Great technology, to use. We have ground moist with water in aquifers which absorb or cushion shocks when the region is subject to earth quakes and tremors. Then in nearby region, we have ground water deep in ground ie bgl is  more than 300 Feet. Because the ground is hard with no water and does not have shock absorbing potential. This phenomenon of having ground hard and with no water is dangerous because when earth quakes occur, all;the shock and trmors atr transmitted to structures made on ground. If the intensity is hig

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Great technology, to use.

We have ground moist with water in aquifers which absorb or cushion shocks when the region is subject to earth quakes and tremors.

Then in nearby region, we have ground water deep in ground ie bgl is  more than 300 Feet. Because the ground is hard with no water and does not have shock absorbing potential.

This phenomenon of having ground hard and with no water is dangerous because when earth quakes occur, all;the shock and trmors atr transmitted to structures made on ground.

If the intensity is hig