Contours and its use

What are contours?
A contour is a line on a map connecting all places of equal height above sea level. When you interpret contour lines you are able to get the size and shape of highlands and lowlands. Contour lines never cross each other because no one point can be at two different heights above the Mean Seal Level (M.S.L).
a)      On very steep slopes they are close to each other but they cannot cross each other.
b)      Contours are drawn in regular steps measured vertically from M.S.L.
c)      These steps are called Vertical Interval (V. I) such as 100, 150 or 200 metres.
d)     The V.I is normally kept constant on a map and it is indicated in the margin of the map.
e)      It is common to thicken the contour lines at a given interval in order to make them easily identifiable.
f)       In many cases they are coloured in brown, orange and red.
g)      Contour lines are numbered along them to indicate their height above M.S.L. in such a way that higher ground lies above the figures.
h)      From the numbering of contours you can determine the direction of the slope and the height of the numbered contour lines correctly.
Some Facts about Contour Lines
                       i.            Contour lines close or join around hills, basins and depressions.
                     ii.            In hills the higher contours are in the middle.
                   iii.            Contour lines never cross each other.
                   iv.            Contour lines form a V-shape pointing upstream to denote a valley and a 
                     v.            V pointing down to denote a spur.
                   vi.            In contour maps all contour lines close or extend to the map edge.

Land Forms on Contour Maps
Highland landforms:
These include:-,
                       i.            Plateaus
                     ii.             hills,
                   iii.            ridges,
                   iv.            spurs,
                     v.            slopes,
                   vi.            scarps,
                 vii.            passes,
               viii.            saddles and
                   ix.            Watersheds.

Lowland landforms:
These include gorges, levees, deltas, flood plains, and V-shaped valleys.

Coastline landforms:
They include:,
                       i.            estuaries,
                     ii.            cliffs and corals,
                   iii.            fringed coastlines.
                   iv.            Since you have already learnt how to represent these features using contour lines in your O-level secondary education we will only remind ourselves how to draw a cross section and calculate the vertical exaggeration and gradient.

Cross Section or Profile
                       i.            Maps show relief in plan.
                     ii.            It is important to visualise the appearance of the features as they are seen from the ground.
                   iii.            Constructing relief sections helps to do this.

Steps considered in relief construction
The following are steps to be followed when constructing a relief section (cross section).
                       i.            Identify the two end points of the required section on a map.
                     ii.            Note their positions and heights and the vertical Interval.
                   iii.            Mark them as A and B and join them with a pencil.
                   iv.            Place the straight edge of a plain paper along the drawn line and mark the end points A and B.
                     v.            Mark along the edge of this paper, the positions and heights of contours, water features and important places that cut the line.

  Remove the paper from the map and place it where you intend to draw the cross section. The width of the cross section will be the distance between A and B. Draw a line equal to the width.
  Find the appropriate vertical scale to show the heights of contours such as 1cm to 100m.
  Construct a frame for the relief-section by drawing perpendicular lines from A to B and divide the heights into equal parts according to the vertical scale you have chosen.
  Place the marked paper along the base line so that AB on the paper lies on AB on the framework.
  Mark each contour line along the horizontal line and proceed with others according to their heights.
  Connect all the points with a pencil. You should smoothen hills and valleys with a smooth curve.
  Mark and label the required information. Indicate the North; add a title to the cross section, as well as the vertical and horizontal scale.

The point to note
The horizontal scale is the map scale. The vertical scale is usually exaggerated

The Vertical Exaggeration
                       i.            This is the amount or number of times by which the vertical scale or height is larger than the horizontal scale or distance.
                     ii.            This relationship is important as it determines the shape and size of features shown such that they are not too small or too large.
                   iii.            If the map scale is 1:50,000 and the vertical scale is 1 cm to 100m,