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首页> 外文期刊>地球科学 >北海道奧尻島沿岸の奇岩の地質環境とその伝説?伝承
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北海道奧尻島沿岸の奇岩の地質環境とその伝説?伝承

机译:北海道的地质环境及其北海道海岸的传说?

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摘要

Various oddly-shaped rocks on the coast of Okushiri Island in southwestern Hokkaido are examined based upon field geology and folklore literature. Characteristic twelve geosites of the island are described with their geology and chronostratigraphy, and determined geological attributions of oddly-shaped rocks. Based on chronostratigraphy, oddly-shaped rocks of Okushiri Island are divided into three horizons, i.e. Cretaceous, middle Miocene and lower Pliocene, in ascending order. The Cretaceous horizon is characterized by Mottate Iwa Rock (granodiorite) after block weathering and wave erosion. The Miocene horizon is represented by Cape Inaho and Benten, which are made of intrusions of volcanic rocks in the Tsurikake Formation after differential weathering and erosion. The Pliocene horizon is characterized by Nabetsuru Iwa, Hoya Ishi and Kabuto Iwa Rocks, which are composed of intrusions of volcanic rocks in the Hotokezawa and Yoneoka Formations after differential weathering and erosion. Folklore of oddly-shaped rocks in Okushiri Island are mainly local origin, but some folklore is related to the legend of Yoshitsune.
机译:基于现场地质和民间传说文学,检查了北海道西南部霍富里岛海岸的各种奇怪的岩石。岛屿的特征十二型地质学描述了它们的地质和计时到图书馆,以及奇形岩石的确定地质归因。基于计时,奥什什里岛的奇怪形状的岩石分为三个视野,即按升序。白垩纪地平线的特点是嵌入风化和波浪侵蚀后的斑驳IWA岩石(Granodiorite)。内科海平植物由海角Inaho和Benten代表,这是由琐静的风化和侵蚀后Tsurikake地层的火山岩的入侵。 Pliocene Horizo​​ n的特点是Nabetsuru Iwa,Hoya Ishi和Kabuto Iwa Rocks,这些岩石由差动风化和侵蚀后的Hotokawa和Yoneoka地层中的火山岩的入侵组成。 Okushiri岛的奇怪形状的岩石民俗主要是局部起源,但是一些民间传说与Yoshitsune的传说有关。

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