- 2068 Bhadra · 7 marks
Contour gradient and characteristics
Short answer
Contour gradient is a line of uniform slope that cuts successive contours at equal horizontal distances (gradient = contour interval / horizontal equivalent). Characteristics: contours are closed curves of equal elevation; they never cross except at overhanging cliffs; spacing indicates slope; they bend upstream at valleys and downstream at ridges; concentric contours with higher inside show a hill, lower inside a depression.
What is contour gradient? Write characteristics of contours with suitable sketches.
Contour gradient
Contour gradient is the line of constant slope (uniform gradient) that cuts the contours at the same horizontal equivalent. It is laid on the ground to fix the route of a road, railway, canal or pipe line. The gradient = CI / HE = 1 in (HE/CI).
Characteristics of contours
- Contours are closed curves. Every contour must close on itself, either inside the map or outside it. It cannot start or end abruptly.
- All points on a contour have the same elevation.
- Contours never cross each other, except at an overhanging cliff or a cave. Two contours of different elevation cannot meet or cross because one point cannot have two elevations.
- Contours of different elevations do not unite to form one line, except at a vertical cliff, where they coincide and appear as one line.
- Closely spaced contours indicate a steep slope; widely spaced contours indicate a gentle slope. Equally spaced contours indicate a uniform slope, and straight, equal and parallel contours indicate an inclined plane.
- Contours cross ridge lines and valley lines at right angles. The direction of the steepest slope is at right angles to the contour.
- A set of concentric closed contours with the higher value inside represents a hill; with the lower value inside it represents a depression (pond or pit).
- Contours bend as V or U shapes across a ridge and a valley. For a ridge (spur) the bend of the contour points towards the lower ground; for a valley the bend points towards the higher ground.
- Contours of the same elevation may reappear on the other side of a ridge or a valley, so one contour value can appear twice on a map.
- A contour cannot lie between two contours of higher (or lower) values unless it closes on itself (hill or depression).
- A saddle (col) is shown by the closed contours of two hills on opposite sides, with lower ground (valleys) on the other two sides; the saddle point lies at the neck between the hills.
HILL DEPRESSION
.--100--. .--100--.
/ .-110-. \ / .--90-. \
| / (120) \ | | / (80) \ |
\ '-----' / \ '-----' /
'-------' '-------'
RL rises to the centre RL falls to the centre
RIDGE (v points downhill) VALLEY (^ points uphill)
130 \ / 120 /\
\ / / \
120 \ / 110 / \
\_/ / \
110 \ / 100 / \
\___/
high ground at top high ground at top
Steep slope Gentle slope Uniform slope
(close) (wide apart) (equal spacing)
----100 ----100 ----100
----101 ----101
----102 ----102
----103 ----101 ----103
✓ Answer checked by Claude Opus 5.5 (high effort)
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