The 1993 Killari (Latur) earthquake in Maharashtra has provided a rare
example of surface rupture in the Precambrian shield, No historic sei
smic events of comparable magnitude have been recorded in Killari. How
ever, deep trenching in the 1993 rupture zone revealed deformational s
tructures consisting of thrust sheets possibly related to previous fau
lting. These structures indicate that the 1993 event was indeed preced
ed by earthquakes in the recent geologic past. Our studies also indica
ted an obsequent fault-line scarp, aligned with the current rupture zo
ne. The morphological features in the area suggest mass removal of the
upper part of the hanging wall, that is on the southwestern side of t
he rupture, aided by the highly crushed nature of the rock and high ra
te of weathering. Our observations imply a long recurrence interval of
seismic events in the epicentral area of the 1993 earthquake.