
    and what we’re not willing to see…
Maps Illustrate and Reinforce Our
    Ideas about the World Around Us
   What we see, what we don’t see,
    and what we’re not willing to see…
   How we think about the world
    around us…
Maps Illustrate and Reinforce Our
    Ideas about the World Around Us
   What we see, what we don’t see,
    and what we’re not willing to see…
   How we think about the world
    around us…
   What is important to us and what is
    not…
Maps Illustrate and Reinforce Our
    Ideas about the World Around Us
 What we see, what we don’t see,
  and what we’re not willing to see…
 How we think about the world

  around us…
 What is important to us and what is

  not…
These things all “appear” on our maps
1600’s
1700’s
1800’s
G.I.S.
   Geographic
    Information Systems
    has revolutionized the
    way we make maps




   However, the
    computer program
    only depicts what we
    tell it to…
A Simplification or a Lie?
A Simplification or a Lie?
      “cartographic censorship”
A Simplification or a Lie?
                    “cartographic censorship”
“[B]asic maps of most cities show streets, landmark structures,
elevations, parks, churches, and large museums--but not
dangerous intersections, impoverished neighborhoods, high crime
areas, and other zones of danger and misery that could be
accommodated without sacrificing information about infrastructure
and terrain.
A Simplification or a Lie?
                     “cartographic censorship”
“[B]asic maps of most cities show streets, landmark structures,
elevations, parks, churches, and large museums--but not
dangerous intersections, impoverished neighborhoods, high crime
areas, and other zones of danger and misery that could be
accommodated without sacrificing information about infrastructure
and terrain.
“By omitting politically threatening or aesthetically unattractive
aspects of geographic reality...our topographic ‘base maps’ are
hardly basic to the concerns of public health and safety officials,
social workers, and citizens rightfully concerned about the well-
being of themselves and others.”
A Simplification or a Lie?
                     “cartographic censorship”
“[B]asic maps of most cities show streets, landmark structures,
elevations, parks, churches, and large museums--but not
dangerous intersections, impoverished neighborhoods, high crime
areas, and other zones of danger and misery that could be
accommodated without sacrificing information about infrastructure
and terrain.
“By omitting politically threatening or aesthetically unattractive
aspects of geographic reality...our topographic ‘base maps’ are
hardly basic to the concerns of public health and safety officials,
social workers, and citizens rightfully concerned about the well-
being of themselves and others.”

                         -Monmonier, How to Lie with Maps, p. 122
Globe vs. Map
Globe vs. Map
All flat maps distort shape or size or direction
All flat maps distort shape or size or direction
 We can hold one constant, but not all three
Map Projections
Map Projections
   Trying to take something round and
    make it flat isn’t easy (especially if
    you’re trying to make it into a
    rectangle)!
Map Projections
   Trying to take something round and
    make it flat isn’t easy (especially if
    you’re trying to make it into a
    rectangle)!
   Map projections attempt to do this
    by “projecting” an image of Earth’s
    surface onto a piece of paper
Cylindrical Projection
Cylindrical Projection




Imagine a light bulb in the center of a globe, with a sheet of paper
wrapped around it in the form of a cylinder. Meridians and parallels
would be "projected'' onto the cylinder as straight, parallel lines.
Meridians on these projections do not meet at the poles, so these
maps are increasingly stretched and distorted toward the poles.
Azimuthal or Planar Projection
Azimuthal or Planar Projection


A perfectly flat piece of paper (a
plane) would touch the globe at a
point (the tangent). This projection is
a good choice for maps with circular
or square shapes. When the point of
tangency is one of the poles,
meridians are shown as straight lines
radiating from the pole. If parallels
are then drawn as equally spaced
concentric circles, this projection
would be equidistant (scale is true
along any line radiating from the
center point, in this case the pole).
Conic Projection
Conic Projection




A cone of paper placed over a globe would touch its surface along
one standard line (usually a parallel). A cone that sliced through the
globe would intersect it twice, creating two standard parallels. Such
a projection is well-suited for showing areas in the middle-latitudes
with a mostly east-west extent (like the United States).
Pseudocylindrical Projection




Pseudocylindrical (or elliptical) projections normally have straight
parallels and curved meridians (usually equally spaced). The
Robinson Projection is a popular example. It was created to make
the world "look" right by keeping angular and areal distortions to a
minimum.
Interrupted Projection
Conformal vs. Equivalent Projections
“Reading” Maps
“Reading” Maps




(Lat.°)
“Reading” Maps




(Lat.°)(min')
“Reading” Maps




(Lat.°)(min') (sec”)
“Reading” Maps




(Lat.°)(min') (sec”) (N/S)
“Reading” Maps




(Lat.°)(min') (sec”) (N/S)   (Long.°)
“Reading” Maps




(Lat.°)(min') (sec”) (N/S)   (Long.°)(min')
“Reading” Maps




(Lat.°)(min') (sec”) (N/S)   (Long.°)(min') (sec”)
“Reading” Maps




(Lat.°)(min') (sec”) (N/S)   (Long.°)(min') (sec”) (E/W)
“Reading” Maps
In order to find your way around a map,
you need to know how standard map
coordinates are written:
 (Lat.°)(min') (sec”) (N/S)   (Long.°)(min') (sec”) (E/W)
“Reading” Maps
In order to find your way around a map,
you need to know how standard map
coordinates are written:
 (Lat.°)(min') (sec”) (N/S)   (Long.°)(min') (sec”) (E/W)
“Reading” Maps
In order to find your way around a map,
you need to know how standard map
coordinates are written:
 (Lat.°)(min') (sec”) (N/S)   (Long.°)(min') (sec”) (E/W)
“Reading” Maps
In order to find your way around a map,
you need to know how standard map
coordinates are written:
 (Lat.°)(min') (sec”) (N/S)   (Long.°)(min') (sec”) (E/W)



  Quest of the day: Where is this place?
“Reading” Maps
In order to find your way around a map,
you need to know how standard map
coordinates are written:
 (Lat.°)(min') (sec”) (N/S)   (Long.°)(min') (sec”) (E/W)



  Quest of the day: Where is this place?
        37°32’12”N 122°20’02”W
Quick Quiz:
Which of the following is written incorrectly?
Quick Quiz:
Which of the following is written incorrectly?


          a) 0º0º
Quick Quiz:
Which of the following is written incorrectly?


          a) 0º0º
          b) 0º180º
Quick Quiz:
Which of the following is written incorrectly?


          a) 0º0º
          b) 0º180º
          c) 38ºS 120ºE
Quick Quiz:
Which of the following is written incorrectly?


          a)   0º0º
          b)   0º180º
          c)   38ºS 120ºE
          d)   89º56’62”W 179º01’59”N
Elements of a Good Map
Elements of a Good Map

All maps need certain characteristics in
      order to be easily readable.
Elements of a Good Map

All maps need certain characteristics in
      order to be easily readable.


Elements of a Good Map

All maps need certain characteristics in
      order to be easily readable.



    So what is it that makes a map
Elements of a Good Map

All maps need certain characteristics in
      order to be easily readable.



    So what is it that makes a map
           a “good” map?
Elements of a Good Map
Elements of a Good Map
       Title
Elements of a Good Map
       Title
       Date
Elements of a Good Map
       Title
       Date
       Legend/Key
Elements of a Good Map
       Title
       Date
       Legend/Key
       Direction
Elements of a Good Map
       Title
       Date
       Legend/Key
       Direction
       Location
Elements of a Good Map
       Title
       Date
       Legend/Key
       Direction
       Location
       Index
Elements of a Good Map
       Title
       Date
       Legend/Key
       Direction
       Location
       Index
       Data Source
Elements of a Good Map
       Title
       Date
       Legend/Key
       Direction
       Location
       Index
       Data Source
       Projection Type
Elements of a Good Map
       Title
       Date
       Legend/Key
       Direction
       Location
       Index
       Data Source
       Projection Type
       Scale
Elements of a Good Map
       Title
       Date
       Legend/Key
       Direction
       Location
       Index
       Data Source
       Projection Type
       Scale
       Relief and Topography
Elements of a Good Map
       Title
       Date
       Legend/Key
       Direction
       Location
       Index
       Data Source
       Projection Type
       Scale
       Relief and Topography
       Design
Topographic Maps
   USGS—United
    States Geological
    Survey
How a Topographic Map is Made
Isolines
Isolines
Four basic characteristics:
Isolines
Four basic characteristics:
Isolines
Four basic characteristics:

1. Isolines always form closed shapes. The connecting section
   may be cut off at the edges of the map, but at some point
   all isolines meet and close.
Isolines
Four basic characteristics:

1. Isolines always form closed shapes. The connecting section
   may be cut off at the edges of the map, but at some point
   all isolines meet and close.
Isolines
Four basic characteristics:

1. Isolines always form closed shapes. The connecting section
   may be cut off at the edges of the map, but at some point
   all isolines meet and close.

2. Except in rare cases (such as an overhanging cliff), isolines
   do not cross.
Isolines
Four basic characteristics:

1. Isolines always form closed shapes. The connecting section
   may be cut off at the edges of the map, but at some point
   all isolines meet and close.

2. Except in rare cases (such as an overhanging cliff), isolines
   do not cross.
Isolines
Four basic characteristics:

1. Isolines always form closed shapes. The connecting section
   may be cut off at the edges of the map, but at some point
   all isolines meet and close.

2. Except in rare cases (such as an overhanging cliff), isolines
   do not cross.

3. The elevation difference between one isoline and the next
   is called an “interval”. Intervals may differ between maps,
   but are usually the same throughout any one map.
Isolines
Four basic characteristics:

1. Isolines always form closed shapes. The connecting section
   may be cut off at the edges of the map, but at some point
   all isolines meet and close.

2. Except in rare cases (such as an overhanging cliff), isolines
   do not cross.

3. The elevation difference between one isoline and the next
   is called an “interval”. Intervals may differ between maps,
   but are usually the same throughout any one map.
Isolines
Four basic characteristics:

1. Isolines always form closed shapes. The connecting section
   may be cut off at the edges of the map, but at some point
   all isolines meet and close.

2. Except in rare cases (such as an overhanging cliff), isolines
   do not cross.

3. The elevation difference between one isoline and the next
   is called an “interval”. Intervals may differ between maps,
   but are usually the same throughout any one map.

4. Where isolines are close together, there is a steep
   gradient, or slope, or a rapid change of some sort. Where
   they are further apart, there is a gentle gradient, slope, or
   slow change.
USGS Topo Maps



Take one and check it out!
Scale

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GEOG100--Lecture 03--Maps

  • 1. Maps—The Geographer’s Tool Cartography: The art and science of making maps
  • 2. A 2-D View of a 3-D World
  • 3. Maps Illustrate and Reinforce Our Ideas about the World Around Us
  • 4. Maps Illustrate and Reinforce Our Ideas about the World Around Us  What we see, what we don’t see, and what we’re not willing to see…
  • 5. Maps Illustrate and Reinforce Our Ideas about the World Around Us  What we see, what we don’t see, and what we’re not willing to see…  How we think about the world around us…
  • 6. Maps Illustrate and Reinforce Our Ideas about the World Around Us  What we see, what we don’t see, and what we’re not willing to see…  How we think about the world around us…  What is important to us and what is not…
  • 7. Maps Illustrate and Reinforce Our Ideas about the World Around Us  What we see, what we don’t see, and what we’re not willing to see…  How we think about the world around us…  What is important to us and what is not… These things all “appear” on our maps
  • 11.
  • 12.
  • 13. G.I.S.  Geographic Information Systems has revolutionized the way we make maps  However, the computer program only depicts what we tell it to…
  • 14.
  • 15.
  • 16.
  • 18. A Simplification or a Lie? “cartographic censorship”
  • 19. A Simplification or a Lie? “cartographic censorship” “[B]asic maps of most cities show streets, landmark structures, elevations, parks, churches, and large museums--but not dangerous intersections, impoverished neighborhoods, high crime areas, and other zones of danger and misery that could be accommodated without sacrificing information about infrastructure and terrain.
  • 20. A Simplification or a Lie? “cartographic censorship” “[B]asic maps of most cities show streets, landmark structures, elevations, parks, churches, and large museums--but not dangerous intersections, impoverished neighborhoods, high crime areas, and other zones of danger and misery that could be accommodated without sacrificing information about infrastructure and terrain. “By omitting politically threatening or aesthetically unattractive aspects of geographic reality...our topographic ‘base maps’ are hardly basic to the concerns of public health and safety officials, social workers, and citizens rightfully concerned about the well- being of themselves and others.”
  • 21. A Simplification or a Lie? “cartographic censorship” “[B]asic maps of most cities show streets, landmark structures, elevations, parks, churches, and large museums--but not dangerous intersections, impoverished neighborhoods, high crime areas, and other zones of danger and misery that could be accommodated without sacrificing information about infrastructure and terrain. “By omitting politically threatening or aesthetically unattractive aspects of geographic reality...our topographic ‘base maps’ are hardly basic to the concerns of public health and safety officials, social workers, and citizens rightfully concerned about the well- being of themselves and others.” -Monmonier, How to Lie with Maps, p. 122
  • 24.
  • 25. All flat maps distort shape or size or direction
  • 26. All flat maps distort shape or size or direction We can hold one constant, but not all three
  • 28. Map Projections  Trying to take something round and make it flat isn’t easy (especially if you’re trying to make it into a rectangle)!
  • 29. Map Projections  Trying to take something round and make it flat isn’t easy (especially if you’re trying to make it into a rectangle)!  Map projections attempt to do this by “projecting” an image of Earth’s surface onto a piece of paper
  • 31. Cylindrical Projection Imagine a light bulb in the center of a globe, with a sheet of paper wrapped around it in the form of a cylinder. Meridians and parallels would be "projected'' onto the cylinder as straight, parallel lines. Meridians on these projections do not meet at the poles, so these maps are increasingly stretched and distorted toward the poles.
  • 32. Azimuthal or Planar Projection
  • 33. Azimuthal or Planar Projection A perfectly flat piece of paper (a plane) would touch the globe at a point (the tangent). This projection is a good choice for maps with circular or square shapes. When the point of tangency is one of the poles, meridians are shown as straight lines radiating from the pole. If parallels are then drawn as equally spaced concentric circles, this projection would be equidistant (scale is true along any line radiating from the center point, in this case the pole).
  • 35. Conic Projection A cone of paper placed over a globe would touch its surface along one standard line (usually a parallel). A cone that sliced through the globe would intersect it twice, creating two standard parallels. Such a projection is well-suited for showing areas in the middle-latitudes with a mostly east-west extent (like the United States).
  • 36. Pseudocylindrical Projection Pseudocylindrical (or elliptical) projections normally have straight parallels and curved meridians (usually equally spaced). The Robinson Projection is a popular example. It was created to make the world "look" right by keeping angular and areal distortions to a minimum.
  • 46. “Reading” Maps (Lat.°)(min') (sec”) (N/S) (Long.°)(min') (sec”)
  • 47. “Reading” Maps (Lat.°)(min') (sec”) (N/S) (Long.°)(min') (sec”) (E/W)
  • 48. “Reading” Maps In order to find your way around a map, you need to know how standard map coordinates are written: (Lat.°)(min') (sec”) (N/S) (Long.°)(min') (sec”) (E/W)
  • 49. “Reading” Maps In order to find your way around a map, you need to know how standard map coordinates are written: (Lat.°)(min') (sec”) (N/S) (Long.°)(min') (sec”) (E/W)
  • 50. “Reading” Maps In order to find your way around a map, you need to know how standard map coordinates are written: (Lat.°)(min') (sec”) (N/S) (Long.°)(min') (sec”) (E/W)
  • 51. “Reading” Maps In order to find your way around a map, you need to know how standard map coordinates are written: (Lat.°)(min') (sec”) (N/S) (Long.°)(min') (sec”) (E/W) Quest of the day: Where is this place?
  • 52. “Reading” Maps In order to find your way around a map, you need to know how standard map coordinates are written: (Lat.°)(min') (sec”) (N/S) (Long.°)(min') (sec”) (E/W) Quest of the day: Where is this place? 37°32’12”N 122°20’02”W
  • 53. Quick Quiz: Which of the following is written incorrectly?
  • 54. Quick Quiz: Which of the following is written incorrectly? a) 0º0º
  • 55. Quick Quiz: Which of the following is written incorrectly? a) 0º0º b) 0º180º
  • 56. Quick Quiz: Which of the following is written incorrectly? a) 0º0º b) 0º180º c) 38ºS 120ºE
  • 57. Quick Quiz: Which of the following is written incorrectly? a) 0º0º b) 0º180º c) 38ºS 120ºE d) 89º56’62”W 179º01’59”N
  • 58. Elements of a Good Map
  • 59. Elements of a Good Map All maps need certain characteristics in order to be easily readable.
  • 60. Elements of a Good Map All maps need certain characteristics in order to be easily readable. 
  • 61. Elements of a Good Map All maps need certain characteristics in order to be easily readable.  So what is it that makes a map
  • 62. Elements of a Good Map All maps need certain characteristics in order to be easily readable.  So what is it that makes a map a “good” map?
  • 63.
  • 64.
  • 65.
  • 66. Elements of a Good Map
  • 67. Elements of a Good Map  Title
  • 68. Elements of a Good Map  Title  Date
  • 69. Elements of a Good Map  Title  Date  Legend/Key
  • 70. Elements of a Good Map  Title  Date  Legend/Key  Direction
  • 71. Elements of a Good Map  Title  Date  Legend/Key  Direction  Location
  • 72. Elements of a Good Map  Title  Date  Legend/Key  Direction  Location  Index
  • 73. Elements of a Good Map  Title  Date  Legend/Key  Direction  Location  Index  Data Source
  • 74. Elements of a Good Map  Title  Date  Legend/Key  Direction  Location  Index  Data Source  Projection Type
  • 75. Elements of a Good Map  Title  Date  Legend/Key  Direction  Location  Index  Data Source  Projection Type  Scale
  • 76. Elements of a Good Map  Title  Date  Legend/Key  Direction  Location  Index  Data Source  Projection Type  Scale  Relief and Topography
  • 77. Elements of a Good Map  Title  Date  Legend/Key  Direction  Location  Index  Data Source  Projection Type  Scale  Relief and Topography  Design
  • 78. Topographic Maps  USGS—United States Geological Survey
  • 79.
  • 80.
  • 81.
  • 82.
  • 83. How a Topographic Map is Made
  • 87. Isolines Four basic characteristics: 1. Isolines always form closed shapes. The connecting section may be cut off at the edges of the map, but at some point all isolines meet and close.
  • 88. Isolines Four basic characteristics: 1. Isolines always form closed shapes. The connecting section may be cut off at the edges of the map, but at some point all isolines meet and close.
  • 89. Isolines Four basic characteristics: 1. Isolines always form closed shapes. The connecting section may be cut off at the edges of the map, but at some point all isolines meet and close. 2. Except in rare cases (such as an overhanging cliff), isolines do not cross.
  • 90. Isolines Four basic characteristics: 1. Isolines always form closed shapes. The connecting section may be cut off at the edges of the map, but at some point all isolines meet and close. 2. Except in rare cases (such as an overhanging cliff), isolines do not cross.
  • 91. Isolines Four basic characteristics: 1. Isolines always form closed shapes. The connecting section may be cut off at the edges of the map, but at some point all isolines meet and close. 2. Except in rare cases (such as an overhanging cliff), isolines do not cross. 3. The elevation difference between one isoline and the next is called an “interval”. Intervals may differ between maps, but are usually the same throughout any one map.
  • 92. Isolines Four basic characteristics: 1. Isolines always form closed shapes. The connecting section may be cut off at the edges of the map, but at some point all isolines meet and close. 2. Except in rare cases (such as an overhanging cliff), isolines do not cross. 3. The elevation difference between one isoline and the next is called an “interval”. Intervals may differ between maps, but are usually the same throughout any one map.
  • 93. Isolines Four basic characteristics: 1. Isolines always form closed shapes. The connecting section may be cut off at the edges of the map, but at some point all isolines meet and close. 2. Except in rare cases (such as an overhanging cliff), isolines do not cross. 3. The elevation difference between one isoline and the next is called an “interval”. Intervals may differ between maps, but are usually the same throughout any one map. 4. Where isolines are close together, there is a steep gradient, or slope, or a rapid change of some sort. Where they are further apart, there is a gentle gradient, slope, or slow change.
  • 94. USGS Topo Maps Take one and check it out!
  • 95. Scale

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