EARTHQUAKES


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Remote sensing allows measuring changes of the terrain surface shape down to the centimetre level. Hence, it can be used to detect small earth crust movements that may be an early warning of an earthquake. In addition, the damages caused by an earthquake may be determined using remote sensing data. ENVISYS proposes an integrated system with these two features and fully automatic retrieval of data. 
 

    

SAR interferometry measures the phase difference between two images, corresponding to the change in the round-trip path length of the radar waves to the same ground point. The right image shows the phase difference between two images. In the left image the colours represent the magnitude of the earth crust movement, with areas of largest movements in red.
 
 
 
 
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