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A 1,000-year sediment record of tsunami recurrence in northern Sumatra

机译:苏门答腊北部1000年海啸复发的沉积记录

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The Indian Ocean tsunami of 26 December 2004 reached maximum wave heights of 35 m in Aceh, the northernmost province of Sumatra. Both the tsunami and the associated Sumatra-Andaman earthquake were unprecedented in Acehnese history. Here we use sand sheets to extend tsunami history 1,000 years into Aceh's past. The 2004 tsunami deposited a sand sheet up to 1.8 km inland on a marshy beach ridge plain. Sediment cores from these coastal marshes revealed two older extensive sand sheets with similar sediment characteristics. These sheets, deposited soon after ad 1290-1400 and ad 780-990, probably resulted from earlier tsunamis. An additional sand sheet of limited extent might correlate with a documented smaller tsunami of ad 1907. These findings, a first step towards a palaeotsunami record for northern Sumatra, suggest that damage-causing tsunamis in Aceh recur infrequently enough for entire human lifetimes to typically elapse between them. Such recurrence adds to the challenge of preparing communities along the northern Indian Ocean shorelines for future tsunamis.
机译:2004年12月26日的印度洋海啸在苏门答腊最北部的省亚齐达到了35 m的最大波高。海啸和相关的苏门答腊-安达曼地震在阿塞罕历史上都是史无前例的。在这里,我们使用砂纸将海啸的历史延伸到亚齐的过去1000年。 2004年的海啸在一块湿s的海滩山脊平原上向内陆沉积了高达1.8公里的沙子。这些沿海沼泽地带的沉积物岩心显示出两个较早的粗砂岩,具有相似的沉积物特征。这些纸页是在广告1290-1400和广告780-990之后不久存放的,可能是早期海啸造成的。另外一个范围有限的沙层可能与1907年有记载的较小海啸有关。这些发现是苏门答腊北部古海啸记录的第一步,表明亚齐省引起破坏性海啸的发生频率不高,足以使整个人类一生消失它们之间。这种复发增加了在印度洋北部海岸线上为未来海啸做好准备的准备工作的挑战。

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