Measuring the Earths Dimensions

Slides:



Advertisements
Similar presentations
Name ______________________________________________ Date _______________ Period ________ M IDTERM R EVIEW S HEET Directions: This sheet is provided to.
Advertisements

Chapter 3 Models of the Earth.
Mapping Our World Goals: Differentiate between latitude and longitude.
Topic II: Measuring the Earth
Mapping.
Chapter 2 Measuring Earth
Topographic Maps.
Topic 2 A look at the Earth’s shape, coordinate systems, topographic maps, and data field analysis.
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.
Coordinate System Unit 1: Mapping the Earth
Earth is extremely round/spherical and smooth.
Models and Dimensions of Earth
Latitude-Longitude System –
Topographic Maps. Contour lines A line which connects points of equal elevation. Index Contours: Thick contour lines which have the elevation written.
Chapter 2: Mapping Our World BIG Idea: Earth Scientists use mapping technologies to investigate and describe the world.
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.
Chapter 3 Section 1- Finding Locations on Earth
The Earth © Lisa Michalek.
Chapter 2-Maps as Models of the Earth By Samantha Pereira.
Mrs. Degl1 It appears that Earth is a perfect circle, however, it is not!!!!! It is really an OBLATE SPHEROID. What does that mean?????????
MAPPING OUR WORLD. MAPPING Cartography- Cartography- science of map makingscience of map making.
Isolines: contour lines on an elevation map Isotherms: contour lines on a temperature map Isobars: contour lines on an air pressure.
Modeling the Earth Topic 2 Earth Science Ms. Cooke
How are Earth’s surface features measured and modeled?
Measuring the Earth  Evidence for Earth’s shape  Ships appear to sink as they go over the horizon.  The highest part of the ship is the last to go out.
Cartography Study of Mapmaking.
Measuring Earth Midterm Review Topics: Earth’s true shape & evidence Positions on Earth (Latitude, Longitude, Angle of Polaris) Time Zones.
Unit 2 Measuring the Earth Mapping. Size and Shape Almost a perfect sphere- slight flattening in the polar regions and a slight bulging at the equatorial.
Aim: How do we know the true shape of Earth? Do Now: Describe the shape of Earth using your own terms.
Model = anything that represents the properties of an object Physical Types of models: Globes Mathematical Mental Mechanical Graphic Equations Water Molecule.
Longitude & latitude Time.. SHAPE Shape – The Earth is not a perfect sphere. The Earth is an oblate spheroid. –This means it is slightly flattened at.
Topic 2 Earth’s Dimensions Earth’s shape Oblate sphere Slight bulge in the middle Due to the rotation of the earth.
 Cartography – science of mapmaking  Equator circles Earth halfway between the north and south poles ◦ Separates Earth into 2 equal halves (hemispheres)
Unit Two Measuring The Earth I. The Earth’s Shape A. Evidence the earth is round: Ships gradually disappear over the horizon from the bottom up when.
Topographic Maps Latitude Longitude 3-D in 2-D Lines of Contour.
Chapter two Review Game
Topic 2: MODEL OF EARTH.
Unit 1 Measuring the Earth
Chapter 2 Measuring Earth
Mapping.
UNIT 4: MAPPING THE EARTH
Models of the Earth.
Earth Science Regents Review
Unit 1 Measuring the Earth
The Earth © Lisa Michalek.
Aim: How can I prepare for my Regents exam?
نقشه های توپوگرافی مهدی کرد.
Measuring Earth Unit 2 ©Mark Place,
Measuring Earth Unit 2 ©Mark Place,
Earth's Dimensions Profiles Topographic Maps Latitude Longitude
Landscapes/Topography/ Measurement of Earth
Chapter 1: Maps as Models of the Earth
Coordinate System Unit 1: Mapping the Earth
Field Maps Aim: What are fields?.
Topic II Measuring Earth.
Topographic Maps.
Question Explanation Latitude = 45o N Longitude = 75o W
Unit 1 Structure of the Earth
Measuring Earth: Earth’s Size and Shape
Mapping.
Earth Science Ch. 1 Mapping the Earth.
Mapping Our World.
Jeopardy Final Jeopardy Polaris Profiles Latitude/long $100 $100 $100
Mapping.
Models of the Earth Earth Science Chapter 3.
After School Review Commack High School
Mapping Earth Do Now: Example: Hills
Presentation transcript:

Measuring the Earths Dimensions Model of the Earth A model is anything that represents the properties of an object or system. 1. Physical & Mechanical 2.  Mental 3.  Mathematical 4.  Graphic Models

II. The shape of the earth A. Observations that the earth is curved. 1. Ships at Sea… 2. Eclipses… 3.  Photographs from space are the best examples proving the earth is round.  

2. Gravity meters tell us so… The earth is an oblate spheroid or a NEARLY PERFECT CIRCLE B. The circumference measured between the poles & the equator are different. 1. Slightly flat at the poles and bulging at the equator 2. Gravity meters tell us so… Gravity Stronger at the poles. Equatorial Diameter =12,756 km Polar Diameter = 12,714 km

Horizon: is where the sky touches the earth. C. Observations of Polaris lead to the conclusion that the earth is round. Parallelism: The north pole points to Polaris. The Altitude of Polaris Equals Your Latitude Altitude: is an angle measured from the horizon. Horizon: is where the sky touches the earth. Zenith: straight above your head.

Altitude of Polaris is Equal To Your Latitude = 42  North Latitude

At the equator your altitude to Polaris is 0  In New York the Average Altitude is Between 41  & 45  North

To find the North Star use the Big Dipper The 2 Pointer Stars Point to Polaris

Finding your way around…. …using Polaris

III. Locating Positions on the Earth A. Coordinate systems are used to locate points on a surface. 1. On a curved surface, such as earth, we use latitude & longitude. Both reference points are found by using stars a.    The equator is the starting point for latitude. Measured 90° North or South Latitude lines are parallel to one another & run like latter rungs.

B. The prime meridian is used for the starting point of longitude lines. Marked in 15° increments as the sun moves across the sky. Run 180 ° East or West to the International Dateline. Each meridian runs the long way meeting at the poles.

C. Latitude is reported first then Longitude 45° North by 30° West ° Degrees `Minutes ``Seconds

D. There are 24 Time Zones The International Date Line @ 180 Separates One Day from the Next. The earth rotates on its axis 15  / hour Time can be tracked by counting the number of hours away from the prime meridian.

IV. Field Maps Field Quantities A field is a region of space that has a measurable value at every location. Scalar Fields: magnitude measurements (Temperature) Vector Fields: magnitude and direction (wind speed) Iso-lines connect points of equal value. 4. Iso-surface is a three dimensional surface in which every point has an equal value.

A. Creating an Isotherm field map Connect temperature points of equal value. Identify Heat Sources and Sinks Heat Sink Heat Source

Topographic Maps gives a two dimensional view of the land. B. Topographic Maps are models showing the elevation, shape, and steepness of the land surface. Contour lines connect points of equal elevation. Topographic Maps gives a two dimensional view of the land. Show Relief or Elevation above sea level. 2000 ft. Contour line

Compass Direction & Magnetic Declination. Contour Interval 2. All topographic maps are referred to as quadrangles or contour maps. ¤ A quadrangle is a 4 cornered map. Scale showing the ratio of actual distance to map distance Compass Direction & Magnetic Declination. Contour Interval

3. Contour Interval is the change in elevation from one contour to the next. Closely Spaced Contours indicate a steep cliff gradient. A hill top has closed looped contour lines Index Contour Lines are thick lines. V-Shaped contours indicate a stream valley & point uphill

A profile….. Note the closed contours and “u” shaped valley.

4. Topographic Profiles can be drawn using contour points. A profile shows the cross sectional view of the landscape

5. Calculating a gradient or the slope of the land. ESRT pg 1 What is the gradient of the hill below the ski lift? G = Change in Field Value Distance G = 1400 ft – 450 ft 0.8 miles G = 950 ft G = 1187.5 ft/mile

Answer the following. What is the contour interval? What is the highest contour elevation? What compass direction is Campbell River from? What do closed contour lines indicate? What do closely packed contours indicate along side a hill? Which compass side of Deer Mountain is the steepest? What is the highest possible elevation for Berry Mountain? Calculate a gradient for line 1 use your ESRT ruler to estimate distances. 9. Calculate a gradient for line 2 use your ESRT ruler to estimate distances. Answer the following. Line 1 Line 2 C.I. = 100 Meters