<unk>  is the "normal" form of magnetism with which most people are familiar, as exhibited in horseshoe magnets and refrigerator magnets. It is responsible for most of the magnetic behavior encountered in everyday life.  The attraction between a magnet and ferromagnetic material is "the quality of magnetism first apparent to the ancient world, and to us today," according to a classic text on<unk> .<unk>  is defined as the phenomenon by which materials, such as iron, in an external magnetic field become magnetized and remain magnetized for a period after the material is no longer in the field.
All permanent magnets are either ferromagnetic or ferrimagnetic, as are the metals that are noticeably attracted to them.
Historically, the term ferromagnet was used for any material that could exhibit spontaneous magnetization: a net magnetic moment in the absence of an external magnetic field.  This general definition is still in common use.  More recently, however, different classes of spontaneous magnetisation have been identified when there is more than one magnetic ion per primitive cell of the material, leading to a stricter definition of<unk> " that is often used to distinguish it from<unk> .  In particular, a material is "ferromagnetic" in this narrower sense only if all of its magnetic ions add a positive contribution to the net magnetization.  If some of the magnetic ions subtract from the net magnetization (if they are partially anti-aligned), then the material is "ferrimagnetic".  If the ions anti-align completely so as to have zero net magnetization, despite the magnetic ordering, then it is an antiferromagnet.  All of these alignment effects only occur at temperatures below a certain critical temperature, called the Curie temperature (for ferromagnets and ferrimagnets) or the Néel temperature (for antiferromagnets).
Ferromagnetism
Superparamagnetism
Paramagnetism
Superdiamagnetism
Mottling
Stripping
Pica
Thumbprinting