Chapter 2 Mapping our World.

Slides:



Advertisements
Similar presentations
Maps Chapter 6, Section 3.
Advertisements

Mapping Our World Goals: Differentiate between latitude and longitude.
Mapping with the Electronic Spectrum
Mapping Our World Cartography What is the equator? Latitude
Objectives Vocabulary Compare and contrast different map projections.
Map Projections.
Ch.2: Mapping Our World Text ref. (pg.26).
Warm Up 9/16 Earth’s major spheres are the ______.
Ch- 7 Using Maps 1 K (What I know) W (Want to know) L (What I learned) Warm up- take out a piece of paper and do the “K” and the “W” for the above topic.
Chapter 2: Mapping Our World
Mapping our World Chap. 2 Latitude and Longitude 2.1 Types of Maps 2.2
California Standards 1h, 9d, 1. * Cartography – The science of map making. * A grid of the imaginary parallel and vertical lines are used to locate points.
Latitude and Longitude
MAPPING OUR WORLD.
Objectives Vocabulary Compare and contrast latitude and longitude.
EARTH SCIENCE Geology, the Environment and the Universe
Chapter 3: Models of Earth
2.1 Latitude and Longitude
Contour Mapping Topographic Maps – a detailed map showing hills, valleys, and other features of a specific area.
Maps are flat models of 3-D objects. All flat maps distort the shapes and areas of land masses to some extent. We will talk about 4 types of maps: Mercator.
Learning Goals Examine a map and articulate strengths and weaknesses of the map Correctly identify 6 different types of projections Differentiate between.
Mapping our world Chapter 2.
Chapter 2: Mapping Our World BIG Idea: Earth Scientists use mapping technologies to investigate and describe the world.
Finding Locations on Earth Chapter 3. Latitude  Latitude is the angular distance north or south of the equator.  Run parallel to the equator.  Called.
Maps as Models of the Earth Chapter 2 AC Earth Science 2009.
Mapping Our World Latitude and Longitude Cartography –Science of mapmaking –Uses imaginary grid of parallel lines and vertical lines to locate points on.
Chapter 6 Views of Earth Sections 2 & 3: Latitude and Longitude and Maps.
Word of the Day Nautical Mile: One minute of arc length of latitude or longitude at the equator, or 1852m.
remote sensing electromagnetic spectrum frequency Landsat satellite Objectives Compare and contrast the different forms of radiation in the electromagnetic.
Earth and Space Science
CHAPTER 2 MAPPING OUR WORLD.
EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.2 Mapping Earth’s Surface.
Earth & Space Science Chapter 2 Mapping Our World.
Mapping Earth Chapter 1 Earth Science. Ch1 L.1 Maps How can a map help determine location? Why are there different map projections for representing Earth’s.
MAPPING OUR WORLD. CARTOGRAPHY THE SCIENCE OF MAPMAKING.
Students will demonstrate understanding of and be able to use major reference lines on a map such as: Lattitude, Longitude, Prime Meridian, Equator. Students.
Cartography Mapping the World.
The Science of Map Making.  Separates the Earth into 2 halves a) Northern Hemisphere b) Southern Hemisphere.
Maps as Models of the Earth Table of Contents Section 1 You Are Here Section 2 Mapping the Earth’s Surface Section 3 Topographic Maps Chapter 2.
Chapter 3. Models of the Earth In order to locate points on Earth, we use models. Two general types of models: Maps Globes 2-Dimensional3-Dimensional More.
Time Zones Because Earth takes about 24 hours to rotate once on its axis, it is divided into 24 times zones, each representing a different hour. Latitude.
Vocabulary Remote Sensing Electromagnetic Spectrum Frequency
-presents- EEn Predict the locations of volcanoes, earthquakes, and faults based on information contained in a variety of maps.
Mapping Our World We will investigate several methods scientists use to map our world. The goal of creating any map is to be able to locate and obtain.
Types of Maps Cartography is the science of mapmaking. For thousands of years, people have used maps to define borders and to find places. What is a.
 Cartography – science of mapmaking  Equator circles Earth halfway between the north and south poles ◦ Separates Earth into 2 equal halves (hemispheres)
  Cartography  Cartography is the science of mapmaking.  Cartographers use an imaginary grid of parallel lines and vertical lines to locate exact points.
Chapter two Review Game
Mapping Our World Chapter 2 Earth Science.
Chapter 2 - Mapping Our World
Latitude and Longitude
Last page of mapping notes
Geographical Lines and Mapping
CHAPTER 1 LESSON 1 UNDERSTANDING MAPS.
Mapping Chapter 2.
Chapter 2-Mapping our World
Mapping Cont..
Chapter 6 Views of Earth.
Maps Ch. 1 Lesson 1.
Chapter 2-Mapping our World
Mapping Our World Cartography What is the equator? Latitude
Mapping Cont..
Latitude and Longitude
Welcome to Earth Science
Unit 1 Ch. 2 Mapping our World
Earth Science Ch. 1 Mapping the Earth.
Mapping Our World.
Chapter 2-Mapping our World
Chapter 2-Mapping our World
Remote Sensing.
Presentation transcript:

Chapter 2 Mapping our World

Latitude and Longitude Section 2.1 Latitude and Longitude Latitude Longitude You will be able to . . . Compare and Contrast latitude and longitude. Describe how time zones vary.

The science of mapmaking is called cartography. Lines of latitude are parallel. The latitude of the north pole is 90° north.

Longitude Longitude – Lines of longitude converge at the poles. The prime meridian represents 0° longitude.

Minutes Each degree of latitude or longitude is divided into 60 smaller units called minutes.

Seconds Each minute of latitude or longitude is divided into 60 smaller units called seconds. 6

Scale Each degree(°) = 111 km Each Minute(‘) = 1.85 km And Each Second(“) = 30.83 m Note: works for latitude only 7

Time Zones Earth is divided into 24 time zones.

International Date Line The International Date Line is another name for the 180° meridian.

International Date Line West Traveling West () across the International Date Line, you would advance your calendar one day. Sept. 1 Sept. 2

International Date Line East Traveling East () across the International Date Line, you would move your calendar back one day. Sept. 1 Aug. 31

Section 2.2 Types of Maps You will be able to . . . Compare and Contrast different map projections. Analyze topographic maps. Describe map characteristics such as map scales and map legends.

Distortion All flat maps distort either the shapes or the areas of landmasses because Earth is a curved, three-dimensional object.

Mercator A Mercator projection distorts areas near the poles. (the areas of landmasses near the poles are exaggerated)

Conic In a conic projection, there is very little distortion along one line of latitude, but the areas and shapes of landmasses near the top and bottom of the projection are distorted.

Gnomonic In a gnomonic projection, the direction and distance between landmasses are distorted. Polar Gnomonic Equatorial Gnomonic Oblique Gnomonic                                                                                                      Gnomonic projection are used by navigators to plot great-circle routes.

Topographic Topographic map a type of map that shows changes in elevation of Earth's surface

Contour Interval Each contour line should represent one elevation. If two lines cross, it means that the point where they cross has two elevations, which is impossible. The difference in elevation between two side-by-side contour lines is called the contour interval.

Legend & Scale A map legend explains what the symbols on a map represent. A graphic scale is a line broken into sections that represent units with each section representing a distance on Earth’s surface.

Section 2.3 Remote Sensing You will be able to . . . Compare and Contrast different the different forms of radiation in the electromagnetic spectrum. Discuss how satellites and sonar are used to map Earth’s surface and its oceans. Describe the Global Positioning System

Light/Electromagnetic Spectrum The frequency of an electromagnetic wave is the number of waves that pass a particular point each second.

Speed of Light The speed of light in a vacuum is 300,000 km/s.

Remote Sensing The process of collecting data about the Earth from above the surface. (Generally using the electromagnetic spectrum.)

GPS GPS - Global Positioning System allows its users to determine their exact position on Earth.

GPS Direction Elevation Position GPS satellites can relay information about all of the following: Direction Elevation Position

Landsat and Topex/Poseidon Both Landsat satellite and Topex/Poseidon satellite collect data about Earth by remote sensing. Topex/Poseidon Satellite Landsat Satellite Uses radar to map features on the ocean floor. Detects energy related to the warmth of surface features.

NOVA Science Now (time-out) Hyperlink on picture 

Mapping Exercise Each degree(°) = 111 km Each Minute(‘) = 1.85 km And Earth is a circle which has 360 degrees (◦) Each degree (◦) is divided into 60 minutes. Each minute is divided into 60 seconds Each degree(°) = 111 km Each Minute(‘) = 1.85 km And Each Second(“) = 30.83 m

Traveling When You Know your starting coordinates and the distance you travel (+) add 40° 45’ 16” , I travel 40° 55’ 16” , I travel 10’ 10” 10’ 10” 29

Distance between When You Know your starting coordinates and ending coordinates (-) subtract 40° 45’ 16” , Start 40° 55’ 16” , start 40° 20’ 15” Stop 39° 10’ 40” stop 30

Conversion When You need to convert degrees,minutes,seconds to a decimal Generally make it a fraction over 60 and add to the number to the left. 120° 40’ 25” = 31

Map Exercises http://geology.isu.edu/geostac/Field_Exercise/topomaps/exercise_1.htm