Vacancy islands formed during room-temperature exposure to sulfur of a subm
onolayer Ag him on Ru(0001) order spontaneously to form a triangular lattic
e at an island area fraction just above 20%. A normal mode decomposition of
the thermal vibrations of this vacancy island crystal, measured with time-
resolved scanning tunneling microscopy, obtains Lame coefficients in the ra
nge of 10(8) N m(-2). We show that these estimates are consistent with stab
ilizing forces derived from long-range elastic interactions between the isl
ands. (C) 1999 Elsevier Science B.V. All rights reserved.