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Historic tsunami in Britain since AD 1000: a review

机译:自公元1000年以来英国的历史性海啸:回顾

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摘要

The British coast is not considered at particular risk from tsunami, a view that is supported by a number of recent government reports. However, these reports largely ignore some written historic records that suggest southern Britain has experienced a number of events over the past 1000 yrs. This study briefly assesses these records and recognises four groups of events: 1) sea disturbance and coastal floods in southeast England linked to earthquakes in the Dover Straits (e.g. 1382 and 1580), 2) far-field tsunami reaching the coast of the British Isles, for example, from earthquakes along the Azores-Gibraltar Fault Zone offshore Portugal (e.g. 1755), 3) tsunami associated with near-coastal low magnitude earthquakes (e.g. 1884 and 1892), and 4) a flood event in AD 1014 that has been linked to comet debris impact. The seismogenic events range from minor water disturbance, through seismic seiching, to small and 'giant' waves, suggesting near-coastal, low-magnitude, shallow earthquakes may be capable of triggering disturbance in relatively shallow water, as supported by similar occurrences elsewhere, and that the British tsunami risk requires a more careful evaluation.
机译:最近的一些政府报告都支持认为海啸对英国沿海地区没有特别的威胁。但是,这些报告在很大程度上忽略了一些书面的历史记录,这些记录表明英国南部在过去1000年中经历了许多事件。这项研究简要评估了这些记录并确认了以下四类事件:1)与多佛海峡地震(例如1382和1580)有关的英格兰东南部的海灾和沿海洪水,2)到达不列颠群岛海岸的远场海啸。例如,来自葡萄牙近海亚速尔群岛-吉布拉塔尔断裂带的地震(例如1755年),3)与近沿海低级地震相关的海啸(例如1884年和1892年)以及4)公元1014年的洪水事件与彗星碎片撞击有关。地震事件的发生范围从轻微的水扰动到地震波,再到小而“巨大”的波,这表明近岸,低震级的浅层地震可能能够在相对浅层的水中引发扰动,其他地方也发生了类似的事件,英国海啸风险需要更仔细的评估。

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