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Valley curve or sag curves are vertical curves with convexity downwards.
They are formed when two gradients meet as illustrated in figure
1 in any of the following four ways:
Figure 1:
Types of valley curve
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- when a descending gradient meets another descending gradient
[figure 1a].
- when a descending gradient meets a flat gradient
[figure 1b].
- when a descending gradient meets an ascending gradient
[figure 1c].
- when an ascending gradient meets another ascending gradient
[figure 1d].
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