Let the magnetic field on the earth be modelled by that of a point magnetic dipole at the center of the earth. The angle of dip at a point on the geographical equator:
(a) | is always zero |
(b) | can be zero at specific points |
(c) | can be positive or negative |
(d) | is bounded |
1. (a, b, c)
2. (a, c, d)
3. (b, c, d)
4. (c, d)
© 2024 GoodEd Technologies Pvt. Ltd.