part 4 (after setu) setu samudram project ramavaradhi adams bridge
TRANSCRIPT
After Effects Of Sethu Bandhan (Rama Varadhi)
Part 4
in a period of 17,50,000 years
After Effects Of Sethu Bandhan
Due to rotation of Earth and due to gravitational pull of Sun and Moon the
variations in sea tide moves from east to west. Sands washed from various rivers of
Bangladesh and east coast of India, falling into Bay of Bengal move along the coast partially deposited on sea shores and the rest tends to moves towards the Equator eastwards.
Prior to Setubandhan the sand moved freely into the Indian Ocean.
Rama Varadhi the Setu blocked drifting sands from various rivers falling into Bay of Bengal deposited on the Indian east coast,
north of Sri Lanka and in Palk bay in a period of 17,50,000 years
After Effects Of Setubandhan
India
Sri Lanka
Sea before Setu
Sea before Setu
After Effects Of Setubandhan
Sri Lanka
After Effects Of SetubandhanDue to block of Rama Setu, Sand from various rivers falling into Bay of Bengal deposited through out the Indian east
coast, north of Sri Lanka and in Palk bay in a period of 1,750,000 years
India
Complete strip of Setubandhan made by Rama is from Ramananthapuram in Tamil Nadu
to Mannar in Srilanka.
Aerial View Of Adams Bridge (Floating Bridge In Ramayanam)
Sri Lanka
Indian SideNotice The Sand Movement Towards Deep Sea.
Notice The Huge Deposit Of Sand
Space images taken by NASA
ADAMS BRIDGE
Pamban bridge
Rameswaram
Dhanushkodi
Under water ridge is visible covering distance between Rameswaram and Manar almost the reverse curvature of the present Adams bridge.
Under water ridge is visible covering distance between Rameswaram and Manar almost the reverse curvature of the present Adams bridge.
Probably the original bridge made by Rama had a
continues curve upward from Ramananta puram
to Manar in Srilanka
Probably the Curve may be upwards against the sea currents when it was made. In this 17,50,000 years it might
have bent down wards due to pressure of drifting sands.
Probably the original bridge
The anchored stones of the floating bridge
attained a shape like Dhanush (bow) due to pressure of sands
prevented from drifting into deep sea of Indian Ocean.
After Effects Of Sethu Bandhan
Notice the Curve bent towards Indian Ocean due to pressure of drifting sands
from Palkbay to Indian Ocean
This part was the floating bridge built by Rama. In course of time the floating part got washed away by the sea. Now the stones visible are the
anchoring stones of the bridge
Sea Bottom
India Sri LankaSea
What is visible from Satellite and attained the name Adams Bridge is the shoal of rocks used as anchors for the floating bridge by Rama.
On passage of time the wooden floating bridge perished.
After Effects Of Sethu Bandhan
Complete strip of Setu Bandhan made by Rama is from Ramananthapuram in Tamil Nadu
to Mannar in Srilanka.
Notice the Curve bent towards Indian Ocean due to pressure of drifting sands from Palkbay to Indian Ocean
Notice the Curve bent towards Indian Ocean due to pressure of drifting sands from Palkbay to Indian Ocean
This part was the floating bridge built by Rama. In course
of time the floating part got washed away by the sea. Now
the stones visible are the anchoring stones of the bridgeProbably the
original bridge
Chilika Lake once a part of sea, was formed due to sand dune formation in a period of 1,750,000 years.
Chilika Lake once a part of sea, was formed due to sand dune formation in a period of 1,750,000 years.
Probable Coast
17,50,000 years back
Sand and silt probably deposited along the coast to form huge deltas along Rivers Godavari and
Krishna, in a period of 17,50,000 years.
Probable Coast
17,50,000 years back
Sand and silt probably deposited along the coast to form huge deltas along Rivers Godavari and
Krishna, in a period of 17,50,000 years.
Probable Coast
17,50,000 years back
Sand and silt probably deposited along the coast to form huge deltas along the River Kaveri
in a period of 17,50,000 years.
Notice the size of the deltas much bigger than Krishna
Probable Coast
17,50,000 years back
Sand and silt probably deposited along the coast to form huge deltas along the River Kaveri in a period of 17,50,000 years.
Notice the size of the deltas much bigger than Godavari and Krishna
The deltas formed by Rivers Narmada and Tapi in west coast are very small compared to the Rivers in East coast.
The deltas of Narmada and tapti are very small. The size of the delta of Kaveri is much larger than Krishna and Godavari.
Notice the increase in length of deltas from Godavari to Kaveri.
Regional Soil Deposits of India
Disaster After Setu Opened
For Navigation
See Part 5 for
The deltas of Narmada and tapti are very small. The size of the delta of Kaveri is much larger than Krishna and Godavari.
Notice the increase in length of deltas from Godavari to Kaveri.