1 / 63

Understanding Ordnance Survey Maps and Slope Gradients

Learn land features, contour lines, slope gradients, and route planning on Ordnance Survey maps. Understand how to interpret relief features and calculate slopes for accurate route navigation.

darlenew
Download Presentation

Understanding Ordnance Survey Maps and Slope Gradients

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. MAR-2-119R7 Map Information Part 2 First Class Training

  2. Objectives • Describe the main land features found on Ordnance Survey maps when planning routes • Use contour lines on Ordnance Survey maps to plan routes • Explain why land features shown on Ordnance Survey maps are important for planning routes • Assess the slope gradient when planning routes • Analyse sections of land profile by projection from map contour lines to get accurately from one point to the next • Plan accurate routes using the features of an Ordnance Survey map

  3. Relief • Features such as hills and valleys • Includes both height and shape • Hard to represent on a two-dimensional map • Shown by: • Spot heights and trig points • Contour lines

  4. Height • It is important to understand the units used • OS maps are measured in metres

  5. Shape • Shape can be shown by: • Hachures

  6. UPHILL

  7. Shape • Shape can be shown by: • Hachures • Thickness and closeness shows gradient • Mostly used to show cuttings and embankments

  8. Shape • Shape can be shown by: • Hachures • Shading – not used on OS maps • Contour lines

  9. 65 UPHILL 60 55 50 45

  10. Shape • Shape can be shown by: • Hachures • Shading – not used on OS maps • Contour lines • Link points of equal height • Numbers always point up-hill • Thicker line at 50m intervals • Intervals • 1:25,000 – 5m • 1:50,000 – 10m

  11. 68

  12. 50 68 65 60 55 50

  13. Understanding Slopes • The closer together contour lines are, the steeper the slope • Remember to work out which way the slope goes! • Use the numbers • Slopes go uphill from small to larger numbers • Numbers have their tops uphill from the bottoms • Features give clues as well – eg lakes will generally form at the base of slopes rather than the top

  14. Shallower slope 65 65 60 60 55 55 Steeper slope 50 50 45 45

  15. Understanding Slopes • A numerical figure can be calculated for how steep a slope is – the gradient • Expressed as a ratio: The smaller the second number, the steeper the slope

  16. Understanding Slopes • 1:10 • For every metre climbed (vertical distance), the slope covers 10 metres horizontal distance. 1 10

  17. Understanding Slopes • A numerical figure can be calculated for how steep a slope is – the gradient • Expressed as a ratio: The smaller the second number, the steeper the slope • To keep ratios understandable, the first number should always be a 1. This can be done by reducing the ratio (just like reducing a fraction).

  18. Understanding Slopes • 2:10 • For every 2 metres of vertical distance the slope covers 10 metres horizontal distance. • 1:5 • For every metre of vertical distance the slope covers 5 metres horizontal distance. 2 1 10 5

  19. Understanding Slopes • Calculating the gradient: • Count the gaps between the contour lines

  20. Understanding Slopes 1 2 3 4 65 60 55 50 45

  21. Understanding Slopes • Calculating the gradient: • Count the gaps between the contour lines • Measure the horizontal distance

  22. Understanding Slopes 65 60 4mm 55 50 45

  23. Understanding Slopes • Calculating the gradient: • Count the gaps between the contour lines • Measure the horizontal distance • Convert both to metres (using the scale) • 4 gaps x 5 metres = 20 m vertical • 4mm x 25,000 • 4m x 25m = 100 m horizontal • This gives 20:100

  24. Understanding Slopes 20 : 100 2 : 10 1 : 5 10 2 = 5

  25. Understanding Slopes • If the gradient doesn’t easily reduce, then reduce the second figure to the nearest integer (whole number)

  26. Understanding Slopes 23 : 128 Remainder is more than half of 23, so round up 1 : 6 128 23 = 5 r15

  27. Understanding Slopes Or…

  28. Understanding Slopes 23 : 128 23 ≈ 20 128 ≈ 120 20 : 120 2 : 12 1 : 6

  29. Understanding Slopes • If the gradient doesn’t easily reduce, then reduce the second figure to the nearest integer (whole number) • In some cases, the second number is 1 and the first number is greater than one – this means that the slope is steeper than 45 degrees

  30. Understanding Slopes • 2:1 • For every metre of horizontal distance, the slope rises 2 metres vertical distance. 2 1

  31. Understanding Slopes • If the gradient doesn’t easily reduce, then reduce the second figure to the nearest integer (whole number) • In some cases, the second number is 1 and the first number is greater than one – this means that the slope is steeper than 45 degrees • This can also be expressed as a ratio with a 1 followed by a fraction, eg the 2 : 1 slope can also be expressed as 1 : 0.5.

  32. Understanding Slopes • 1 : 0.5 • For every metre of vertical distance, the slope rises half a metre of vertical distance. 1 0.5

  33. Understanding Slopes • Convex – steeper at the bottom than the top • Concave – steeper at the top than at the bottom • Some parts of a convex slope may not be visible from others • The entirety of a concave slope can be seen from any part of the slope Concave slope Convex slope

  34. Convex slope 50 45 55 60 65 70 75 80

  35. Concave slope 50 45 55 60 65 70 75 80

  36. Undulation • Only features larger than the contour interval will show on contours – but the land between contours could undulate significantly • This is the reason why hachures are used for notable features too small to show with contours 15 15 10 15 10

  37. Land Features - Ridge • A long narrow stretch of elevated ground

  38. 823

  39. 780 785 790 795 800 805 810 RIDGE 815 820 820 823 815 810 805 800 795 790 785 780 775 770 765

  40. Land Features - Ridge • A long narrow stretch of elevated ground • If between two peaks, it is known as a col or a saddle

  41. 847

  42. COL (SADDLE) 847

  43. Land Features - Valley • A valley is the inverse of a ridge

  44. v VALLEY

  45. Land Features – Spur • A spur can be thought of as a ridge running perpendicular to a slope. • It is a bit like half a col: SPUR COL

  46. 847

  47. 847 SPUR

More Related