The Shiva Crater

  The Shiva Crater: An Awe-Inspiring Geological Wonder



    Located in the Arabian Sea, South of the western coast of India, there exists a geophysical phenomenon that has remained a subject of interest to scientists for more than four decades now; the Shiva Crater. The monstrous structure is estimated to be about 500 kilometers in diameter and perhaps has its origin in a cataclysmic event which occurred millions of years back which drastically changed the geography of the planet and its history.


    Shiva Crater is a force of nonpareil destructive force, observing the destructive ability of the natural forces and the over whelming power of Space on earth. Due to its size and complex structures of geography and geology that are contained in it, it has been attracting scientific interest from geologists, astronomers, and researchers all over the world.

Exploring the Face of the Moon Hidden by Shiva Crater

    Exploration makes the discover of the Shiva Crater was a spectacular achievement Scientists. Responding to a question during the program, Dr Y in his late thirties, the leader of the team of researchers who discovered this HUGE geologic formation these many years back in the late 1990s with the help of Satellite Imagery and Seismic data said – Theoretically, the practical consequences of what they were stating was phenomenal, considering that the Shiva Crater is one of the biggest impact craters on earth.


    Based on the investigations carried out the scientists have been able to establish the actual history of the formation of the Shiva Crater. According to the theories, several millions of years ago there was an impact of a huge asteroid, which diameter was assumed to be several kilometers, with the surface of the Earth at this area. The great impact alone produced numbers of shock waves that caused a series of disastrous events that would alter tremendously the existence of life on the planet Earth.







Reference

1.       Renne, Paul R.; Deino, Alan L.; Hilgen, Frederik J.; Kuiper, Klaudia F.; Mark, Darren F.; Mitchell, William S.; Morgan, Leah E.; Mundil, Roland; Smit, Jan (7 February 2013). "Time Scales of Critical Events Around the Cretaceous–Paleogene Boundary". Science. 339 (6120): 684–687. Bibcode:2013Sci...339..684Rdoi:10.1126/science.1230492PMID 23393261S2CID 6112274.

2.    Chatterjee, S. (1997). "'Multiple impacts at the KT boundary and the death of the dinosaurs". Comparative Planetology, Geological Education, History of Geology: Proceedings of the 30th International Geological Congress, Beijing, China, 4–14 August 1996. VSP. pp. 31–54. ISBN 978-90-6764-254-5.

3.   Chatterjee, S., N. Guven, A. Yoshinobu, and R. Donofrio. (2006) Shiva Structure: a possible KT boundary impact crater on the western shelf of India. Museum of Texas Tech University Special Publications. 50, 39pp.

4.      Agrawal, P., Pandey, O. (November 2000). "Thermal regime, hydrocarbon maturation and geodynamic events along the western margin of India since late Cretaceous". Journal of Geodynamics. 30 (4): 439–459. Bibcode:2000JGeo...30..439Pdoi:10.1016/S0264-3707(00)00002-8.

5.      Rampino, M. R., and B. M. Haggerty (1996) The “Shiva Hypothesis”: Impacts, mass extinctions, and the galaxy. Earth, Moon, and Planets. 72(1–3):441–460.

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