The Earth's
magnetic field is quite complicated in detail, however, much of it can
be approximated as if there was a bar magnet, with a positive (+) pole
and a negative (-) pole, at the center of the Earth -- remember it is the
electric currents in the outer core that produce the field -- but it
mimics the lines of force associated with bar magnet, which many of you
have played with in your childhood (and maybe still do on your refrigerator
door).
The north pole of the Earth's magnetic field is near the Earth's geographic north pole, which is defined by the Earth's
rotational axis -- but does NOT occupy the same, exact location -- but
it is close.
Measurements
of the Earth's magnetic field, especially information of the Earth's past
magnetic field now locked in rocks beneath the seafloor, provided critical
information in the development of the theory of plate tectonics -- we
will learn more about this later in the expedition.