What Is Magnetic Dip?
Answers
Answer :-
The magnetic dip is defined as the angle made with the horizontal by the earth’s magnetic field lines. It is also known as dip angle or magnetic inclination and was discovered by Georg Hartmann in the year 1544. When the inclination is positive it indicates that the earth’s magnetic lines are pointing downward in the northern hemisphere and when the inclination is negative it indicates that the earth’s magnetic lines are pointing upward in the southern hemisphere.
In the year 1581 Robert Norman discovered a dip circle which is a method used to measure the dip angle. The other terms used are isoclinic lines (when the contour lines are equal at the earth’s surface) and aclinic lines (when the locus of the points are having zero dip).
Explanation:
Magnetic dip, dip angle, or magnetic inclination is the angle made with the horizontal by the Earth's magnetic field lines. This angle varies at different points on the Earth's surface. ... The value can be measured more reliably with a special instrument typically known as a dip circle.
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