The document discusses magnetic declination, which is the difference between true north and magnetic north on a compass. It provides the declination for Warrenton, Virginia in 1994 (9°54'), 1974 (7°47'), and 2009 (10°9'). It explains that declination diagrams on maps are used to convert between grid north and magnetic north readings. When navigating with a map, grid bearings are used, and when navigating on the ground, magnetic bearings from a compass are used. The document also discusses how to properly orient a map and compass for navigation.