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How-To

How to Read a Topographic Map

Contour lines, scale, and the handful of patterns that turn a sheet of squiggles into terrain you can picture.

Written by William • Updated August 2026 • 7 min read

A topographic map encodes three-dimensional terrain on a flat sheet using contour lines. Once you can read the four or five common patterns, you can look at a map and picture the ground — which is what makes it a navigation tool rather than a decorative object.

  1. 1

    Contour lines and the interval

    Every point on a contour line is the same elevation. The contour interval, printed in the map legend, is the vertical distance between adjacent lines — commonly 40 feet or 20 metres. Lines close together mean steep ground; lines far apart mean gentle. Cliffs appear as lines so close they merge.

  2. 2

    Read scale and measure distance

    A 1:24,000 map means one inch equals 24,000 inches on the ground, about 2,000 feet. Use the printed scale bar rather than doing arithmetic. Remember that map distance is horizontal — a steep mile is longer to walk than a flat mile and takes considerably more time.

  3. 3

    Recognise ridges and valleys by the V

    This is the pattern that unlocks the rest. Contours crossing a drainage form a V pointing uphill, toward higher ground. Contours crossing a ridge form a V or U pointing downhill. If you can tell a ridge from a gully at a glance, you can follow terrain rather than just following a line.

  4. 4

    Spot saddles, summits, and depressions

    A summit is a small closed contour with higher ground inside. A saddle is the low point between two summits, appearing as an hourglass of contours — and saddles are usually the easiest crossings between drainages. Depressions are closed contours with small tick marks pointing inward.

  5. 5

    Estimate time, not just distance

    A common approach adds roughly half an hour per 1,000 feet of climb to your flat-ground pace. Count the contour lines your route crosses, multiply by the interval, and you have your elevation gain. This is what turns a map into a schedule.

    Trip planningTurning map reading into a day plan
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  6. 6

    Check the declination note

    Maps are drawn to true north; compasses point to magnetic north. The difference, called declination, is printed on the map and varies by location and over time. Ignoring it introduces a bearing error that compounds over distance.

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Contour Patterns

PatternWhat it means
Lines close togetherSteep ground
Lines far apartGentle ground
V pointing uphillDrainage, gully, or stream
V or U pointing downhillRidge or spur
Small closed circleSummit or high point
Hourglass between summitsSaddle — often the easiest crossing
Closed contour with tick marksDepression

Frequently Asked Questions

What map scale is best for hiking?
1:24,000 for detail on foot, which is the standard USGS quad scale. 1:50,000 and smaller cover more ground with less detail and suit route overviews.
Do I need paper maps if I have a phone?
A phone with offline maps is excellent and it depends on battery, screen, and not being dropped. A paper map and compass have no failure modes that a cold night can trigger.
How do I know if my map is current?
Check the revision date. Trails, roads, and water sources change; older quads can show trails that no longer exist and miss ones that do.