noun
1. : one of the poles of a magnet
2. : either of two nonstationary regions on the earth which sometimes move many miles in a day, toward which the isogonic lines converge, and at which the dip is plus or minus 90 degrees
noun
1. : one of the poles of a magnet
2. : either of two nonstationary regions on the earth which sometimes move many miles in a day, toward which the isogonic lines converge, and at which the dip is plus or minus 90 degrees
Webster's New International English Dictionary. Новый международный словарь английского языка Webster. 2012