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Mapping the Earth’s Surface Chapter 3.2
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Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Jan 18, 2016

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Page 1: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Mapping the Earth’s Surface

Chapter 3.2

Page 2: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Mapping the Earth’s Surface

1.Mapping the Earth’s Surfacea. Globes are very useful in

studying large features such as continents and oceans. However, they are generally too small to show small details such as streams and highways.

Page 3: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Mapping the Earh‘s Surface

b.To show and study the different features of earth, many different forms of maps have been developed.

c. Cartography is the science of map making and is a subfield of earth science and geography.

Page 4: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Map projections

1.Map Projectionsa.A map projections is a flat map

that represents the three-dimensional curved surface of a globe.

Page 5: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Map Projections

b. Three major map projections are Mercator, gnomonic, and conic projections.i.None of these are perfectly accurate

projections of the earth, but each one is beneficial for specific needs.

Page 6: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Mercator Projections1.Mercator Projections

a.This is like stretching the globe into a square or rectangle.

b.Meridians appear as straight parallel lines with an equal amount of space between them. i.This causes distortion of continents and

oceans near the poles, because on a globe meridians meet at the poles.

Page 7: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Mercator Projections

c. Advantages of Mercator Projectionsi.Longitude and latitude are on a grid

which makes it easy to locate positions with a simple ruler.

ii.Distortion of small areas is minimal.iii.Good tool used for navigation.

Page 8: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Mercator Projection

Page 9: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Gnomonic Projection

1.Gnomonic Projectiona.This is like placing a sheet of paper on the

globe, holding it tight so it only touches in one place, and projecting the globe’s image onto it.

b.Meridians and Parallels appear as flat lines, as if they were making contact with a globe in only one place.

Page 10: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Gnomonic Projection

c. Minimal distortion is caused at the point of “contact”. However, distortion increases as one moves away from the point of contact, but distortion is proportional in all directions.

Page 11: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Gnomonic Projectiond. Used in navigation for air travel.

i.Recall: Great circles are the shortest distance between any two points on the globe.

ii.When great circles are projected onto a gnomonic projection they appear as a straight line which can be used by pilots to find the shortest path between two points on earth.

Page 12: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Gnomonic Projection

Page 13: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Conic Projection

1.Conic Projectiona.This is like placing a paper cone over

the axis of the globe and transferring the globe’s image onto it. The cones base must touch one parallel of latitude.

b.Use in series to map a number of neighboring areas. Fitting all areas together will produce a continuous map.

Page 14: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Conic Projecions

c. Maps made this way are called polyconic projections.

d. Minimal distortions is present on these maps.

Page 15: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Conic Projections

Page 16: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Reading a Map1.Reading a Map

a.Maps provide information about the earth’s surface and are considered models of the earth.

b.Maps have many symbols that represent items such as cities, rivers, and roads.

c.Map symbols and meanings are explained in the map legend.

Page 17: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Map Legend

Page 18: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Map Compass

d. Maps are generally drawn with north at the top and south at the bottom. i. A compass is generally shown to state map

direction.

Page 19: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Map Scale

e. The scale of a map indicates the relationship between distance as shown on the map and actual distance on earth.

f. Scales may be presented as a graphic, fractional, or verbal scale.

Page 20: Mapping the Earth’s Surface Chapter 3.2. Mapping the Earth’s Surface 1.Mapping the Earth’s Surface a.Globes are very useful in studying large features.

Map Scale