A state that is locally stable but not globally stable, like supercooled water.A metastable state is a condition of a system that is locally stable—it resists small perturbations—but not globally stable, meaning a sufficiently large disturbance or a slow transition can push it to a lower-energy, more stable configuration. Supercooled water is the classic example: it remains liquid below 0°C until a tiny impurity or vibration triggers rapid freezing. Metastable states are ubiquitous in physics, chemistry, and materials science, from supersaturated solutions to excited atomic states that persist far longer than typical lifetimes.
The concept of metastability was formalized in the late 19th century by scientists studying phase transitions, notably Wilhelm Ostwald, who articulated the idea of metastable states in his work on chemical equilibria and crystallization.
The system sits in a local minimum of its energy landscape, separated from the global minimum by an energy barrier. Thermal fluctuations or quantum tunneling can occasionally overcome this barrier, but the probability is low if the barrier is high relative to the available energy. In many cases, the metastable state is 'trapped' because the transition requires a coordinated rearrangement of many particles—like the nucleation of a crystal in a supercooled liquid—which is statistically unlikely without a seed. The lifetime of a metastable state can range from nanoseconds to the age of the universe, depending on the barrier height and temperature.
Metastable states are exploited in technologies like phase-change memory (where a material switches between crystalline and amorphous states) and in pharmaceutical formulations that use metastable polymorphs to improve drug solubility.
Diamonds are a metastable form of carbon—at room temperature and pressure, graphite is actually more stable, but the energy barrier is so high that diamonds persist for billions of years.










