Verneshot

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A verneshot (named after French author Jules Verne) is a hypothetical volcanic eruption event caused by the buildup of gas deep underneath a craton. Such an event may be forceful enough to launch an extreme amount of material from the crust and mantle into a sub-orbital trajectory, leading to significant further damage after the material crashes back down to the surface.

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Connection with mass extinctions

Verneshots have been proposed as a causal mechanism explaining the statistically unlikely contemporaneous occurrence of continental flood basalts, mass extinctions, and "impact signals" (such as planar deformation features, shocked quartz, and iridium anomalies) traditionally considered definitive evidence of hypervelocity impact events. [1]

The verneshot theory suggests that mantle plumes may cause heating and the buildup of carbon dioxide gas underneath continental lithosphere. If continental rifting occurs above this location, an explosive release of the built up gas may occur, potentially sending out a column of crust and mantle into a globally dispersive, super-stratospheric trajectory. It is unclear whether such a column could stay coherent through this process, or whether the force of this process would result in it shattering into much smaller pieces before impacting. The pipe through which the magma and gas had travelled would collapse during this process, sending a shockwave at hypersonic velocity that would deform the surrounding craton.

A verneshot event is likely to be related to nearby continental flood basalt events, which may occur before, during or after the verneshot event. This may help in searching for evidence for the results of verneshot events; however, it is also quite probable that most of such evidence will be buried underneath the basalt flows, making investigation difficult. J. Phipps Morgan and others have suggested that subcircular Bouguer gravity anomalies recognized beneath the Deccan Traps may indicate the presence of verneshot pipes related to the Cretaceous–Paleogene extinction event. [1]

If the Deccan Traps were the location of a verneshot event at the Cretaceous–Paleogene boundary, the strong iridium spike at the Cretaceous–Paleogene boundary could be explained by the iridium-rich nature of volatiles in the Reunion mantle plume, which is currently beneath Piton de la Fournaise, but during the end Cretaceous was located beneath India in the area of the Deccan Traps; the verneshot event could potentially distribute the iridium globally. [1]

Tunguska event

A verneshot has been proposed as an alternate explanation for the Tunguska event, widely regarded as the result of an atmospheric explosion of a small comet or asteroid. Arguments offered for this mechanism include the lack of extraterrestrial material at the event site, the lack of a credible impact structure, and the presence of shocked quartz in surface outcrops. [2] However, this hypothesis has not been generally accepted, with Mark Boslough arguing that there is no basis for rejecting the impact hypothesis. [3]

Name

In 1865 Jules Verne's novel From the Earth to the Moon introduced the concept of a ballistic projectile escaping the Earth's gravity, from which Phipps Morgan and others derived the name "Verneshot" in their paper theorizing a connection between extinction events and cratonic gas ejection.

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The Deccan Traps is a large igneous province of west-central India. It is one of the largest volcanic features on Earth, taking the form of a large shield volcano. It consists of numerous layers of solidified flood basalt that together are more than about 2,000 metres (6,600 ft) thick, cover an area of about 500,000 square kilometres (200,000 sq mi), and have a volume of about 1,000,000 cubic kilometres (200,000 cu mi). Originally, the Deccan Traps may have covered about 1,500,000 square kilometres (600,000 sq mi), with a correspondingly larger original volume. This volume overlies the Archean age Indian Shield, which is likely the lithology the province passed through during eruption. The province is commonly divided into four subprovinces: the main Deccan, the Malwa Plateau, the Mandla Lobe, and the Saurashtran Plateau.

<span class="mw-page-title-main">Tunguska event</span> 1908 meteor air burst explosion in Siberia

The Tunguska event was a large explosion of between 3 and 50 megatons that occurred near the Podkamennaya Tunguska River in Yeniseysk Governorate, Russia, on the morning of 30 June 1908. The explosion over the sparsely populated East Siberian taiga flattened an estimated 80 million trees over an area of 2,150 km2 (830 sq mi) of forest, and eyewitness accounts suggest up to three people may have died. The explosion is generally attributed to a meteor air burst, the atmospheric explosion of a stony asteroid about 50–60 metres wide. The asteroid approached from the east-south-east, probably with a relatively high speed of about 27 km/s (60,000 mph). Though the incident is classified as an impact event, the object is thought to have exploded at an altitude of 5 to 10 kilometres rather than hitting the Earth's surface, leaving no impact crater.

<span class="mw-page-title-main">Chicxulub crater</span> Prehistoric impact crater in Mexico

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<span class="mw-page-title-main">Cretaceous–Paleogene extinction event</span> Mass extinction event about 66 million years ago

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<span class="mw-page-title-main">Asish Basu</span> Indian geologist, academic, and researcher

Asish R. Basu is a geologist, academic, and researcher. He is Professor Emeritus of Earth and Environmental Sciences at the University of Texas at Arlington. He is most known for his research in Earth Science -related subjects, such as isotope geochemistry, flood basalt volcanism, and mineralogy-petrology.

References

  1. 1 2 3 Phipps Morgan, J.; Reston, T. J.; Ranero, C. R. (15 January 2004). "Contemporaneous mass extinctions, continental flood basalts, and 'impact signals': are mantle plume-induced lithospheric gas explosions the causal link?" (PDF). Earth and Planetary Science Letters . 217 (3–4): 263–284. Bibcode:2004E&PSL.217..263P. doi:10.1016/S0012-821X(03)00602-2. (First submitted 17 April 2003). For an informal introduction see Professor Jason Phipps Morgan's faculty biography Archived 22 September 2006 at the Wayback Machine at Cornell University from May 2004: I became interested in the causes of mass-extinctions, in particular worrying about the 'too-many-coincidences' problem that these periods appear to be associated (if we believe what's published in the mainstream literature) with BOTH extremely rare continental flood basalts and continental rifting, and even rarer 'impact signals' commonly presumed to come from large extraterrestrial bolide impacts. Our recently published Verneshot hypothesis is our best guess on how to explain these coincidences in a self-consistent causal manner.'
  2. Vannucchi, Paola; Morgan, Jason P.; Della Lunga, Damiano; Andronicos, Christopher L.; Morgan, W. Jason (January 2015). "Direct evidence of ancient shock metamorphism at the site of the 1908 Tunguska event". Earth and Planetary Science Letters. 409: 168–174. Bibcode:2015E&PSL.409..168V. doi:10.1016/j.epsl.2014.11.001.
  3. Cohen, David (25 June 2008). "Tugnuska 100 years on". New Scientist. 198 (2662): 38–41. doi:10.1016/S0262-4079(08)61618-8.