A layered paper topographic model of hills and a river valley showing contour lines

Topographic maps appear throughout Programming & Analysis (PA) and Project Planning & Design (PPD). A question might ask where water will collect, which part of a site is flattest, where a building or parking lot should go, or how much a path rises. Almost all of them depend on reading the contours correctly — and a handful of rules does most of the work.

Rule 1: each line joins points of equal elevation

A contour line connects every point on the ground at one elevation. Walk along a contour and you never go up or down. Two consequences follow:

  • Contour lines never cross (one point can’t have two elevations) and never split.
  • Water flows perpendicular to the contours, from higher lines toward lower ones — it never flows along a contour, because along a contour there is no slope.

Each map has a contour interval, the elevation difference between neighboring lines — for example, 1 ft, 2 ft or 5 ft. Labels on some lines (often every fifth, drawn heavier) tell you which direction is up.

Rule 2: spacing tells you the slope

The closer the contours, the steeper the ground. To put a number on it:

slope = vertical rise ÷ horizontal distance

With a 2 ft contour interval:

  • lines 40 ft apart → 2 ÷ 40 = 5%
  • lines 20 ft apart → 2 ÷ 20 = 10%
  • lines 10 ft apart → 2 ÷ 10 = 20%

Evenly spaced lines mean a uniform slope. Lines that are close together at the top of a hill and spread out toward the bottom describe a concave slope; the reverse describes a convex one.

Rule 3: the V-rule — valleys and ridges

Where contours cross a stream, swale or valley, they bend into a V that points uphill, toward higher elevation. Where they cross a ridge or spur, the V points downhill.

The easiest way to remember it: water carves the ground, so contours bend back upstream to find the same elevation on both sides of the valley.

Putting it together: a site question

Suppose a site slopes down from north to south, with contours at a 2 ft interval. Halfway across, the lines form Vs pointing north. Here’s how to read it:

  1. Find "up." The labels increase toward the north, so north is uphill.
  2. Find the drainage. The Vs point north — uphill — so they mark a valley. Surface water from both sides will gather there and run south.
  3. Find the buildable ground. Away from the valley, where the contours are widely spaced, the ground is flattest — the natural place for a building pad or parking.
  4. Check the consequences. Placing a building across the valley would block natural drainage; you would need to redirect water around or under it.

Contours in grading plans

On grading plans, existing contours are usually drawn dashed and proposed contours solid. Where a proposed line departs from the existing one, the ground is being changed: a proposed contour moved downhill from its existing position means fill has been added there; moved uphill means cut.

Grading questions often ask you to keep water moving away from a building. The test is simple: right next to the building, the proposed contours should show ground falling away from the walls, not toward them.

Practice routine

  1. Take any site plan and mark north/uphill first, every time.
  2. Draw arrows perpendicular to the contours to show where water goes.
  3. Calculate the slope at two or three points using the interval and the scale.
  4. Circle the valleys and ridges using the V-rule, then check them against the labels.

The PA exam guide and the PPD exam guide show where site analysis fits within each division.