Shinpukuji Temple Ruins

Japanese: 真福寺遺跡 - しんぷくじいせき

This site is located in Shinpukuji, Iwatsuki City, Saitama Prefecture, and dates from the end of the late to early final Jomon period. It is located on the left bank of the Ayase River valley, facing west at the back of a small tributary of the Iwatsuki Hills, and consists of a late shell mound on the plateau and a late peat layer in the alluvial plain at the western foot of the hill. The name Angyo-style pottery from this period comes from the Sarugai shell mound in Kawaguchi City (formerly Angyo Village), but the actual pottery type is based on the excavated materials from this shell mound, which was excavated by the Oyama Institute of Prehistory in 1926 and reported by Kono Isamu. Later, Yamauchi Kiyoo distinguished between the Angyo-2 type excavated from the shell mound and the Angyo-3 type excavated from the peat layer as late and late, and built the basis for the chronology from Angyo-1 to Angyo-3C types.

Source: Heibonsha World Encyclopedia, 2nd Edition Information

Japanese:

埼玉県岩槻市真福寺にある縄文時代後期末から晩期前半の遺跡。綾瀬川渓谷の左岸，岩槻丘陵の小支谷の奥に西面し，台地上にある後期の貝塚と，西側裾部の沖積地にある晩期の泥炭層からなる。この時期の安行（あんぎよう）式土器の名称は，川口市(旧，安行村)猿貝貝塚に由来するが，土器型式の実態は1926年に大山史前学研究所が発掘調査し，甲野勇が報告した本貝塚の出土資料を標準とする。その後山内清男は，貝塚出土の安行2式と泥炭層出土の安行3式を後期と晩期に区別し，安行1式から安行3C式にいたる編年の基礎を築いた。

出典　株式会社平凡社世界大百科事典第２版について　情報

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