The cross-stream dimension of a horizontal, thermally stratified intrusion flow, that travels underneath an insulating wall into a heavier, isothermal fluid, is investigated experimentally. The observed development of a regular temperature variation along that third dimension is linked to a Rayleigh-Bénard-like instability, which is caused by the fact that the upper part of the intrusion flow is effectively heated from below through internal heat advection. These results can be understood by linear stability calculations and contradict the assumption of all previous investigations that the flow is essentially two dimensional.