When a vessel leaves the surface and plunges to the seabed, a lot of things can happen that will affect its orientation and position on the seabed and the creation and distribution of the debris field. Crushing and catastrophic implosion due to the rapidly increasing hydrostatic pressure has been noted on portions of many wrecks. Extensive damage due to bottom impact and subsequent motions have also been observed and documented. This paper describes the successful numerical modeling of the sinking of several historic vessels. One was in deep water and another in shallow water. In both cases it was possible for the simulation to replicate important details of the debris field. Further work is planned to help explain some of the taphonomy observed as the wreck decays over time as it is acted on by bottom currents, benthic storms and in the shallow case storm waves.

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