A limestone stratum distributed widely from the central to southern parts of the Ryukyu Islands. It originated from a coral reef in the Quaternary Pleistocene of the Cenozoic Era. It accounts for about 30% of the total area of Okinawa Prefecture, forming plateaus and capes. It has been used as a building material since ancient times, and can be seen in Shuri Castle and the stone-paved roads. Source: About Shogakukan Digital Daijisen Information | Legend |
南西諸島の中部から南部にかけて広く分布する石灰岩の地層。新生代第四紀更新世のサンゴ礁に起源する。沖縄県では総面積の約3割を占め、台地や岬などを形成する。古くから建材として利用され、首里城や石畳の道などで見られる。
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