= Ductility (Earth science)
{wiki=Ductility_(Earth_science)}
In earth science, ductility refers to the ability of a material, particularly rocks and minerals, to deform under stress without breaking. It is a measure of the material's capacity to undergo significant plastic deformation when subjected to tensile or compressive forces. This property is crucial in understanding geological processes, such as the behavior of Earth's crust during tectonic movements. Ductile materials can bend, stretch, or flow over time when subjected to sustained pressure, rather than fracturing.
Back to article page
