It is also called magnetic variation . Magnetic declinationt is fefinedas the angle on the horizontal plane between magnetic north which is the direction the north end of a compass needle points, corresponding to the direction of the Earth's magnetic fieldlines) and and true north (the direction along a meridian towards the geographic North Pole). This angle always varies depending on position on the Earth's surface and changes with respect to time.
In using a magnet to find north, the term “declination” represents a. the angle below the horizontal of the earth’s magnetic field. b. Not given c. the angle above the horizontal of the earth’s magnetic field. d. the degree of weakness of the magnetic field. e. another term for “angle of dip”.
The magnetic bearing of line PQ is S40E and the magnetic declination is 8, 5'E what is the true bearing of the line?
10. Current magnetic declination is 03002'E and annual change is 00002' westward. If a current magnetic bearing is s 01ø22'E what was the line's magnetic bearing 50 years ago?
MN GN 15% 0°27' 267 MILS 8 MILS UTM GRID AND 1966 MAGNETIC NORTH DECLINATION AT CENTER OF SHEET 2. Declination is the angular difference between the direction to magnetic north (m. n.) and true north (indicated at the bottom of the map by a "North Star"). Remember the declination changes gradually with time. What is the declination between true north and magnetic north indicated on the 1966 map? Express your answer in degrees.
MN GN 15% 0°27' 267 MILS...
A magnetic azimuth of 290° 20' has a known declination of 15° '30 W. What is the geodetic azimuth?
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