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The origin of the Sunderbans is as baffling and mysterious as its crisscrossed riverine basin. It provides fascinating subjects of study for scientists Authentic Rashaad Penny Jersey , historians, geologists and naturalists alike. A sundarban tour is a must for people like us.

The most common belief is that a series of tectonic activity causing elevations and depressions of the gneissic hills occured in the Gondwana belt 200 million years ago. This coupled with the gradual deposition of alluvial silt brought from the folded Himalayas in the North through centuries, resulted in the basic formation of this lower Gangetic delta. Previously the marshy land stretched upto Rajmahal hills of the Chotanagpur area of what is now the state of Jharkhand. Around 35 million years ago in the late Tertiary period Tedric Thompson Jersey , the debris from the Himalayas filled the entire area.

Some experts affirm that the Ganga and Brahmaputra were east-flowing rivers until the block-faulting in the Garo-Rajmahal Hills, changed their course southwards. During the <"http:sundarban.tours">sundarban tour ,the slope of the river bed in this region being less than 12 cm Nazair Jones Jersey , the river current was slow. It precipitated a huge deposit of silt from the Himalayas, causing numerous islands to form through the ages.

According to the geologist and structuralist Oldham the whole area of the Sunderbans is a delta formed solely by the drainage of the mighty rivers of the Gangetic plain. While his sundarban tour he also suggested that the trough of the land was the result of the pressure of a huge alluvial deposit. It pushed the earth’s crust down. But here again confusions arise, as some fossils of an estuarine nature were found while digging a deep-well near Garden Reach Delano Hill Jersey , Kolkata, at a depth of 950 ft. Another geologist, J. Fargusson Frank Clark Jersey , on his sundarban travel stated that the entire Bengal basin was a shallow marine land in the early Pleistocene age. In the late Pleistocene age, the sea receded completely from this area. The bulk of the alluvial deposit carried by the rivers covered the marine sediments. However, not many traces of marine animals were found below the ground.

Some scientists on hid sundarban tour studying the physiography of the region have studied the Sunderbans in relation to tidal action. They contend that due to tidal waves and the presence of innumerable tidal estuaries Jarran Reed Jersey , the silt rushed back from the Bay of Bengal. It was pushed back into the moribund channels. The river bed got raised. This blocked water led to the formation of an island. The soil study confirmed that the alluvial deposit of this area is enriched with various salts.

Thus, no chronological scientific history of this area can be traced; however excavations, assumptions and theories ascertain that simultaneous upheavals and subsidence still continue and that the low-lying Sunderbans is still under formation. Aside from this Germain Ifedi Jersey , periodic flooding, and alluvial and diluvion deposits on the banks have changed the course of the innumerable waterways. These crisscross over region forming the world’s largest delta—the Sunderbans.
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