This article is devoted to the investigation of soil surface subsidenc
e caused by the production of fluids (water, oil and gas). It first de
scribes the methods available for measuring this subsidence, methods t
hat have become extremely accurate today. Cases are selected from the
literature to identify the mechanisms causing subsidence: reservoir an
d aquifer compaction associated with depletion, mechanisms connected w
ith fluid injections in specific cases (thermal creep, action of water
on chalk). These mechanisms must be taken into account by models prog
ressively enriched with geological, petrophysical and mechanical descr
iptions, substantiated by in situ measurements. Subsidence control dem
ands the control of the in situ pressure, maintained by a fluid compat
ible with the formation. If this control is applied early enough, the
risk of subsidence is virtually nit.