The impact of a nearly cylindrical water mass on a water surface is st
udied both experimentally and theoretically. The experiments consist o
f the rapid release of water from the bottom of a cylindrical containe
r suspended above a large water tank and of the recording of the free-
surface shape of the resulting crater with a high-speed camera. A bubb
le with a diameter of about twice that of the initial cylinder remains
entrapped at the bottom of the crater when the aspect ratio and the e
nergy of the falling water mass are sufficiently large. Many of the sa
lient features of the phenomenon are explained on the basis of simple
physical arguments. Boundary-integral potential-flow simulations of th
e process are also described. These numerical results are in fair to g
ood agreement with the observations.