4.6 Article

Bridging Legends and Science: Field Evidence of a Large Tsunami that Affected the Kingdom of Tonga in the 15th Century

期刊

FRONTIERS IN EARTH SCIENCE
卷 9, 期 -, 页码 -

出版社

FRONTIERS MEDIA SA
DOI: 10.3389/feart.2021.748755

关键词

tsunami; megablock; sedimentology; radiocarbon dating; bioclasts; legend; southwest Pacific

资金

  1. French National Agency for Research [ANR11-LABX-0046]
  2. Laboratory of Physical Geography, UMR 8591 CNRS-Paris 1-UPEC
  3. Tongan Ministry of Land and Natural Resources, Natural Resources Division
  4. Institut Universitaire de France
  5. VEILA project H2020-MSCA-IF-2017

向作者/读者索取更多资源

Despite significant scientific advances in recent years, the pre-colonial history of Tonga and West Polynesia before the 16th century still has major gaps. In the 14th century, the powerful Tu'i Tonga kingdom united the islands under central authority, but by the mid-15th century, they faced deep crisis possibly linked to a large tsunami event.
The pre-colonial history (i.e. before the 16th century) of Tonga and West Polynesia still suffers from major gaps despite significant scientific advances in recent years, particularly in the field of archaeology. By the 14th century, the powerful Tu'i Tonga kingdom united the islands of the Tongan archipelago under a centralised authority and, according to tradition, extended its influence to neighbouring island groups in the Central Pacific. However, some periods of deep crisis were identified, e.g. in the mid- 15th century, marked by an abrupt cessation of inter-archipelago migration on the deep seas in the Pacific, significant cultural changes, and a decrease in accessible natural resources. The origins of these disturbances are still debated, and they are usually assigned to internal political problems or loss of external influence vis-a-vis neighboring chiefdoms. However, the hypothesis of a major natural disaster was rarely suggested up to now, while field evidence points to the occurrence of a very large tsunami in the past, including the presence of numerous megablocks that were deposited by a red wave (or peau kula, which also mean tsunami in the Tongan language) according to a local myth. Drawing on a body of new evidence from sedimentary signatures and radiocarbon dating of charcoal and marine bioclasts, geomorphology, and sedimentology, in support of previously published archaeological data, we argue that a large tsunami inundated large areas of Tongatapu island in the mid-15th century with runup heights up to 30 m, and that the Tu'i Tonga kingdom was severely impacted by this event. We also discuss the likely sources of this tsunami.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.6
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据