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Mycale (). also Mykale and Mykali (), called Samsun Daği and Dilek Daği (Dilek Peninsula) in modern Turkey, is a mountain on the west coast of central Anatolia in Turkey, north of the mouth of the Maeander and divided from the Greek island of Samos by the 1.6 km wide Mycale Strait. The mountain forms a ridge, terminating in what was known anciently as the Trogilium promontory (Ancient Greek Τρωγίλιον or Τρωγύλιον).〔. Downloadable Google Books.〕 There are several beaches on the north shore ranging from sand to pebbles. The south flank is mainly escarpment. In classical Greece nearly the entire ridge was a promontory enclosed by the Aegean Sea. Geopolitically it was part of Ionia with Priene placed on the coast on the south flank of the mountain and Miletus on the coast opposite to the south across the deep embayment into which the Maeander River drained. Somewhat further north was Ephesus. The ruins of the first two Ionian cities mentioned with their harbor facilities remain but today are several miles inland overlooking instead a rich agricultural plain and delta parkland created by deposition of sediments from the river, which continues to form the geological feature named after it, maeanders. The end of the former bay remains as a lake, Çamiçi Gölü (Lake Bafa). Samsun Daği does retain a promontory. The entire ridge was made into a national park of , Dilek Yarimadisi Milli Parki ("Dilek Peninsula National Park") in 1966, which is in part accessible to the public. The remainder is a military reservation. The park's isolation has encouraged the return of the native ecology, which is 60% maquis. It is a refuge for species that formerly were more abundant in the region. == Geophysics == Western Turkey is mainly fault-block terrain with steep-sided ridges running east-west and rivers in the rifts. The source of the faulting is the closing of Tethys Sea and the collision of the African and Arabian plates with the Eurasian plate. The smaller Turkish and Aegean plates are being pushed together, generating ridges in Turkey. This orogenic belt was in place by 1.6 mya and continues to be a hot spot of earthquakes and volcanos. Mount Mycale is part of a larger ridge, which continues in Samos on the other side of the Samos Strait, and to the northeast in the Aydin Dağlari ("Aydin Mountains"), ancient Messogis range, on the other side of low hills and passes. The entire block of mountains around the Menderes (Maeander) River is the Menderes Massif. Mycale is scored transversely by numerous ravines through which sources drain. The biggest ravine is Oluk Gorge, with cliffs high. The main permanent streams are the Bal Deresi, the Sarap Dami and the Oluk Dereleri. The ample water supply supports a verdant maquis. The rock is primarily metamorphic: marble and limestone formed from rocks originating in the Mesozoic,crystalline schists formed from rocks originating in the Palaeozoic and conglomerates of the Cenozoic. These materials were not wasted on the renowned builders and sculptors of Ionia. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Mycale」の詳細全文を読む スポンサード リンク
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