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首页> 外文期刊>Quaternary International >Combining historical and C-14 data to assess pyroclastic density current hazards in Banos city near Tungurahua volcano (Ecuador)
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Combining historical and C-14 data to assess pyroclastic density current hazards in Banos city near Tungurahua volcano (Ecuador)

机译:结合历史数据和C-14数据,评估通古拉瓦火山(厄瓜多尔)附近巴尼奥斯市的火山碎屑流密度危害

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摘要

Pyroclastic density currents (PDCs) from Tungurahua volcano, Ecuador, recurrently rush down the northern Vazcun valley and threaten the small tourist city of Banos located on its mouth. Estimating PDC hazards, i.e. PDC return rate and extent, is difficult in Banos and Vazcun because data from the literature are rare and debated, while geological exposures are few and vegetated. To improve our awareness of PDC hazards in the Banos area, we examined historical documents, conducted new geological research in the Vazcun valley, and obtained additional C-14 data. We highlight complex radiocarbon results that may lead to difficulties when interpreting the PDC chronology, and offer recommendations to improve sampling strategies for C-14 age determinations of PDC deposits. Overall, our results show that the 1640, 1773, and 1886 PDC-forming eruptions are recorded in the valley, while products of the 1918 and 2006 events were likely removed. Through considering recorded/unrecorded bias in the reconstruction of past PDC emplacement in Vazcun, we calculate a minimal average return rate of 18 PDC-forming events for pre-Columbian and historical eruptions since the devastating 3 ka BP eruption, which translates into a maximum average return rate of 150-200 years in the valley. However, the archives suggest that most PDCs did not affected the now-urbanized Banos area (e.g. 1918, 2006) and we estimate that the city is impacted on average every 350-500 years, a duration that is likely perceived as fairly long for people living in the area. The Banos case-study thus raises questions on how to communicate on uncertain threats and impacts, and how to improve alert messages in a town where economic incomes are essentially based on tourist activities. To better address these issues we plan in future works to focus on cognitive perception of risk and volcanic hazard judgment by populations of Banos and nearby rural communities. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:来自厄瓜多尔通古拉瓦火山的火山碎屑密度流(PDC)反复涌入北部的Vazcun山谷,并威胁到位于其嘴上的小型旅游城市Banos。在Banos和Vazcun中,难以估计PDC危害,即PDC的返还率和程度,因为文献中的数据很少且存在争议,而地质暴露很少且植被茂盛。为了提高我们对Banos地区PDC危害的认识,我们检查了历史文献,在Vazcun山谷进行了新的地质研究,并获得了其他C-14数据。我们重点介绍了复杂的放射性碳结果,这些结果可能会在解释PDC年代学时带来困难,并提供建议,以改善PDC沉积物C-14年龄确定的采样策略。总体而言,我们的结果表明,山谷中记录了1640、1773和1886年形成PDC的喷发,而1918年和2006年事件的产物很可能已被清除。通过考虑瓦兹村过去PDC安置重建中记录的/未记录的偏差,我们计算了自毁灭性的3 ka BP喷发以来,哥伦布前和历史性喷发的18个PDC形成事件的最小平均回报率,这转化为最大平均谷地的回报率是150-200年。但是,档案表明,大多数PDC都没有影响到现已城市化的Banos地区(例如1918年,2006年),并且我们估计该城市平均每350-500年受到影响,这一持续时间对人们来说可能相当长生活在该地区。因此,Banos案例研究提出了一个问题,即如何在不确定的威胁和影响方面进行沟通,以及如何在经济收入主要基于游客活动的城镇中改善警报信息。为了更好地解决这些问题,我们计划在未来的工作中重点关注巴诺斯人和附近农村社区对风险和火山危害判断的认知。 (C)2015 Elsevier Ltd和INQUA。版权所有。

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