The two-dimensional displacement vector field on the Earth's surface associ
ated with a large earthquake near Iwate volcano in Japan, was mapped by com
bining satellite radar interferometry images from two different track direc
tions. The displacement reveals not only large main ruptures, but details o
f many small faults movement of aftershocks and volcanic earthquakes. The d
isplacements of the aftershock faults coincide with a stress held reorganiz
ed by the main earthquake that accelerated the aftershock fault movements.
The displacements mimic the topography, suggesting that repeated movements
of the same faults in the Quaternary have led to the presently existing top
ography.