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Communities and catastrophe: Tillamook response to the AD 1700 earthquake and tsunami, northern Oregon coast.

机译:社区与灾难:蒂拉穆克(Tillamook)对公元1700年地震和俄勒冈州北部海啸的反应。

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摘要

Since Euro-American settlement, the southern Northwest Coast of North America has not experienced a large magnitude earthquake. An extensive body of geological evidence, however, suggests large earthquakes have repeatedly struck the region throughout the Holocene. The Cascadia Subduction Zone, an area of converging tectonic plates off the southern British Columbia, Washington, Oregon, and northern California coasts, generates these earthquakes, causing subsidence of coastal lands and producing large tsunamis. The most recent earthquake and tsunami occurred in January, AD 1700. I examine the effects of these events on the Tillamook people and environments of Netarts and Nehalem bays, now located in Tillamook County, Oregon.;Archaeologists have suggested that the AD 1700 earthquake and tsunami caused destruction and abandonment of Native settlements, disturbed shellfish and fish populations upon which people relied, and altered coastal landscapes. Earthquakes and tsunamis have been portrayed as catastrophes for Native peoples. To assess Tillamook susceptibility to these natural hazards, I evaluate the ethnohistoric and ethnographic records of Netarts and Nehalem bays. I also analyze oral traditions of earthquakes and tsunamis from the southern Northwest Coast to assess Native perceptions, explanations, and responses to these hazards. This study is the first to involve archaeological fieldwork designed to assess the effects of Cascadia earthquakes and tsunamis on Native peoples. Sites occupied around AD 1700 on Netarts and Nehalem bays were investigated to refine their chronologies of occupation and gather information about subsistence and landscape changes. I also reexamined previously excavated materials from two sites on Netarts Bay.;I suggest that the AD 1700 earthquake and tsunami were not completely disastrous for Tillamook communities of Netarts and Nehalem bays. Radiocarbon dates provide little evidence for the sites' abandonment following the earthquake and tsunami. Faunal data from Netarts Bay suggest that small fish, mussels, and terrestrial mammals were more intensively used following the earthquake. At Nehalem Bay, people continued to rely heavily on salmon after AD 1700. People at both estuaries continued to occupy low elevation, hazardous areas following the earthquake and tsunami. Southern Northwest Coast peoples and coastal environments may have been more resilient to these hazards than previously portrayed.
机译:自从欧洲人定居以来,北美南部西北海岸就没有经历过大地震。但是,大量的地质证据表明,整个全新世地区都多次发生大地震。卡斯卡迪亚俯冲带(Cascadia Subduction Zone)是不列颠哥伦比亚省南部,华盛顿州,俄勒冈州和北加利福尼亚海岸附近汇聚的构造板块区域,引发了这些地震,造成了沿海土地的沉陷并产生了大量海啸。最近的地震和海啸发生于公元1700年1月。我考察了这些事件对现在位于俄勒冈州蒂拉穆克县的提拉穆克人和Netarts和Nehalem海湾环境的影响;考古学家建议公元1700年的地震和海啸造成了土著居民定居点的破坏和遗弃,扰乱了人们赖以生存的贝类和鱼类种群,并改变了沿海地貌。地震和海啸已被描绘成土著人民的灾难。为了评估Tillamook对这些自然灾害的敏感性,我评估了Netarts和Nehalem海湾的民族历史和人种志记录。我还分析了西北西北部南部地区地震和海啸的口头传统,以评估当地人对这些灾害的看法,解释和应对措施。这项研究是第一个涉及旨在评估卡斯卡迪亚地震和海啸对土著人民影响的考古野外工作的机构。对Netarts和Nehalem海湾在公元1700年左右占领的场地进行了调查,以完善其占用时间,并收集有关生存和景观变化的信息。我还重新检查了内塔特斯湾两个地点以前发掘的材料。我建议,公元1700年的地震和海啸对内塔特斯和尼哈莱姆湾的提拉穆克社区来说并不是完全灾难性的。放射性碳日期几乎没有证据表明该地点在地震和海啸后被遗弃。 Netarts湾的动物数据表明,地震后对小鱼,贻贝和陆生哺乳动物的使用更为密集。在Nehalem湾,公元1700年以后,人们继续严重依赖鲑鱼。两个河口的人们在地震和海啸之后仍处于低海拔,危险地区。西北海岸南部的人民和沿海环境可能比以前描述的更具抵抗力。

著录项

  • 作者

    Losey, Robert Justin.;

  • 作者单位

    University of Oregon.;

  • 授予单位 University of Oregon.;
  • 学科 Archaeology.
  • 学位 Ph.D.
  • 年度 2002
  • 页码 636 p.
  • 总页数 636
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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