MAPPING OUR WORLD. MAPPING Cartography- Cartography- science of map makingscience of map making.

Slides:



Advertisements
Similar presentations
Mapping Our World Goals: Differentiate between latitude and longitude.
Advertisements

Earth Science – Unit 1.1 Reading Topographic Maps
FIELD METHODS IN ENVIRONMENTAL GEOLOGY LABORATORY GEOS 3110
Jeopardy Time Maps Q $100 Q $100 Q $100 Q $100 Q $100 Q $200 Q $200
Chapter 2 Measuring Earth
Topographic Mapping Honors Earth Science Parkland High School.
Maps.
Chapter 2: Mapping Our World
Mapping Earth's Surface Review and Assessment Answers
Topographic Map Vocabulary
Coordinate System Unit 1: Mapping the Earth
MAPPING OUR WORLD.
Finding Locations on Earth 3.1
Section 1: Finding Locations on EarthFinding Locations on Earth
3 Models of Earth 3.1 Modeling the Planet 3.2 Mapmaking and Technology
World Geographic Grid Fig. 1-8: The world geographic grid consists of meridians of longitude and parallels of latitude. The prime meridian ( 0º) passes.
Chapter 2: Mapping Our World BIG Idea: Earth Scientists use mapping technologies to investigate and describe the world.
Mapping Our World Section 2.1.
Chapter 3 Models of Earth.
Finding Locations on Earth Chapter 3. Latitude  Latitude is the angular distance north or south of the equator.  Run parallel to the equator.  Called.
Models of the Earth. Latitude Also called parallelsAlso called parallels Measured in degrees north or southMeasured in degrees north or south Equator.
The Earth © Lisa Michalek.
Maps Projections of The Earth. Cardinal Directions North, South, East, and West are all Cardinal Directions.
Chapter 6 Views of Earth Sections 2 & 3: Latitude and Longitude and Maps.
Latitude, Longitude, and Maps.  Cartography is the science of making maps.  Use of imaginary grid of parallel and vertical lines to give exact locations.
Lines of Latitude & Longitude
CHAPTER 2 MAPPING OUR WORLD.
Mapping.
Mapping The art of mapmaking is known as cartography - Has changed a lot over time (just 500 years ago the Earth was flat!!) Practical reasons such as.
Mapping. What is a map? It is a representation of something (Earth, stars, solar system, a building, etc… It is a representation of something (Earth,
Chapter 5 The Changing Surface of Earth
Models of the Earth Section 1 Preview Key Ideas Latitude Longitude Comparing Latitude and Longitude Great Circles Finding Direction Section 1: Finding.
Cartography Study of Mapmaking.
Table of Contents Exploring Earth’s Surface Models of Earth Topographic Maps Mapping Earth’s Surface.
The Science of Map Making.  Separates the Earth into 2 halves a) Northern Hemisphere b) Southern Hemisphere.
Topographic maps. Features on a Topographic Map Relief: difference in elevation between any two points– hills, valleys, mountains Water Features: lakes,
Topographic & Geologic Maps Plus: Latitude and Longitude!
Global Grid Mapping a 3-dimensional world in 2 dimensions.
Model = anything that represents the properties of an object Physical Types of models: Globes Mathematical Mental Mechanical Graphic Equations Water Molecule.
Finding Locations on Earth. Typical Graph This is an example of a typical graph we are all familiar with. The graph is made up of different “points” with.
-presents- EEn Predict the locations of volcanoes, earthquakes, and faults based on information contained in a variety of maps.
 Cartography – science of mapmaking  Equator circles Earth halfway between the north and south poles ◦ Separates Earth into 2 equal halves (hemispheres)
CATALYST On a sticky: 1.Draw a compass and all its parts.
What is a map? A Map is a two or three-dimensional model or representation of the Earth’s surface. 2-Dimensional map.
  Cartography  Cartography is the science of mapmaking.  Cartographers use an imaginary grid of parallel lines and vertical lines to locate exact points.
Mapping Our World Chapter 2 Earth Science.
Maps as Models of the Earth
Chapter 2 Measuring Earth
Chapter 2 - Mapping Our World
Mapping.
Chapter 3 Objectives Distinguish between latitude and longitude.
Earth Science Regents Review
The Earth © Lisa Michalek.
Latitude and Longitude Types of Maps Remote Sensing
Mapping Chapter 2.
Chapter 2-Mapping our World
Coordinate System Unit 1: Mapping the Earth
Chapter 2-Mapping our World
Mapping Our World Cartography What is the equator? Latitude
1.3: Representing Earth’s Surface
Welcome to Earth Science
How do you use a time zone map. Do Now: Times vary around the globe
Earth Science – Unit 1.1 Reading Topographic Maps
Mapping.
Mapping Our World.
Chapter 2-Mapping our World
Mapping.
Chapter 2-Mapping our World
Modeling the Planet Chapter 3
Models of the Earth Earth Science Chapter 3.
Presentation transcript:

MAPPING OUR WORLD

MAPPING Cartography- Cartography- science of map makingscience of map making

Maps *Flat models of 3-dimensional spaces **Earth is always distorted on maps

Typical Graph This is an example of a typical graph we are all familiar with. This is an example of a typical graph we are all familiar with. The graph is made up of different “points” with lines that connect the points. The graph is made up of different “points” with lines that connect the points. The points are referenced to the x and y axis The points are referenced to the x and y axis

Maps are Similar to Graphs Let each of the four quarters be designated by North or South and East or West. Let each of the four quarters be designated by North or South and East or West. N S EW

What are the 0 points? Equator – Equator – Separates the Earth into two equal halves called the northern hemisphere and the southern hemisphereSeparates the Earth into two equal halves called the northern hemisphere and the southern hemisphere It is an imaginary belt that runs halfway point between the North Pole and the South Pole.It is an imaginary belt that runs halfway point between the North Pole and the South Pole. Equator

What are the O points? Prime Meridian – Prime Meridian – Divides the Earth runningDivides the Earth running North -South Separates the Earth into two halves – the Eastern hemisphere and the Western hemisphereSeparates the Earth into two halves – the Eastern hemisphere and the Western hemisphere Goes through Greenwich, England – home of Royal Naval ObservatoryGoes through Greenwich, England – home of Royal Naval Observatory PRIMEPRIME MERIDIANMERIDIAN

East West, North South on the Earth The N tells us we’re north of the Equator. The S tells us we’re south of the Equator. The N tells us we’re north of the Equator. The S tells us we’re south of the Equator. The E tells us that we’re east of the Prime Meridian. The W tells us that we’re west of the Prime Meridian. The E tells us that we’re east of the Prime Meridian. The W tells us that we’re west of the Prime Meridian. (N, W) (N, E) (S, W) (S, E)

Latitude and Longitude The earth is divided into lots of reference lines called latitude and longitude. The earth is divided into lots of reference lines called latitude and longitude.

What is Latitude? Latitude is the distance from the equator along the Y axis. Latitude is the distance from the equator along the Y axis. Lines running parallel to equator Lines running parallel to equator Measures NORTH – SOUTH, but runs East- West Measures NORTH – SOUTH, but runs East- West All points along the equator have a value of 0 degrees latitude. All points along the equator have a value of 0 degrees latitude. North pole = 90°N North pole = 90°N South pole = 90°S South pole = 90°S Values are expressed in terms of degrees. Values are expressed in terms of degrees. Y X 90°S 90°N

What is Latitude? Each degree of latitude is divided into 60 minutes. Each degree of latitude is divided into 60 minutes. Each minute is divided into 60 seconds. Each minute is divided into 60 seconds. Ex: coordinates of Sunny Hills HS Ex: coordinates of Sunny Hills HS 33°52′48″N 117°55′43″W Y X 90°S 90°N This is also true of longitude.

What is Longitude? Longitude is the distance from the prime meridian along the X axis. Longitude is the distance from the prime meridian along the X axis. Lines running parallel to Prime Meredian Lines running parallel to Prime Meredian Measures EAST – WEST, but runs North-South Measures EAST – WEST, but runs North-South All points along the prime meridian have a value of 0 degrees longitude. All points along the prime meridian have a value of 0 degrees longitude. The earth is divided into two parts, or hemispheres, of east and west longitude. The earth is divided into two parts, or hemispheres, of east and west longitude. Y X 180°W 180°E

What is Longitude? The earth is divided into 360 equal slices (meridians) The earth is divided into 360 equal slices (meridians) 180 west and 180 east of the prime meridian 180 west and 180 east of the prime meridian Y X 180°W 180°E

The Size of 1 o Latitude Latitude degree of latitude is approximately 69 miles, and a minute of latitude is approximately 1.15 milesdegree of latitude is approximately 69 miles, and a minute of latitude is approximately 1.15 miles Longitude Longitude A degree of longitude varies in size – it decreases to zero as meridians come together at the polesA degree of longitude varies in size – it decreases to zero as meridians come together at the poles At the equator, it is approximately 69 miles, the same size as a degree of latitude.At the equator, it is approximately 69 miles, the same size as a degree of latitude. At a latitude of 45 degrees, a degree of longitude is approximately 49 miles.At a latitude of 45 degrees, a degree of longitude is approximately 49 miles.

Coordinate System

Time Zones The Earth is divided into 24 time zones The Earth is divided into 24 time zones Each time zone is 15˚ wideEach time zone is 15˚ wide There are 6 different time zones in the U.S.There are 6 different time zones in the U.S.

International Date Line The International Date Line, or 180˚ meridian, serves as the transition line for calendar days The International Date Line, or 180˚ meridian, serves as the transition line for calendar days If you were traveling west across the IDL, you would advance your calendar one day.If you were traveling west across the IDL, you would advance your calendar one day. If you were traveling east across the IDL, you would move your calendar back one day.If you were traveling east across the IDL, you would move your calendar back one day.

Earth’s Magnetic Field Our planet has a magnetic field as if a giant bar magnet were buried within Earth. Our planet has a magnetic field as if a giant bar magnet were buried within Earth. When you use a magnetic compass, the compass needle points toward Earth’s magnetic pole that is very close to the geographic north pole. When you use a magnetic compass, the compass needle points toward Earth’s magnetic pole that is very close to the geographic north pole.

Mercator Projections: Mercator Projections: 1. Parallel lines of latitude and longitude 2. Land masses near the poles are exaggerated

Rotation The Earth rotates 15 o of longitude every hour The Earth rotates 15 o of longitude every hour 24 lines of longitude (24 hours) in one day 24 lines of longitude (24 hours) in one day 15 x 24 = 360 o total (full circle) 15 x 24 = 360 o total (full circle) 180 o longitude on each side of Prime Meridian180 o longitude on each side of Prime Meridian

See If You Can Tell In Which Quarter These Lon/Lats Are Located 1. 41°N, 21°E 1. 41°N, 21°E 2. 37°N, 76°W 2. 37°N, 76°W 3. 72°S, 141°W 3. 72°S, 141°W 4. 7°S, 23°W 4. 7°S, 23°W 5. 15°N, 29°E 5. 15°N, 29°E 6. 34°S, 151°E 6. 34°S, 151°E AB C D

1. B 1. B 2. A 2. A 3. C 3. C 4. C 4. C 5. B 5. B 6. D 6. D

Topographic Maps

Topographic Map A graphical illustration of the 3-D shape of the land at the surface of the earth A graphical illustration of the 3-D shape of the land at the surface of the earth Shows changes in elevation as well as land features such as rivers or roads Shows changes in elevation as well as land features such as rivers or roads

Features of Topographic Maps Relationship between 3D and 2D representation 3D view 2D view

Topographic Map Show the shape of the Earth’s Surface. Contour lines drawn on a map give the elevations for a region. Where the lines are close, the slope of the ground is steep. Where the lines are far apart, the slope of the ground is gentle.

Contour Lines Imaginary lines that connects points of equal elevation (height above sea level) Imaginary lines that connects points of equal elevation (height above sea level)

Contour Lines contour lines do not intersect, branch or cross, except in a vertical or overhanging cliff. When contour lines cross a stream, they form a “V” with the point of the V pointing upstream

Contour Lines steep slopes are shown by closely spaced contour lines gentle slopes are shown by widely spaced contour lines

Depression Contour Lines When the elevation is lower than the surroundin g area there are “hachures” on the line When the elevation is lower than the surroundin g area there are “hachures” on the line

Contour Interval The difference in elevation between two side-by-side lines The difference in elevation between two side-by-side lines Each map has a unique contour interval, so locate label on the map Each map has a unique contour interval, so locate label on the map

Contour Map Example On this map, the vertical distance between each of the contour lines is 10 feet. 1.Which hill is higher, hill A or hill B? 2.Which hill is steeper, hill A or hill B? 3.How many feet of elevation are there between contour lines? 4.How high is hill A? Hill B? 5.Are the contour lines closer on hill A or hill B?

Determining Gradient and Slope The rate of change in field values between two points in a field. The rate of change in field values between two points in a field. The average slope, or gradient, between any two points (A and B) on a mountain can be determined from a contour map. The average slope, or gradient, between any two points (A and B) on a mountain can be determined from a contour map. Gradient = Difference between A & B Gradient = Difference between A & B Distance between A & B

Determining Gradient Example Calculate the average slope of a mountain trail from the 980-meter contour line to the 480-meter contour. Calculate the average slope of a mountain trail from the 980-meter contour line to the 480-meter contour. The distance between these two elevations measures 4 kilometers. The distance between these two elevations measures 4 kilometers. Gradient = Difference in elevation (m) Gradient = Difference in elevation (m) Distance between the points (km) Distance between the points (km) = 980m – 480m 4km = 500m 4km 4km = 125 m/km

Map Scale A means of showing the relationship between the size of an object indicated on a map and the actual size of the object on the ground. Definition

Scale Types Fractional scale: - is a fixed ratio between linear measurements on the map and corresponding distances on the ground. Example: 1:62,500 Graphical scale: - is simply a line or bar drawn on the map and divided into units that represent ground distances. Example: Verbal scale: - is a convenient way of stating the relationship of map distance to ground distance. Example: 1 inch equals 1 mile Miles

Legend - describe what the symbols on the map represent