Describe the Narmada and Ganga Basin.
Answers
With due respect to all of your votes, I wanna say something out of the box contents. I know Ganga flows thro different path & ends in Gangasagar…..and never meets Narmada. But if you just” google -earth” river Narmada, especially zooming Gujarath….you”ll find a small village Chandod on the north bank of Narmada which is again situated on the confluence of Aurvi river & Narmada river. Going thro some excerpts from Narmada-puran…..a statement is made stating that once in a year in Vaishakh { may }month”s saptami, Ganga comes and meets Narmada to cleanse its own pap [ rather deposited by Ganga devotees when they take a holy deep for their cleansing }.
Now that”s stupefying……how”s that……
But to me ….half physical science approach & half devotional attitude, in the month of May…Ganga gets a partial floodage in its basin as the glaciers thro which it is supplied get melted due to heat…naturally its water level rises somewhat whereas rest of the rivers which dont discharge from glaciers….their water level is surprisingly lowered in this period. As we study the topographical position we”ll find outer basin of river Aurvi is connected to outerbasin of Parbati river which in turn is the tributary of Charmanvati [ Chambal ] . chambal meets to Yamuna which susequently confluences to Ganga in Prayag. So if you reverse this path as about turn….it is quite possible that in the later dried stages of May..we may find this amazing feat to be in reality… But still as a physical science student a question remains…..how the water can take this capillary action defying the laws of Physics?
But considering this whole scenario thro goggles of Astral science rather Metaphysics I would say….. river Narmada is the oldest river on earth which runs through a big Rift. So it”s clear that it is very very deep. Rather it runs thro the Earth’s crest [ ALFRED WEGNER …German scientist says this ] also. And if we just google …the deepest man- made hole prevailing on the earth is in Russia called as KOLA BOREHOLE which is 7.2 km deeper and amazingly we find clear source of water after 7 km. in that KOLA. Going deep in for seven km we find some life in it which is called as PLANKTONIC CREATURES. So this undercurrent can be termed as PLANKTONIC UNDERWAY which is under-interconnected to Gangetic undercurrent whose suitable path meets in Chandod village. This is all underground novelty. As Narmada’s course beneath earth which looks ulterior but prevails lively contains calcareous sandstone, calcified sandstone, mottled nodular sandstone, smectic, chlorite, kaolinite,illite, & volcanic calcidonite which in gross produce PLANKTONS & PHYTOPLANKTONS. PHYTOPLANKTONS found in Narmada are of ten types outta which CYNOPHYCEAE is found in abundance. Now coming toward Gangetic attributes……Ganga uniquely produces BACTORIOPHAGUS whose only job ever is to eliminate impurities & keep Gangetic water pure ,holy & clean forever.[ that”s why Ganga is revered as a Holy ]
In the month of May, production of BACTERIOPHAGES drastically lowers down and struggles its sustainability which in turn causes Ganga to flow towards Narmada thro undercurrent as CYNOPHYCEAE increases production of BACTO. in exuberence….and turns back vice versa back to Ganga. This phenomenon lasts for a couple of days.
The Ganges basin is a part of the Ganges-Brahmaputra basin draining 1,086,000 square kilometres in Tibet, Nepal, India and Bangladesh. To the north, the Himalaya or lower parallel ranges beyond form the Ganges-Brahmaputra divide. On the west the Ganges Basin borders the Indus basin and then the Aravalli ridge. Southern limits are the Vindhyas and Chota Nagpur Plateau. On the east the Ganges merges with the Brahmaputra through a complex system of common distributaries into the Bay of Bengal. Its catchment lies in the states of Uttar Pradesh (294,364 km²), Madhya Pradesh(198,962 km²), Bihar (143,961 km²), Rajasthan(112,490 km²), West Bengal (71,485 km²), Haryana (34,341 km²), Himachal Pradesh(4,317 km²) , Delhi, Arunachal pradesh(1,484 km²), the whole of Bangladesh, Nepal and Bhutan. Several tributaries rise inside Tibet before flowing south through Nepal. The basin has a population of more than 500 million, making it the most populated river basin in the world.