Brief: All ferromagnets have a maximum temperature where the ferromagnetic property disappears as a result of thermal agitation. This temperature is called the Curie temperature.

Ferromagnetism is a phenomenon by which a material can exhibit a spontaneous magnetization, and is one of the strongest forms of magnetism. It is responsible for most of the magnetic behavior encountered in everyday life and (including the special case of ferrimagnetism, below) is the basis for all permanent magnets (as well as 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 magnetization have been identified when there is more than one magnetic ion per primitive cell of the material, leading to a stricter definition of "ferromagnetism" that is often used to distinguish it from ferrimagnetism. 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).

Definition courtesy of 

Ferromagnetic Curie Temperatures

Material Curie temperature
Fe 1043
Co 1388
Ni 627
Gd 293
Dy 85
CrBr3 37
Au2MnAl 200
Cu2MnAl 630
Cu2MnIn 500
EuO 77
EuS 16.5
MnAs 318
MnBi 670
GdCl3 2.2
Fe2B 1015
MnB 578
Data from F. Keffer, Handbuch der Physik, 18, pt. 2, New York: Springer-Verlag, 1966 and P. Heller, Rep. Progr. Phys., 30, (pt II), 731 (1967)

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