…Of these, the Asahi Mountains, with their high-level low-relief surfaces at an altitude of 1,200 to 1,600 meters, are relics of the peneplain mentioned above, and Mt. Asahi, which protrudes a level higher than that, is thought to be a remnant hill. In addition, at an altitude of about 600 meters, there is an Eck bed (a ridge between two confluent rivers, a type of river terrace) with fresh riverbed gravel, which indicates that the uplift of the mountains continued until very recently. *Some of the terminology that refers to the "ECK bed" is listed below. Source | Heibonsha World Encyclopedia 2nd Edition | Information |
…そのうち,標高1200~1600mの高位小起伏面群をもつ朝日山地主部は,前記の準平原の遺物を残し,それより一段と高く突出する朝日岳は残丘と考えられる。また,標高600mほどのところに新鮮な河床礫(かしようれき)をのせるエック床(合流河間山稜面。河岸段丘の一種)があり,山地の隆起運動がごく最近まで続いていることを示す。… ※「エック床」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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