When an asteroid strikes Earth, its kinetic power is rapidly transferred primarily to the atmosphere, surface, and subsurface in the forms of thermal energy (heating and vaporization), mechanical energy (crater formation and ejecta), and seismic energy (earthquakes and waves).
When an asteroid strikes Earth, its kinetic power is rapidly transferred primarily to the atmosphere, surface, and subsurface in the forms of thermal energy (heating and vaporization), mechanical energy (crater formation and ejecta), and seismic energy (earthquakes and waves).