The high-pressure structural behaviour of AgF has been studied by the
powder neutron diffraction technique. The material undergoes a pressur
e-induced transition at 2.70(2) GPa from the rocksalt structure to the
CsCl-type arrangement with a volume change of similar to 10%. On decr
easing pressure, the reverse CsCl --> rocksalt transition occurs via a
n intermediate phase possessing the hexagonal anti-NiAs structure. A p
lausible structural model to explain this observation is provided, tog
ether with a discussion of the relative stability of the (anti-) NiAs
arrangement as a high-pressure polymorph in binary MX compounds.