

Earth Science 2.7 and 2.8
Presentation
•
Science
•
9th Grade
•
Easy
+6
Standards-aligned
Marcus Page
Used 4+ times
FREE Resource
14 Slides • 4 Questions
1
2.7 Maps
2.8 Map Projections
2
Multiple Choice
What is this map tool called?
scale
map
compass rose
map title
3
What information does a map show?
Maps can convey a variety of information.
They can tell you where you are and provide details about a location.
Different maps show different types of information.
4
Maps as models
A map is a picture of specific parts of Earth’s surface.
Different maps provide different types of information.
Example: Road maps help you navigate on a road trip.
5
Map legends
The legend explains the symbols and features on the map.
Example: A scale of miles shows the distance represented on the map.
Most maps orient north at the top.
6
Types of maps
Political/Geographic Maps: Show state and country borders.
Satellite Maps: Display terrains and vegetation.
Relief Maps: Show elevations and contours.
Topographic Maps: Provide detailed elevation features.
Climate Maps: Indicate average temperatures and rainfall.
Precipitation Maps: Show the amount of rainfall in different areas.
Weather Maps: Track storms, air masses, and fronts.
Radar Maps: Visualize storms and rainfall.
Geologic Maps: Detail the types and locations of rocks.
7
Multiple Choice
Use the map legend to answer the questions. The triangles are a symbol for?
8
Summary
Maps are two-dimensional representations of a surface, usually Earth's.
They use symbols and legends to display complex information efficiently.
There are many types of maps, each designed to show different types of information.
9
2.8 Map projections
How does Greenland change size?
10
Does Greenland really change size?
No, Greenland does not change size! It's about how the map is made.
Different map projections make Greenland appear larger or smaller.
11
What is map projection?
Earth is a three-dimensional sphere.
To map Earth on flat paper, mapmakers use projections.
Projections can cause distortions, especially near the poles.
12
Multiple Choice
13
Multiple Choice
14
Mercator projection
Created by Gerardus Mercator in 1569.
Wraps a flat sheet of paper around a cylindrical model of Earth.
Distorts sizes near the poles, making Greenland look much larger.
15
Conic projection
Uses a cone shape to map Earth.
Better represents regions near the poles.
Reduces distortion compared to the Mercator projection.
16
Gnomonic projection
Projects Earth’s surface onto a flat piece of paper placed on one point.
Accurate near the point of contact but distorts areas further away.
Often used to map the poles.
17
Robinson projection
Developed by Arthur Robinson in 1963.
Uses mathematical formulas to reduce distortion.
Shapes and sizes of continents are closer to their true dimensions.
18
Summary
Map projections show Earth’s three-dimensional surface in two dimensions.
All projections cause some distortion.
Greenland’s size varies on different projections due to how they represent the poles.
2.7 Maps
2.8 Map Projections
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