We report that during the two devastating 1999 earthquakes in Turkey, ruptu
re propagated over a large part of the nearly 200km long fault zone at supe
rshear speed approaching 5km/s. We present observations and modeling which
confirm the original inference of supershear rupture during the Izmit earth
quake and we show that supershear rupture also occurred during the Duzce ea
rthquake. We show that the rupture velocity measured - about root2 times th
e shear wave velocity - is the value predicted by theoretical studies in fr
acture dynamics. We look for clues to explain these observations.