The Oppenheimer-Snyder model describes a homogeneous ball of pressureless matter collapsing from rest, with a closed FLRW metric inside and a Schwarzschild metric outside. In geometric units its interior is , with and . The boundary is a fixed comoving angle. Density conservation gives constant, and the Friedmann equation at the initial turning point gives .
The comoving dust ball in the Oppenheimer-Snyder model is an Oppenheimer-Snyder cloud. Its pressureless matter has uniform density on each constant-proper time slice and reaches a simultaneous final singularity in the ideal homogeneous model.
Radial outgoing null geodesics in the interior of Oppenheimer-Snyder collapse obey . Trace the ray crossing the boundary at backward: it starts at the centre at . This ray is the event horizon; it can exist inside the cloud before the surface crosses . An event horizon is determined by global escape to future null infinity, rather than by a local stopwatch signal.
A boundary clock in Oppenheimer-Snyder collapse reads . Its event horizon crossing occurs at , giving the displayed angle, and the final curvature singularity occurs at . The remaining proper time is . For this approaches , but it is not exactly that value for finite release radius.
At the boundary of an Oppenheimer-Snyder cloud, its areal radius is . Matching to a Schwarzschild metric gives . Thus and . The boundary is a radial timelike geodesic with specific Killing energy . Its radial equation is . The induced metric and the angular extrinsic curvature agree on both sides, so no surface layer is required.

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The Oppenheimer–Snyder model is a solution to Einstein's general relativity that describes the gravitational collapse of a homogeneous dust sphere. It was first introduced by physicists J. Robert Oppenheimer and Hartland Snyder in a landmark paper published in 1939. This model is significant in theoretical physics as it lays the groundwork for understanding black holes and gravitational collapse.