Deformation where layers of material slide past each other.Shear is a type of deformation in which layers of a material slide past one another parallel to the applied force. Unlike compression or tension, which change volume, shear changes the shape of an object while keeping its volume constant. This concept is fundamental in understanding how fluids flow, how solids deform under stress, and how geological faults cause earthquakes.
The concept of shear stress and strain was formalized in the 19th century by scientists like Augustin-Louis Cauchy, who developed the mathematical framework for continuum mechanics.
When a shear force is applied, adjacent layers of material move relative to each other. The shear strain is defined as the displacement of one layer relative to another divided by the distance between them. In fluids, shear causes viscous flow, where the resistance to sliding is characterized by viscosity. In solids, shear stress can lead to plastic deformation or fracture, depending on the material's strength and the magnitude of the stress.
Shear is central to the design of lubricants, the analysis of earthquake fault mechanics, and the processing of polymers and metals in manufacturing.
When you stir honey with a spoon, you are applying shear — the honey's resistance to that shear is what makes it feel thick and sticky.















