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ルソン島北部、カガヤン川下流域の貝塚遺跡に見られる居住の断絶と継続 : 河川の氾濫との関連で
https://keiai.repo.nii.ac.jp/records/1698
https://keiai.repo.nii.ac.jp/records/1698240b7781-c4e7-4579-9b91-854c50cab029
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
KJ00004271090.pdf (1.3 MB)
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| Item type | [ELS]紀要論文 / Departmental Bulletin Paper(1) | |||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2016-08-18 | |||||||||||
| タイトル | ||||||||||||
| タイトル | ルソン島北部、カガヤン川下流域の貝塚遺跡に見られる居住の断絶と継続 : 河川の氾濫との関連で | |||||||||||
| タイトル | ||||||||||||
| タイトル | The Continuity and the Discontinuity of the Occupation of the Shell-midden Sites in the Lower Reaches of the Cagayan River, Northern Luzon : with the Relation to Floods of the Cagayan River | |||||||||||
| 言語 | en | |||||||||||
| 言語 | ||||||||||||
| 言語 | jpn | |||||||||||
| 資源タイプ | ||||||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||||
| 資源タイプ | departmental bulletin paper | |||||||||||
| 雑誌書誌ID | ||||||||||||
| 収録物識別子タイプ | NCID | |||||||||||
| 収録物識別子 | AN1041551X | |||||||||||
| 著者 |
田中, 和彦
× 田中, 和彦
× TANAKA, Kazuhiko
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| 抄録(英) | ||||||||||||
| 内容記述タイプ | Other | |||||||||||
| 内容記述 | There are two objectives in this article. The First is to clarify the relationship between floods and the sites in the lower reaches of the Cagayan River. The second is to clarify the correlation of two sites in this area. For these objectives, I used the data obtained by the excavations of two shell-midden sites at the different locations: the Catugan Shell-midden Site (Tanaka 1998a) on the natural riverbank and the Magapit Shell-midden Site (Aoyagi, Aguilera, Ogawa and Tanaka 1989, 1991) on the limestone hill in the lower reaches of the Cagayan River. The analyses of the excavated data revealed the following facts: 1. The pottery of Layer V of the Catugan Shell-midden Site and the pottery of the upper part of Layer V of the Magapit Shell-midden Site are almost contemporaneous on the basis of the typological analysis of the pottery of both sites. 2. The soil of Layer V of the Catugan Shell-midden Site is the clay partially containing the silt. 3. Layer IV of the Catugan Shell-midden Site and the pottery of Layer V o the same site are typologically totally different. Layer IV mainly contain the black pottery and the brown pottery. Meanwhile, Layer V mainly contains the red-slipped pottery. 4. The pottery from the lower part of Layer V to Layer II of the Magapit Shell-midden Site is typologically continuous. 5. The Catugan Shell-midden Site is located on the natural riverbank. The level of the site is about 10 meters above the mean sea level. On the other hand, the Magapit Shell-midden Site is located on the limestone hill. The level of the site is about 48 meters above the mean sea level. On the basis of these facts, it is certain that the Catugan Shell-midden Site was abandoned during the period marked by the red-slipped pottery, probably because of the flood. Meanwhile, it is also certain that the Magapit Shell-midden Site was continuously occupied after abandonment of the Catugan Shell-midden Site. It is probable that the Magapit Shell-midden Site is one of the places where the people, who had abandoned the Catugan Shell-midden Site (Layer V) by the flood, transferred. | |||||||||||
| 書誌情報 |
環境情報研究 en : Journal of Environmental Studies 号 11, p. 83-99, 発行日 2003-04-30 |
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