As an object enters the atmosphere at 7+ km/s, aerodynamic heating converts kinetic energy into heat at a rate that destroys most materials within seconds. What survives tells us about composition and structure.
As an object enters the atmosphere at 7+ km/s, aerodynamic heating converts kinetic energy into heat at a rate that destroys most materials within seconds. What survives tells us about composition and structure.
Material properties — melting point, density, thermal conductivity — determine survivability.
Surviving fragments spread across a ground footprint spanning hundreds to thousands of kilometres.
The combination of mostly-ocean corridors and mostly-ablated mass means uncontrolled re-entries, while newsworthy, carry extremely low individual risk.