Magnetic Declination                   Troop

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From Kjetil Kjernsmo's illustrated guide ...

Magnetic Declination - Understanding It

There is something called magnetic declination. You see, the compass is pointing towards the magnetic northpole, and the map is pointing toward s the geographic northpole, and that is not the same place. each of the northsTo make things even more complicated, there is on most hiking-maps something (that is very useful) called the UTM-grid. This grid doesn't have a real north pole, but in most cases, the lines are not too far away from the other norths. Since this grid covers the map, it is convenient to use as meridians.

On most orienteering maps (newer than the early 70's), this is corrected, so you won't have to worry about it. But on topographic maps, this is a problem.

First, you'll have to know how large the declination is, in degrees. This depends on where on the earth you are. So you will have to find out before you leave home. Or somewhere on the map, it says something about it. One thing you have to remember in some areas, the declination changes significantly, so you'll need to know what it is this year.

If you are using a map with a "UTM-grid", you want to know how this grid differs from the magnetic pole.

 

the directionsThe declination is given as e.g. "15 degrees east". When you look at the figure, you can pretend that plus is to the right, or east, and minus is to the left and west. Like a curved row of numbers. So when something is more than zero you'll subtract to get it back to zero. And if it is less, you'll add. So in this case you'll subtract 15 degrees to the azimuth, by turning the compass housing, according to the numbers on the housing. Now, finally, the direction of travel-arrow points in the direction you want to go. Again, be careful to aim at some distant object and off you go.

You may not need to find the declination before you leave home, actually. There is a fast and pretty good method to find the declination wherever you are. This method has also the advantage that corrects for local conditions that may be present. This is what you do:

  1. Determine by map inspection the grid azimuth from your location to a know, visible, distant point. The further away, the more accurate it gets. This means you have to know where you are, and be pretty sure about one other feature in the terrain.
  2. Sight on that distant point with the compass and note the magnetic azimuth. You do that by turning the compass housing so that it is aligned with the needle. You may now read the number from the housing where it meets the base of the direction of travel-arrow.
  3. Compare the two azimuths. The difference is the declination.
  4. Update as necessary. You shouldn't need to do this very often, unless you travel in a terrain with lots of mineral deposits.