JPRS said:
GN stands for Geographic North, not grid north. GN is the point around which the Earth rotates. It doesn't line up precisely with Polaris, the North Star. The little diagram on the map shows the variance between GN and the North Star.
This is very wrong, and Borg is correct. GN stands for grid north, not geographic north. Look at different topographic maps. Every topographic map has three different concepts of "north". True north, which points toward the Earth's rotation axis; grid north, which is parallel to the vertical edge paper on which the map is printed; and magnetic north, which is the direction in which a compass points. The question is, why is this done?
arabianights said:
when I look at large scale map such as USGS top maps, i noticed that maps' grid are not aligned with the map frame. looking at the declination diagram at the bottom of the map, there's a difference between true north and GN (Grid north)
can someone explain to me why the map grid doesn't align with True north?
The basic problem is that maps are flat while the Earth is more or less spherical. There is no perfect representation of the surface of the Earth on a flat piece of paper. Every projection involves some sort of compromise. Lines of latitude and longitude are orthogonal to one another in a Mercator projection. This projection does a nice job near the equator, but it is rather lousy more than a few degrees from the equator.
Topographic maps instead typically use a transverse Mercator projection. A transverse Mercator projection generalizes the concept of Mercator projection to some great circle other than the equator. The universal transverse Mercator maps used in topographic maps are a bit of a misnomer. The problem with any Mercator projection is that they are not "universal." A Mercator projection is rather lousy in places far from the great circle used as the basis for the projection.
The solution used in UTM projections is to use sixty different transverse Mercator projections, each centered on a line of latitude rather than the equator. The sixty different projections correspond to 6 degree wide slices of an orange. This reduces the distortions that result from using a global Mercator projection, but at the cost of having lines of latitude and longitude being curves rather than lines.
Finally, to answer the question, true north typically is not parallel to an edge of the paper on which a topographic map is printed.