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Depletion zones are the least well understood component of mud volcanic systems. They are generally difficult to image using reflection seismic data, and have only rarely been identified and described in the subsurface. This study documents 277 mapped depletion zones in the western Nile Cone, offshore Egypt, of which the dimensions and stratigraphic characteristics of a sub-set of 86 depletion zones associated with mud volcanoes of early Pliocene to Recent age are recorded. The primary database used is a large (4,300 km2) 3D seismic survey in which depletion zones can be confidently interpreted using a set of simple criteria. The sub-set of 86 depletion zones were selected for morphometric analysis by virtue of the quality of seismic imaging. The depletion zones are characterised by circular to elliptical planforms with a bowl or conical geometry. They exhibit truncational stratal relationships with their parent stratigraphic unit, which in this area is the Mid-Late Miocene aged OM2 unit, and which occurs directly beneath the Messinian Evaporites. This geometry implies a top-down formation mechanism. Their diameters and relief range from is 600 m–3300 m, and 100 m–740 m, respectively, with a modest scaling relationship between diameter and relief. Flank angles of bowls and cones range from 11⁰ to 41⁰, with a crudely normal distribution, with median and mean values of 26⁰. A model for the evolution of depletion zones in the study area is based on two previous models developed for single source layer plumbing systems and invokes mobilisation of the source layer by sediment collapse and shear-induced liquefaction following initial seal failure by hydraulic fracturing of the evaporite seal. This mechanism may be more widely applicable to mud volcano systems than currently appreciated. • Documentation of detailed morphology of 86 depletion zones to mud volcanoes in the Eastern Mediterranean using 3D seismic imaging. • Stratigraphic traps beneath Messinian Salt provided the template for extremely high overpressure, seal failure and hydraulic fracturing. • Expulsion of highly overpressured fluids from the Pre Salt led to shear-induced liquefaction and expulsion of muddy slurry to form the mud volcanoes. • A general model is developed for single source layer depletion by liquefaction to fuel mud volcanism. • Depletion zones grow by a self-similar process resulting in conical morphologies with a narrow range of flank angles (mean flank angle 26⁰). [ABSTRACT FROM AUTHOR]