Volume change in argillaceous sediments can take place due to either swelli
ng of expansive clay or gypsification of anhydrous calcium sulfate. Gypsifi
cation offers a variety of serious geotechnical hazards such as high swell
pressure, Boor heave in tunnels, massive rock uplift in dams, and damages t
o light structures and pavements. Some of these phenomena have been observe
d in the Arabian Gulf coastal region, where the behavior of local argillace
ous sediments is controlled by severe climatic and environmental conditions
. Based on laboratory investigation of natural and synthetic samples, this
paper studies the influence of gypsification of anhydrite on the engineerin
g behavior of calcareous expansive clay.