...It is an alluvial plain formed by the Hii River and the Kandō River, and developed due to the changes in the course of the Hii River. Lake Jinzai in the southwest is the Kandō no Mizuumi in the Izumo no Kuni Fudoki, and there was a large amount of marshland nearby. The Hii River once flowed westward passing north of the slight elevation of Oyama in Izumo City, and alluvialized the northern part of the Kandō no Mizuumi to form the land around Taisha Town. *Some of the terminology explanations that refer to "Kamimon Suikai" are listed below. Source | Heibonsha World Encyclopedia 2nd Edition | Information |
…斐伊(ひい)川と神戸(かんど)川による沖積平野で,斐伊川の河道変遷により成長した。南西部の神西(じんざい)湖は《出雲国風土記》の神門水海(かんどのみずうみ)で,付近には沼沢地がかなり広がっていた。かつて斐伊川は出雲市小山の微高地の北を通って西流し,神門水海の北部を沖積して大社町付近の土地を形成した。… ※「神門水海」について言及している用語解説の一部を掲載しています。 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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