Top Banner
EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth
16

EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Jan 05, 2016

Download

Documents

Cornelius May
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

EARTH AND SPACE SCIENCE

Chapter 3 Models of the Earth

3.1 Finding Locations on Earth

Page 2: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

3.1 Finding Locations on Earth Objectives

• Distinguish between latitude and longitude.

• Explain how latitude and longitude can be used to locate places on Earth’s surface.

• Explain how a magnetic compass can be used to find directions on Earth’s surface.

Page 3: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Introduction

• Since Earth is a sphere, there is no top, sides, or bottom to use as reference points for finding location.

• To solve this problem, Earth’s axis of rotation is used to establish reference points.

• The reference points established where the axis transcends the Earth’s surface are the North and South geographic poles.

• The equator, a circle between the poles, divides the Earth into the Northern and Southern hemispheres.

Page 4: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Latitude

• Lines of latitude can be thought of as a set of parallel circles used to describe positions north and south of the equator.

• Lines of latitude run east and west.

• Latitude is the angular distance north or south of the equator.

Page 5: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Latitude

• Latitude is measured in degrees.• The distance from the equator to a pole is ¼

that of the circle that would be formed by going all the way around the Earth.

• The Earth, being a sphere, is 360° all the way around, so ¼ of that would be 90°.

• Each pole is 90° latitude in its respective hemisphere.

• Each degree of latitude is about 111 km (1/360th of the Earth’s diameter).

Page 6: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Latitude

• Each degree of latitude consists of 60 equal parts called minutes (‘).

• Each minute of latitude is equal to 1.85 km.

• Each minute of latitude is divided into 60 equal parts called seconds (“).

Page 7: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Longitude

• East-west locations are established by using meridians, semicircles that run from pole to pole along the curvature of the Earth.

• Prime meridian (0° longitude) is located in Greenwich, England.

Page 8: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Longitude

• The circumference of the world is 360°, so half way around the world is 180°.

• All locations west of the prime meridian have longitudes between 0°and 180° west and locations east of the prime meridian have longitudes between 0°and 180° east.

• Lines of longitude are not parallel, they are farthest apart at the equator (about 111 km) and get closer toward the poles.

• Exact locations on the surface of Earth can be stated with a latitude and longitude, such as Oneonta High School at 33°56’02”N 86°29’47”W.

Page 9: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Great Circles

• A great circle is any circle that divides the globe into halves, or marks the circumference of the globe.

• Great circles are often used for navigation, especially by long-distance aircraft.

• Great circles can run in any direction around the globe.

• The route along a great circle is the shortest distance between the two widely spaced points.

Page 10: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.
Page 11: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Finding Direction

• A magnetic compass may be used to find direction on Earth due to the Earth’s magnetic field.

• The geographic poles are located in different places than the Earth’s geomagnetic poles.

• Magnetic declination is the angle between the direction of the geographic pole and the direction in which the compass needle points.

• Magnetic declination has been determined for points all over the Earth.

• The magnetic declination for points all over the globe are changing because the Earth’s magnetic field is constantly changing.

Page 12: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Finding Direction

• When a person uses a compass, it is important to figure in the magnetic declination to determine geographic north.

• Determining geographic north is important in mapmaking and navigation.

• Global positioning system (GPS) is a satellite navigation system that is based on a global network of 24 satellites that transmit radio signals to Earth’s surface.

• A GPS receiver uses signals from three satellites to determine latitude, longitude, and elevation.

• Personal GPS receivers are accurate up to 10 to 15 meters.

Page 13: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.
Page 14: EARTH AND SPACE SCIENCE Chapter 3 Models of the Earth 3.1 Finding Locations on Earth.

Magnetic Declination