Reconnection of the magnetic lines of force can effectively occur in t
he solar atmosphere, not only in the high-temperature coronal plasma b
ut also in the temperature minimum region between the photosphere and
the chromosphere. A simple model for reconnection in this region is co
nsidered. Parameters of the stationary reconnecting current sheet are
expressed through the concentration and temperature of the outside col
d and dense plasma, magnetic field intensity, and the speed of the pho
tospheric convective flows. The flux of matter through the current she
et upward F congruent-to 10(10) - 10(12) g s-1 is sufficient for promi
nence formation in the upper chromosphere or lower corona.