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Nature Trail of Michinoku Coastal Trail - Sanriku Geo-Park
Sannoiwa的点评
点评：The ria coastline is shaped by steep cliffs and offshore rock formations of various sizes. Nature shaped these rocks by erosion over 10,000 years by waves and winds from strata that are 100 million years old . The rock surface of sandstone and conglomerate formed during the Cretaceous period (~ .100 million years ago). they serve as a breeding ground for the black-tailed gull,
It consists of three giant rocks including 50-meter-high Otoko-iwa (male rock) in the center, Onna-iwa (female rock) on the left and Taiko-iwa (drum rock) on the right. It shows horizontal stripes of sandstone and conglomerate strata. The cove which has the port of Kawamukai was hit by the tsunami caused the earthquake of 11th March 2011 of 9.1 magnitude which occurred 80 miles off the coast. The rocks can be approached from above or below by a steep path.
It consists of three giant rocks including 50-meter-high Otoko-iwa (male rock) in the center, Onna-iwa (female rock) on the left and Taiko-iwa (drum rock) on the right. It shows horizontal stripes of sandstone and conglomerate strata. The cove which has the port of Kawamukai was hit by the tsunami caused the earthquake of 11th March 2011 of 9.1 magnitude which occurred 80 miles off the coast. The rocks can be approached from above or below by a steep path.
翻译：里亚海岸线由陡峭的悬崖和各种大小的近海岩层形成。大自然通过 10,000 多年的海浪和风对已有 1 亿年历史的地层进行侵蚀，塑造了这些岩石。砂岩和砾岩的岩石表面形成于白垩纪（约 1 亿年前）。它们是黑尾鸥的繁殖地，
它由三块巨石组成，包括中间 50 米高的男岩（雄岩）、左侧的女岩（雌岩）和右侧的太鼓岩（鼓岩）。它显示出水平条纹的砂岩和砾岩地层。2011 年 3 月 11 日，距离海岸 80 英里的 9.1 级地震引发的海啸袭击了川向港所在的海湾。可以通过一条陡峭的小路从上方或下方接近岩石。
它由三块巨石组成，包括中间 50 米高的男岩（雄岩）、左侧的女岩（雌岩）和右侧的太鼓岩（鼓岩）。它显示出水平条纹的砂岩和砾岩地层。2011 年 3 月 11 日，距离海岸 80 英里的 9.1 级地震引发的海啸袭击了川向港所在的海湾。可以通过一条陡峭的小路从上方或下方接近岩石。
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