A rheid d is a non-molten solid that deforms by viscous flow at least a thousand times faster than it would deform elastically under the same applied stress. The term, which was coined by S. Warren Carey in 1953, has the same Greek root as rheology, the science of viscoelasticity and nonlinear flow. ==Types of rheids== Almost any type of rock can ...
Found on
http://en.wikipedia.org/wiki/Rheid
substance that flows viscously when below its melting point
Found on
http://phrontistery.info/r.html
No exact match found.
