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Byōbugaura
is an inlet on the northeast coast of Chiba Prefecture that ranges from Cape Inubō in Chōshi to Cape Gyōbumi in Asahi. Byōbugaura is an important part of the coastal area in Chiba Prefecture, as it connects the northern point of the Pacific Ocean coast at Chōshi to Kujūkuri Beach, which covers a large portion of the western side of the prefecture. The name of the inlet is formed from the word "byōbu", the Japanese-style folding screen, and "ura", meaning an inlet. Byōbugaura resembles the White Cliffs of Dover on the English Channel. For this reason the inlet is sometimes called , or "Dover of the East."〔()〕 Byōbugaura is known for its long history of marine erosion.
==Description==
Byōbugaura spans approximately , with precipitous cliffs that reach an altitude of . Three strata are clearly visible on the cliffs of the inlet: the reddish Kantō Loam Stratum at the top, the Katori Statum in the middle, the chalky-white Iioka Stratum prominently on the cliff face, and the Naarai Stratum at the base. The Kantō Loam Stratum is red and is composed of material from volcanic eruptions of Mount Fuji and Mount Hakone, and the white portions of the cliff face consist of easily eroded clay.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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