The surface roughness of hydraulic fractures reflects the fracturing proces
s at the tip. We conducted an experimental study of hydraulic fracture prop
agation and observed a characteristic roughness pattern. The roughness deve
loped without sheer or torsional loading in the plane of the penny-shaped f
racture and is determined by material properties and the externally applied
stresses on the sample, which represent the effective in-situ stresses. We
quantified the roughness and showed that it correlated well with a measure
of the plastic zone size around the fracture tip. New explanations for fra
cture surface roughness that develops under Mode I loading conditions are p
resented.