The Earth's magnetic field is generated in the mobile outer core composed of liquid iron and nickel. The source of the magnetic field cannot be permanently magnetized material, because the interior of the Earth is too hot for any material to retain its magnetism. This means that the Earth's magnetism must be generated electromagnetically. The Earth behaves much like that of a bar magnet. Think of the Earth as having a giant bar magnet passing from one pole to the other pole through its center.
Magnetism of an iron magnet is caused by electric currents associated with the spinning motion of atomic electrons. If the magnetometer indicates a large magnetic field for Eros then it could be assumed that there is a current circulating Eros causing the field. To get a general idea of what a magnetic field looks like, think of iron filings sprinkled around a bar magnet. The iron filings would take on the appearance of the characteristic dipole pattern. A magnetic field might exist in the space around a magnet, similar to the way an electric field surrounds a charged body.
![[Magnetometer sensor and electronics]](mag.jpg)
![[Magnetometer antenna dish assembly]](mag_dish.jpg)
Lesson Plan on
Magnetism
Magnetometer Overview on NEAR Web Server
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Contact Steve Bowser (slbowser@umd5.umd.edu)
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