Two Norths

There are actually two "Norths" that matter in navigation:

These two points are not in the same place. As of 2026, magnetic North is located somewhere in the Arctic Ocean, roughly 500 km south of true geographic North — and it moves every year.

What Is Magnetic Declination?

Magnetic declination (also called magnetic variation) is the angle between true North and magnetic North at a given location. This angle varies:

Real-World Examples

Let's say you're hiking in Maine, USA, where declination is approximately 14°W. If your compass says you're heading 0° (magnetic North), you're actually heading 14° east of true North. Over a 10-kilometer hike, that 14° error translates to about 2.5 km of drift — enough to miss your intended destination significantly.

Conversely, in parts of Australia, declination can be as high as 12°E — meaning compass North is east of true North, and the correction goes the other way.

Fortunately, in most of central Europe, East Africa, and Southeast Asia, declination is relatively small (under 5°) — small enough that casual navigation can ignore it entirely.

Does Your Phone Automatically Correct for Declination?

It depends on the app and settings:

Practical note: For most everyday uses — finding Qibla, orienting a room, casual navigation — the difference between magnetic and true North is negligible. For serious surveying, land navigation, or marine piloting, always account for declination.

How to Find Your Local Declination

NOAA (National Oceanic and Atmospheric Administration) maintains a free declination calculator at ngdc.noaa.gov. Enter your location and get the current magnetic declination value with its annual rate of change.

How to Apply Declination Manually

If you're using a compass that shows magnetic North and need true North:

Memory aid: "Declination East, compass least (subtract). Declination West, compass best (add)." This mnemonic is used in traditional compass navigation courses worldwide.

The Moving Magnetic Pole

Earth's magnetic north pole is accelerating. It moved about 10 km/year in the mid-20th century; by the 2010s it was moving 50+ km/year, drifting generally toward Siberia. Scientists believe this reflects convective flows in Earth's liquid outer core. This drift is why magnetic declination values change over time, and why navigation charts carry a "date of magnetic information" note.

For context: if you used a 1980 nautical chart without updating the magnetic variation correction, you could introduce a navigation error of several degrees — potentially dangerous in coastal waters with rocks and shoals.