ten degrees ten degrees
degree of declination (19 letters to fit in your crossword puzzle)
magnetic declination
The University of North Carolina is located in Chapel Hill, North Carolina. It begins with the letter U.
There's no physical difference, the number at the end is the PSP's region which will affect what movie UMDs you can play, and some online features such as the PSN. PSP-2000 is the Japanese regional variant, PSP-2001 is the North American.
The Tasman Sea is between Australia and New Zealand. The Thracian Sea is part of the Aegean Sea. The Timor Sea is north of Australia.
Charlotte is a city in North Carolina. Chimney Rock is a village in North Carolina.
North or south
magnetic variation
magnetic variation
Magnetic declination or variation.
True. Declination is the angular difference between true north (the direction of the North Pole) and magnetic north (the direction a compass points towards).
It is measured exactly the same in the Southern hemisphere (no difference between the two hemispheres). It is the difference between magnetic north and true north and it varies all over the globe. Magnetic declination (also called magnetic variation) is positive when magnetic north is east of true north (clockwise) and it is negative when magnetic north is west of true north (anti-clockwise).
The magnetic declination in San Diego, California is approximately 12 degrees east, which means there is a 12 degree difference between true north and magnetic north in that area.
Assuming the subject is magnetic declination the difference between the north pole and the true north pole this difference, is the magnetic declination, there is not information on what purpose it serves.
An ordinary magnetic compass points to magnetic north, not to true north. If the difference between the two directions is large and not accounted for, you can get lost.
the magnetic north pole moves while the geographic north pole stays in the same place
Geographic north is the direction towards the North Pole, while magnetic north is the direction towards the north-seeking pole of a magnet. The two points do not align perfectly due to the Earth's magnetic field, causing a discrepancy between true north and magnetic north.
There is a general geographical difference, called magnetic declination. In addition, there may be differences that arise locally, as a result of nearby objects that attract a magnet, which is called magnetic deviation. Related links are given below.
The difference is referred to as magnetic, or compass, declination.