This paper reports an experimental study on the evolution of an isolat
ed turbulent region in an otherwise quiescent linearly stratified flui
d. A turbulent patch was generated by pulsed horizontal injection of a
small volume of fluid. It was found that the turbulent blob thus prod
uced initially grows as in a nonstratified fluid for a nondimensional
time period of Nt approximate to 4 - 5 (with N the buoyancy frequency)
, attains a maximum height, and then physically collapses slowly to fo
rm a planar, quasi- two-dimensional dipole pattern. The timescale for
the physical collapse of the blob was found to be much larger than tha
t of the turbulence collapse. Scaling arguments are presented to expla
in the evolution of the turbulent region, and the experimental results
are compared with the model predictions.