海洋理工学会誌
Online ISSN : 2188-3262
Print ISSN : 1341-2752
ISSN-L : 1341-2752
原著
物理探査による沖縄西表島網取遺跡地域の地下構造
馬場 久紀, 北條 芳隆, 上野 信平
著者情報
ジャーナル フリー

2009 年 15 巻 2 号 p. 159-171

詳細
抄録
As a part of studies for the Amitori remains, we carried out recently the seismic and electrical explorations in Iriomote Island, southwestern Okinawa prefecture. Amitori village was finally abandoned in 1971. because of its imperfect infrastructures. At present, however, there only exists one institution, the Okinawa Regional Research Center of Tokai University. Archaeological explorations in the Amitori area have already been made several times and many relics of the past were dug out within a 1.5-2.0 m thick surface layer. This is the first attempt to apply geophysical (seismic refraction and electrical resistivity) methods to the Amitori area in order to make clear a detailed shallow structure down to the depths of 10m or so. We selected three main survey lines with the lengths of about 100-150 m. two of which locating within the central part of village and the other in a nearby rice field. The results obtained are summarized as follows; (1)The most suitable seismic model of the underground structure in this area is composed of four layers. These are, the surface layer (sand), 2nd (sand stone), 3rd (mud stone), and 4th (sandy shale) layers, continuously. The distribution patterns of electrical resistivity are harmonized strongly with the seismic model. Moreover low resistivity zones may be inferred as to be connected with groundwater distribution. (2)The thickness of surface layer is presumed as about 2.0 m uniformly within the whole area of Amitori village. In the archaeological surveys most of the relics are found in the surface zone within 1.5-2.0 m thickness, consequently all relics being buried in the first layer. (3)Generally it is difficult to discriminated directly on the location and, or shape of buried relics using simply the seismic on electrical method, but it must be easy to make clear on the form or boundary of surface layer as an object of archaeological surveys. Therefore the present results obtained by geophysical techniques may play an important role in the archaeological studies of Amitori remains. Iriomote Island. SW Okinawa.
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