新马德里地震遗失的历史

J. Whayne
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引用次数: 0

摘要

新马德里地震遗失的历史。Conevery Bolton Valencius著。(芝加哥:芝加哥大学出版社,2013。460页。插图、地图、注释、书目论文、致谢、索引。35.00美元)。《遗失的新马德里地震历史》将成为世界历史上一些最大规模地震的权威历史——1811-1812年发生在现在密苏里州东南部和阿肯色州东北部的地震。Conevery Bolton Valencius不仅掌握了二手文献,挖掘了原始文献,她还完成了以前没有学者做到的事情。通过从21世纪地震学的角度观察1811年和1812年的灾难性事件,她对可能导致地震的原因以及在那些灾难性的日子里究竟发生了什么提供了一个翔实的描述。这可能是人们对一位受过哈佛科学史课程训练的有成就的学者的期望,但瓦伦修斯通过将社会和宗教历史仔细地纳入叙述中,使他的叙述更加有说服力和持久。在这本深思熟虑且敏锐的引言中,她提出了她想要回答的四个问题:(1)为什么地震在发生的时候很重要?如果它们在当时如此重要,为什么生活在21世纪的人几乎不知道它们呢?(3)地震是如何以及为什么“突然”被科学家重新发现的?(4)沿着新马德里断层线进一步活动的威胁可能是什么?瓦伦修斯围绕这些关键问题撰写了这本书。她首先用美国边疆最具代表性的人物之一戴维·克罗克特(Davy Crockett)来说明当时人们是如何理解地震的。克罗克特声称自己在追赶一只熊时滑进了地震裂缝。这个故事的优点是,至少以一种介绍性的方式回答了作者的两个问题:19世纪早期的边疆居民是如何理解和经历地震的,以及地震是如何成为民间传说的主题的。随着时间的推移,编年史家淡化了裂缝作为故事的一个方面,就像公众对地震失去了兴趣一样。科技和农业的创新消除了地震留下的大部分痕迹,随着现代交流将民间故事变成了浪漫的艺术品,地震逐渐从民族意识中消失了。即使民间传说和口述的真实性在理解地震的范围和原因方面受到怀疑,“两个深刻的变化塑造了现代地震学的学科:在[19到20世纪]交替的几十年里地震观测的仪器化和对地球组成和运动的重新概念化”(. ...页)
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The Lost History of the New Madrid Earthquakes
The Lost History of the New Madrid Earthquakes. By Conevery Bolton Valencius. (Chicago: University of Chicago Press, 2013. Pp. 460. Illustrations, maps, notes, bibliographic essays, acknowledgments, index. $35.00.)The Lost History of the New Madrid Earthquakes will stand as the authoritative history of some of the most massive earthquakes in world history-those that shook what is now southeastern Missouri and northeastern Arkansas in 1811-1812. Not only has Conevery Bolton Valencius mastered the secondary literature and mined the primary documents, she has accomplished what no scholar before had managed. By viewing the cataclysmic events of 1811 and 1812 through the lens of twenty-first century seismology, she has provided an informed characterization of what probably caused the quakes and what precisely happened on those fateful days. This may be what one would expect of an accomplished scholar trained in Harvard's history of science program, but Valencius has rendered the account at once more persuasive and enduring by also carefully incorporating social and religious history into the narrative.The thoughtful and perceptive introduction poses four questions she intends to answer: (1) Why did the earthquakes matter at the time they occurred? (2) If they mattered so much at the time, how could they be nearly unknown to those living in the twenty-first century? (3) How and why were the earthquakes "suddenly" rediscovered by scientists? (4) What might be made of the threat of further activity along the New Madrid fault line? Valencius shapes the volume around these crucial questions. She addresses first how the quakes were understood at the time by using one of the American frontier's most iconic figures: Davy Crockett, who claimed to have slipped into an earthquake fissure while pursuing a bear. The tale has the advantage of responding, at least in an introductory way, to two of the author's questions: How the earthquakes were understood and experienced by early nineteenth century frontiers people and the manner in which they came to be the subject of folklore. Over time, chroniclers diminished the fissure as an aspect of the tale just as the public in general lost interest in the earthquakes. Technological and agricultural innovation eradicated most of the traces leftby the earthquakes and, as modern communication reduced folk tales themselves to romantic artifacts, the earthquakes faded from the national consciousness.Even as the veracity of folk tales and oral accounts became suspect in terms of understanding both the scope and the cause of earthquakes, "two profound changes shaped the discipline of modern seismology: the instrumentalization of seismic observation in the decades surrounding the turn of the [nineteenth to twentieth] century and the reconceptualization of the earth's composition and movement" (p. …
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