MULLAPERIAR DAM , GOVERNMENT AND PEOPLE OF KERALA , BE WARNED - CAPT AJIT VADAKAYIL

RUSH RUSH RUSH..

WARNING--.

THERE IS A SCARE IN KERALA THAT THERE ARE EARTH QUAKE TREMORS , CAUSING CRACKS ON HOME WALLS AND COMPOUND WALLS ..

THESE CRACKS ( WHEN FAR AWAY FROM A DAM ) HAVE NOTHING TO DO WITH EARTH QUAKES ..IT HAS TO DO WITH INSUFFICIENT FOUNDATION OF THE STRUCTURE..

I WARN THE KERALA CM -- DO NOT ALLOW IDUKKI DAM RESERVOIR TO GO BEYOND 2402 FEET HEIGHT… TAKE THIS FROM A MAN WHO IS AN EXPERT ON WATER..

NOT A SINGLE DAM IN INDIA HAS BEEN BUILT WITH INBUILT DE-SILTING FACILITIES..

AS A RESULT WHEN DAM RESERVOIRS GET SILTED, THE STUPID COLLEGIUM JUDGES INCREASE THE WATER LEVEL ARBITRARILY, LIKE WHAT HAPPENED AT MULLAPERIAR.. ALL THEY DELIBERATE ON IS IF THE DAM WALL S STRONG ENOUGH…

THESE LAWYERS TURNED JUDGES WHO TAKE TECHNICAL DECISIONS ( PIL BASED ) ARE THE BOTTOM DREGS OF THE SCHOOL CEREBRAL BARREL..

WHEN WATER LEVEL IS RAISED , IMMEDIATELY WATER SURFACE AREA IN THE SILTED RESERVOIR INCREASES --INUNDATING MORE LAND AROUND.. MORE SURFACE AREA MEANS MORE EVAPORATION OF WATER HELD BY THE DAM .

THE MORE DANGEROUS THING IS THIS CAN CAUSE LANDSLIDES AND SOLITION WAVE ( TSUNAMI ) WHICH CAN CRASH INTO THE DAM WALL BREACHING IT..

http://ajitvadakayil.blogspot.com/2011/11/mullaperiar-dam-biggest-disaster-in.html

CRITICAL MESSAGE --- NOW ABOUT TREMORS NEAR DAMS ..

GOD NEVER INTENDED MAN TO BUILD DAMS..

WHEN HUGE DAMS ARE BUILT WITH HIGH WATER LEVELS IN THE RESERVOIR IT CAUSE GEOPATHIC STRESS WHICH MAKES THE AREA TREMOR PRONE.

RESERVOIR INDUCED EARTH QUAKES ARE TERMED RIS ( RESERVOIR INDUCED SEISMICITY)...THIS SUBJECTS HAS BEEN STUDIES AS POST DISASTER REACTIONS – AND NEVER PROACTIVELY BEFORE BUILDING A DAM..

80% OF INDIAs LARGE DAMS ARE PRONE TO RIS – AS THEY HAVE BEEN BUILT WITHOUT PROPER GEOLOGICAL STUDIES ON UNSUITABLE AREAS …

Reservoirs can both increase the frequency of earthquakes in areas of already high seismic activity and cause earthquakes to happen in areas previously thought to be seismically inactive.

Artificial dam reserviors alters in-situ stress along an existing fault or fracture.

In these reservoirs, the weight of the water column can significantly change the stress on an underlying fault or fracture by increasing the total stress through direct loading, or decreasing the effective stress through the increased pore water pressure.

This significant change in stress can lead to sudden movement along the fault or fracture, resulting in an earthquake.

The 6.3 magnitude 1967 Koynanagar earthquake occurred in Maharashtra, India with its epicenter, fore- and aftershocks all located near or under the Koyna Dam reservoir. 180 people died and 1,500 were left injured. The effects of the earthquake were felt 230 km away in Mumbai with tremors and power outages.

LATUR EARTHQUAKE NEAR BHEED MARATHWADA---

Latur earthquake was one of the deadliest earthquakes Maharashtra has seen till date. The earthquake struck at about 3.56 am on September 30, 1993. In the intraplate earthquake about 52 villages were destroyed, over 30,000 were injured and approximately 10,000 were killed. The earthquake left a huge hollow at Killari, which was also the epicentre, remains in place till date.

The 1979 MORVI DAM BURST ( rajkot , gujarat ) is in the Guinness book of world records.

Has India ever investigated the reason for 26,000 deaths at Morvi due to induced seismicity ?

Has India investigates the 1967 Koynanagar earthquake occurred in Maharashtra, with its epicenter, fore- and aftershocks all located near or under the Koyna Dam reservoir.

In dam water reservoirs, the crushing weight of the water column can significantly change the stress on an underlying fault or fracture by increasing the total stress through direct loading.

God has made huge NATURAL lakes in safe areas --unlike man's ARTIFICIAL DAM RESERVOIRS.
Significant change in stress can lead to sudden movement along the fault or fracture, resulting in an earthquake. When dam reservoirs are filled or drained, induced seismicity can occur immediately or with a small time lag.


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