The ability of a material to retain its previous magnetization state after being altered.Magnetic memory is the property of a magnetic material to retain its magnetization state after the external field that set it is removed. This hysteresis—the lag between input and output—is what makes permanent magnets permanent and is the physical basis for all magnetic data storage. Without it, a hard drive would forget everything the moment the write head moved away.
The term 'hysteresis' was coined by James Alfred Ewing in 1881, who studied magnetic lag in iron. The first practical magnetic recording used steel wire in the late 19th century, but the modern understanding of retention as an energy-barrier problem emerged with the work of Louis Néel in the 1940s.
When an external field aligns magnetic moments, the material's energy landscape has multiple local minima separated by energy barriers. After the field is removed, thermal fluctuations can push moments over these barriers, causing relaxation. If the barriers are high compared to thermal energy (k_B T), the state persists for a long time. The coercivity—the field needed to flip the magnetization—quantifies this stability. Materials with high coercivity (like neodymium magnets) retain strong magnetization; low-coercivity materials (like soft iron) lose it easily.
Magnetic memory is the foundation of hard disk drives, magnetic tape, and magnetic random-access memory (MRAM), where bits are stored as magnetization directions.
The Earth's magnetic field itself is a form of magnetic memory: rocks record the field direction at the time they cool, giving geologists a history of plate tectonics and pole reversals.




