For
anyone who spends a lot of time in the woods you need to know
how to navigate using a map and compass. It's not as easy as
you might think. Taking a bearing from the map and utilizing
the information you have gotten from the map to move across
the ground is a science that needs to be practiced. Its not
just a matter of dialing in the bearing and stepping off.
The
Norths
There
are three different types of North out there and each one has
its own use in navigating. True North is the geographic top
of the world and the North that coincides with the top of the
world is also the one that you read from your GPS if you own
one. Magnetic North is approximately 150 West of Frobisher Bay
and it moves yearly. It's also the North that your compass points
to. Grid North is the top of your map, and it is usually different
from True North by a couple of degrees depending on how far
North of the equator you are. Think of it this way. The earth
is a sphere much like an orange. In order to make a map you
need to make a two dimensional representation of something that
is three-dimensional. In order to do this you need to "spread"
the top of the map in order for it to lie flat. As it spreads
the difference between Grid North and True North becomes greater
the farther north you go. So in essence we have three different
Norths all pointing to different places and giving us differing
information. What we need is a way to figure out how to use
all the information in order to navigate with precision.

Magnetic North and lines of Declination
Declination
All
Maps have some sort of Declination or Magnetic Variation. On
a Topo map it can be found as a symbol that looks like this:

This
shows the difference between the Norths. The Star equates to
True North, The square Equates to Grid North and the Arrow equates
to Magnetic North. You can see from our example that the difference
between Grid and True North is 0° 32' and the difference
between Grid North and Magnetic North is 13°12'. This angle,
between Grid and Mag, is known as the Grid Magnetic angle and
it is the one we are concerned with when navigating from a map
to the ground. In order to get from point "A" to point
"B" we need to take a bearing from the map. All a
bearing is an angular measurement taken from one point to another
with the zero reference being north. In the case of a map that
north is Grid North. So when we take a bearing off the map we
have, in essence, a Grid Bearing. From our example we can see
that there is a difference of a little over 13° between
Grid North and Mag North, so if we took our Grid bearing and
applied it to our compass we would be out by 13° to start
with and the longer the leg we walked the greater our error
would be at our arrival point.
So we need to apply the Magnetic Declination to our compass
in order to take into account the differences between Grid and
Mag. If you remember the following little saying you cant go
wrong:
Variation
East, Magnetic Least.
Variation West, Magnetic Best.
All
that means is that if you have Easterly variation, your magnetic
bearing will be the lesser of the two bearings. How can we tell
if the variation is Easterly or Westerly? By looking at our
example. The Arrow for Mag North lies to the West of Grid North
so we have Westerly Variation. If it was on the other side we
would have Easterly variation.
So
if we take a Grid bearing from the map and we want to make it
into a Mag bearing so we can walk across the ground with precision
and the Variation is Easterly on our map then we need to subtract
the variation from the grid bearing to come up with the correct
Mag bearing. If the variation is Westerly on your map then you
need to add the variation to the Grid Bearing to come up with
the correct Mag bearing.
Now there is one last small calculation that needs to be made
in order to be precise in your navigating. The information provided
on your topo map is only accurate when the map was printed.
In order to be as precise as possible then we need to update
the information to today's values. Also included with the declination
arrows are when the measurement took place and how much it is
changing by. For example

Now
we have all the required information we need. In 1995 there
was 13°12' declination. It is now 2004, that's a difference
of 9 years. There is a change of 3.2' per year. Multiply 3.2'
by 9 years gives us 28.8 minutes of change. I round up to 29
in this case. The change is decreasing yearly so we need to
subtract our 29 minutes of change from the 13°12' that was
measured in 1995. So 13°12 minutes minus 28 minutes leaves
us with 12°44' declination. As a rule of thumb if it's below
30 minutes, which is ½ a degree then I round down. More
than 30 minutes then I round up. So in this case 12°44'
would still be 13° or no real change. You still need to
know how to do this especially if you have an older map.
So
if you remember the rules for applying the Magnetic Declination
to your compass when you are navigating with a map you cant
go wrong. Just remember that the bearing you take off your map
isn't necessarily the correct one until you convert it.