夏威夷群岛东莫洛卡岛Honoko 'i Gulch新发现的玄武岩Adze采石场

IF 1.4 3区 地球科学 0 ARCHAEOLOGY
Patrick V. Kirch, Jillian A. Swift, Kepa Lyman, Greg Solatorio, Kylie Tuitavuki, Steven Lundblad, Peter Mills
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引用次数: 0

摘要

到目前为止,莫洛卡伊岛东部还没有采石场,人们认为西莫洛卡伊岛上的Kaluako 'i采石场向东莫洛卡伊社区提供了adze材料。在这里,我们报道了在岛东端Hālawa山谷附近的Honoko 'i Gulch的一个主要采石场的鉴定。暴露在巨大悬崖中的细粒玄武岩(技术上是夏威夷-mugearite)被提取出来,并在采石场本身以及几个剥落区被还原成扁坯。对采石场材料的EDXRF分析表明,它与先前在Hālawa沙丘遗址分析的A组玄武岩碎屑相同,表明Honoko 'i采石场是Hālawa山谷居民的重要adze材料来源。从火野古岛和Hālawa沙丘遗址的放射性碳年代测定表明,采石场早在公元1366-1610年就开始使用了。采石场本身的一个不寻常的特征是存在几个拟人化的岩画。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Newly Identified Basalt Adze Quarry at Honoko‘i Gulch, East Moloka‘i, Hawaiian Islands

To date, no quarries were known on the eastern part of Moloka‘i Island, and it was assumed that the Kaluako‘i quarries on West Moloka‘i supplied the East Moloka‘i communities with adze material. Here, we report on the identification of a major quarry at Honoko‘i Gulch, near Hālawa Valley at the island's eastern tip. Fine-grained basalt (technically hawaiite-mugearite) exposed in a massive cliff was extracted and reduced to adze preforms at the quarry itself as well as at several flaking areas. EDXRF analysis of the quarry material demonstrates that it is identical to the Group A basalt debitage previously analyzed at the Hālawa Dune Site, indicating that the Honoko‘i quarry was a significant source of adze material for the occupants of Hālawa Valley. Radiocarbon dates from Honoko‘i and from the Hālawa Dune Site indicate that the quarry was in use from as early as AD 1366–1610. An unusual feature at the quarry itself is the presence of several anthropomorphic petroglyphs.

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来源期刊
Geoarchaeology-An International Journal
Geoarchaeology-An International Journal 地学-地球科学综合
CiteScore
3.60
自引率
5.90%
发文量
51
审稿时长
>12 weeks
期刊介绍: Geoarchaeology is an interdisciplinary journal published six times per year (in January, March, May, July, September and November). It presents the results of original research at the methodological and theoretical interface between archaeology and the geosciences and includes within its scope: interdisciplinary work focusing on understanding archaeological sites, their environmental context, and particularly site formation processes and how the analysis of sedimentary records can enhance our understanding of human activity in Quaternary environments. Manuscripts should examine the interrelationship between archaeology and the various disciplines within Quaternary science and the Earth Sciences more generally, including, for example: geology, geography, geomorphology, pedology, climatology, oceanography, geochemistry, geochronology, and geophysics. We also welcome papers that deal with the biological record of past human activity through the analysis of faunal and botanical remains and palaeoecological reconstructions that shed light on past human-environment interactions. The journal also welcomes manuscripts concerning the examination and geological context of human fossil remains as well as papers that employ analytical techniques to advance understanding of the composition and origin or material culture such as, for example, ceramics, metals, lithics, building stones, plasters, and cements. Such composition and provenance studies should be strongly grounded in their geological context through, for example, the systematic analysis of potential source materials.
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