1. Modeling the Earth Topic 2 Earth Science Ms. Cooke 2015-2016

2. Part 1 – What is a map? A map is a representation of an area or location on Earth. A map is a pf the Earth, or an object. Parts of a Map: – A is someone who makes maps.

4. The Coordinate System To locate places on the Earth, a grid system has been developed that assigns to numbers to each location. - The angular distance north or south of the Equator (). –Determined by the angle of the North Star () above the horizon in the Northern Hemisphere. –Angles of latitude are also called Why?

5. Latitude

6. Angle of Polaris Latitude can be determined by fins=ding above the horizon. Use and astrolabe to find angle.

7. Latitude

8. Hemispheres by Latitude

9. Longitude Longitude – Based on the apparent movement of the. (Time) Measures the Angular Distance or of the (). Angles of Longitude go from to. –

10. Longitude

11. Hemispheres by Longitude

12. Hemispheres

13. Coordinate Practice

14. Time Zones Time zones are based on Rules – – –If the time difference between New York City and London, England (0°) is 5 hours, What is the Longitude of NYC?

15. World Time Zones

16. US Time Zones

17. Coordinate Precision Every of latitude is of the Earth’s Circumference =. Each consist of (‘). –1 minute = –Each consists of (“). 1 second =

18. Mapping Technology GPS – –Uses 29 satellites that transmit microwave signals to receivers on the ground (GPS Unit). –GPS Information

19. Mapping Technology GIS - technology and satellites have made it easier to integrate valuable information into very specialized maps. Anyone can access mountains of data (using the internet) to create maps of almost anything.

20. GIS Imagery GIS has almost infinite possibilities GIS changes the way we can view data and study problems Business, government agencies, scientists, & ordinary people are using GIS everyday. »http://maps2.cattco.org/parcel/http://maps2.cattco.org/parcel/

21. Part 2 Modeling the Earth in 3D TOPOGRAPHC MAPS

22. Topography Topography – The shape of features of an object (such as the Earth)

24. Fields and Isolines A is a in which a similar quantity can be measured at every point or location. connect points of. on a field map (EVERY POINT ON THE LINE IS THE SAME) No isoline can ever cross… why? Types –

25. Topographic Maps Two dimensional model of the Earth’s surface (represents 3-D world) Topographic maps are also known as contour maps. Contour lines – type of isoline used to show elevation, or height above sea level.

29. Contour Map “Real World”

30. Index Contours & Contour Intervals Index Contour – Usually every 5 th line is printed darker and has an elevation printed on it. Contour Interval – the distance between each contour line.

32. Contour Interval Contour IntervalContour Interval – difference in elevation between each line. MUST be equal spacing. Contour interval = 20 feet 520 540 560 580

33. Finding Elevations 1 st – Find the contour interval of the map1 st – Find the contour interval of the map 2 nd – Find the indec contours near the location2 nd – Find the indec contours near the location 3 rd – If the location id on s line, you know the elevation. If it is between – estimate!3 rd – If the location id on s line, you know the elevation. If it is between – estimate! Contour Interval = 20 ft

34. Rules for Contours 1.Contour lines never cross

35. Rules for Contours 2. Contours form closed loops (even if not shown of the map.

36. Rules for Contours 3. Contours bend upstream (uphill) when crossing a stream.

38. Rules for Contours 4.The maximum possible elevation for a hill is “1” less than what the next contour “should” be. The highest possible elevation of the hill is just below the value of the next line that is not shown 50 60 70 80 90

39. 239 399 179

40. Rules for Contours 5. The lowest possible elevation for a depression is “1” more than what the next contour “should” be. The lowest possible elevation of a depression is just above the value of the next line that is not shown 50 90 80 70 60 51

41. Rules for Contours 1.Contour lines never cross. 2.Contours form closed loops (even if not shown of the map. 3.Contours bend upstream (uphill) when crossing a stream. 4.The maximum possible elevation for a hill is “1” less than what the next contour “should” be. 5.The lowest possible elevation for a depression is “1” more than what the next contour “should” be.

42. Steepness Steeper Slope (Gradient) – contour lines are closer together.

44. Steepness Gradual/Gentle Slope (Gradient) – contour lines are farther apart.

45. Steepness Steeper Slope (Gradient) – contour lines are closer together. Gradual/Gentle Slope (Gradient) – contour lines are farther apart.

47. A B

48. Hills and Valleys Hills have contour lines that form smaller and smaller concentric circular shapes towards a central point Valleys are shown by the “V” shapes in the contour lines, between hills.

49. Depressions Contour lines which show a depression, crater, or sinkhole on a map. Drops in elevation towards a central point. Shown by dashed lines (hachure marks) on the inside of a contour line The elevation of the first depression contour is the same as the lowest regular contour near it.

50. Determining Direction Direction Is determined by the. –Often, the top of the map is - Due to the Earht’s magnetic field, a compass does not point, instead it points to the.

51. Magnetic Declination On the map you will see – 1.States the magnetic declination at the time the map was made. 2.Varies by location and over time. 3.Today our magnetic declination is about 11 degrees. 4.What is the magnetic declination shown here?

52. Finding Distance Use the scale on the map to find the distance between two points.

53. Finding Distance Use the scale on the map to find the distance between two points.

54. Finding Distance Use the scale on the map to find the distance between two points.

55. Finding Distance Use the scale on the map to find the distance between two points.

56. Relief The difference in elevation between the highest and lowest points. –What is the relief?

57. Relief Calculate the relief between points A and B

58. Calculating Gradient or Slope The slope between any two points on a hill Gradient = Change in Field Value Distance

59. Calculating Gradient or Slope Gradient = Change in Field Value Distance

60. Gradient A trail is four miles long as measured by the scale on a map. The beginning of the trail is at the 1,060 ft contour line and the end of the trail is at the 960 ft contour line. Calculate the gradient of the trail. Gradient = = 1060 ft – 960 ft 4 miles 25.0 ft/mi

61. Topographic Profile The side view