Water entry is an impulsive two-phase flow often met in nature and in industrial processes. Violent vertical entries are observed when the projectile is heavy and when the Froude number is high enough: they form a distinct category characterized by an elongated cavity trailed by the projectile. The guiding idea in the present approach is to regard the union of the deep cavity caped by the sphere as a composite deformable body relevant to the theory of flows past slender bodies. This process allows linearization, making the problem analytically tractable when air behaves as a passive component, a case occurring very often due to the contrast in density between air and water. Asymptotic analysis shows that the length of the slender body is of the order of RF 2∕3, with F=U(gR)−12 the Froude number, R being the radius, U the speed at entry and g the gravity. That gives rise to a parameter scaling the importance of the air flow inside the cavity, D=(ρa∕ρ)F4∕3, with ρ and ρa the water and air densities. In what follows we adopt the mathematical symbols o and O , with D=o(1) when D≪1 and D=O(1) when D is of the order of 1 but cannot become ≪1. As long as water and air are considered as inviscid, the dimensionless parameters governing the flow are F, D and ρb∕ρ, with ρb the projectile density. In the present contribution we introduce the concept of ideal deep cavity, which does not take into account some transitory perturbations occurring just after impact. Access is obtained to the water velocity potential and to the equations governing the shape of the cavity and the air flow filling the cavity. The problem is solved for D=o(1), which is met in most cases owing to the smallness of ρa /ρ, even if F is very high. Water velocity and air pressure are expressed in terms of the sectional area S of the slender body. Still for D=o(1), a full solution including friction, turbulence and separation is obtained afterward provided the characteristic Reynolds number Re is high. However, transient unsteadiness instigated by a sudden impingement, or transition from laminar to turbulent regimes cannot be characterized by quantitative criteria put in advance, making the task difficult. One of significant features revealed by the present contribution is the important role of friction, which has been generally ignored in previous investigations. The cavity seal appears to be closely connected to friction and instability through the way how separation occurs. The theoretical model is consistent with separation taking place above the equator. A typical property arises: violent cavity sealing occurs in the first third of the distance between atmosphere and the sphere. Present results come complete past entry models elaborated at moderate Froude number. Finally, validation is based on results obtained almost seventy years ago at the Naval Ordnance Laboratory, USA.