Evidence is presented of the dynamic nucleation of ice induced by an i
solated stable cavitation bubble in undercooled water. The evidence su
pports the notion of dynamic nucleation as a result of the freezing po
int shift due to high pressure pulses associated with a collapsing bub
ble. It is found that the cavitation bubble requires minimum undercool
ing, 5 K, to initiate nucleation on ide. This undercooling may be attr
ibuted to the temperature rise of the water due to the heat generated
by compression of the bubble or the undercooling required for normal i
ce to nucleate on a high pressure phase. (C) 1998 American Institute o
f Physics.