The expected future super-eruption of the Yellowstone super volcano (USA) is “cancelled” by the Pleistocene glaciation and by the inversion of caldera complex development

Q4 Earth and Planetary Sciences
I. Melekestsev, И В Мелекесцев
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引用次数: 0

Abstract

The review of the reconstructions of the eruptive activity of the Yellowstone Caldera Complex (YCC) in the USA allows to suggests three groups of arguments supporting that the “volcanic super-eruption of Yellowstone” is not likely to occur in the coming hundreds or thousands of years. First is the gradual weakening of the volcanic potential of the magmatic source (which is the frontal lobe of the magmatic super-flow, and not the mantle plume) during the last 2 million yeats. Second is the impact of the repeated occurrence of ice sheets in the YCC area during the past 640 thousand years. Finally, the equivalent super-eruption, in terms of energy released and the mass of exploded material, had already occurred at about 70 thousand years ago, and since that time, the YCC has passed from the volcanic to the hydrothermal evolutionary stage.
预计美国黄石超级火山未来的超级喷发因更新世冰川作用和破火山口复合体的倒转而“取消”
对美国黄石火山口综合体(YCC)喷发活动重建的回顾表明,有三组论点支持“黄石火山超级喷发”在未来数百年或数千年内不太可能发生。首先是在过去200万年中,岩浆源(即岩浆超流的额叶,而不是地幔柱)的火山潜力逐渐减弱。其次是过去64万年中YCC地区冰盖反复出现的影响。最后,就释放的能量和爆炸物质的质量而言,等效的超级喷发已经发生在大约7万年前,从那时起,YCC已经从火山演化到了热液演化阶段。
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来源期刊
Geomorfologiya
Geomorfologiya Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
0.80
自引率
0.00%
发文量
8
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