Linked from

The 24 pages that link to Curie temperature, each with the reason it gives.

• PaleomagnetismRelated: Cooling below it is the moment a lava locks in the field's direction.

• FerromagnetismRelated: Thermal disorder destroys ferromagnetic alignment above this material-specific threshold.

• Magnetic domainRelated: Above it, thermal disorder destroys the domain structure of a ferromagnet.

• MagnetizationRelated: Crossing this temperature sharply changes the material’s possible magnetization.

• MagnetiteRelated: Above roughly 580 °C, magnetite no longer retains ferrimagnetic order.

• Symmetry breakingRelated: Crossing it illustrates the loss of an ordered, symmetry-broken magnetic phase.

• FerrimagnetismRelated: Heating past this threshold destroys ferrimagnetic order.

• Neodymium magnetRelated: Heating toward this threshold can permanently impair a neodymium magnet’s performance.

• Permanent magnetRelated: Heating beyond this threshold can destroy a magnet’s ordered magnetic state.

• FerriteRelated: Ferrite’s magnetic behavior changes near iron’s Curie temperature, about 770 °C.

• Rare-earth magnetRelated: Heating toward this limit weakens a rare-earth magnet’s magnetic performance.

• NeodymiumRelated: It sets a critical operating limit for neodymium-based permanent magnets.

• GadoliniumRelated: Gadolinium becomes paramagnetic above its Curie temperature, near room temperature.

• Thermoremanent magnetizationRelated: Above this threshold, thermal agitation erases the ordered magnetization that cooling can later lock in.

• Curie's lawRelated: Near this transition, interactions and critical behavior invalidate the simple law.

• Iron(II,III) oxideRelated: Above magnetite's Curie temperature, its spontaneous ferrimagnetic order disappears.

• Spontaneous magnetizationRelated: It marks the thermal transition that destroys ferromagnetic order.

• Charles-Édouard GuillaumeRelated: Magnetic transitions help explain why certain iron–nickel alloys show unusual thermal expansion.

• Hopkinson effectRelated: The Hopkinson peak occurs just below this transition, where magnetic order is weakening.

• Rock magnetismRelated: Heating through this threshold can erase a mineral’s remanent record.