Jump to content

Shiva crater

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by David Fuchs (talk | contribs) at 21:07, 21 February 2008 (adding image). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

File:Chatterjee-dia-sm.jpg
This computer graphic shows the elevation of the formation, with red peaks being the highest. Specific basins are labeled.

The Shiva crater is an ancient sea floor structure —thought by some researchers to be an impact crater— located beneath the Indian Ocean, west of Mumbai, India. It was named by the paleontologist Sankar Chatterjee after Shiva, the Hindu god of destruction and renewal.

According to the impact hypothesis, it formed around 65 million years ago, at about the same time as a number of other impact craters and the Cretaceous-Tertiary extinction event (K-T boundary). Although the site has shifted since its formation because of sea floor spreading, it has been suggested that when pieced together the putative crater would have been about 600 km by 400 km across and 12 km deep (and may be just part of a larger crater). It is estimated that a crater of that size would have been made by an asteroid or comet 40 km in diameter.

At the time of the K-T extinction, India was located over the Réunion hotspot of the Indian Ocean. Hot material rising from the mantle flooded portions of India with a vast amount of lava, creating a plateau known as the Deccan Traps. The eruptions started a few million years before the K-T extinction and become very abundant at about 65 million years ago. The fact that the supposed Shiva crater lies near the Deccan Traps has been claimed as support for the controversial idea that the eruptions were triggered or accelerated by an impact event. However, it is now thought that impact events ought to cause eruptions on the opposite side of the Earth to where they impacted. It has been hypothesized that either the crater or the deccan traps associated with the area are the reason for the high level of oil and natural gas reserves in the region.[1]

Discovery

Feature specifics

Geology and morphology

Shiva and mass extinction

The discovery of Shiva and other features similar to impact craters like the Chicxulub site has led to the hypothesis that there were in fact multiple impacts which caused the massive extinction event at the end of the Cretaceous period.[2] Other theories have argued that since the Chicxulub impact is believed by some researchers to have occurred earlier than the extinction of the dinosaurs, Shiva's impact was enough cause the mass extinction.[3]

While Chatterjee is confident that Shiva was one of many impacts, stating that "the K-T extinction was definitely a multiple-impact scenario,"[4] other scientists remain unconvinced both that the extinction event was caused by multiple impacts, and that the Shiva feature is in fact a crater; for example, a recent article in the journal Nature suggested another supposed impact feature at Silverpit was in fact a sinkhole depression.[4]

References

  1. ^ http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V9X-402K864-4&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=3b9de0be5aa1e39026ba23a166b27643
  2. ^ http://www.springerlink.com/content/j0204x4768353r20/
  3. ^ Davis, John W (2006-11-15). "Texas Tech Paleontologist Finds Evidence That Meteorite Strike Near Bombay May Have Wiped Out Dinosaurs". Texas Tech University. Retrieved 2008-02-12.
  4. ^ a b Mullen, Leslie (2004-11-02). "Shiva: Another K-T Impact?". SpaceDaily. Retrieved 2008-02-20. - original article at source

18°40′N 70°14′E / 18.667°N 70.233°E / 18.667; 70.233

Template:Geol-stub