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・ Rikuzen-Tomiyama Station
・ Rikuzen-Toyosato Station
・ Rikuzen-Yachi Station
・ Rikuzen-Yahagi Station
・ Rikuzen-Yamashita Station
・ Rikuzen-Yokoyama Station
・ Rikuzen-Ōtsuka Station
・ Rikuzentakata mayoral election, 2007
・ Rikuzentakata, Iwate
・ Riky Rick
・ Riky Widianto
・ Rikyu (film)
・ Rikyū
・ RIL
・ Ril Lake (Ontario)
Rila
・ Rila (disambiguation)
・ Rila Fukushima
・ Rila Monastery
・ Rila Monastery Nature Park
・ Rila motorway
・ Rila Municipality
・ Rila National Park
・ Rila Point
・ Rila, Bulgaria
・ Rila, Tibet
・ Rilaena
・ Rilaena triangularis
・ Rilakkuma
・ Rilamulla


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Rila : ウィキペディア英語版
Rila

Rila ((ブルガリア語:Рила), ) is a mountain range in southwestern Bulgaria and the highest mountain range of Bulgaria and the Balkans, with its highest peak being Musala at 2,925 m. The massif is also the sixth highest mountain in Europe (when each mountain is represented by its highest peak only), coming after the Caucasus, the Alps, Sierra Nevada, the Pyrenees and Mount Etna, and the highest between the Alps and the Caucasus. More than one-third of the mountain is occupied by the Rila National Park, the rest lies within the Rila Monastery Nature Park.
The name ''Rila'' is believed to be of Thracian origin and is thought to mean "well-watered mountain", owing to Rila's abundance of glacial lakes (about 200) and hot springs in fault areas at the base of the mountain. Some of the Balkans' longest and deepest rivers originate from Rila, including the Maritsa, the Iskar and the Mesta.
Culturally, Rila is famous for the Rila Monastery, Bulgaria's largest and most important monastery, founded in the 10th century by Saint John of Rila. Alongside the cultural landmarks the mountain is also famous for the Seven Rila Lakes.
==Geology==
Rila is a dome-shaped horst mountain, part of the Balkans' oldest land, the Macedono-Thracian Massif. It was formed by granite and gneiss rocks and crystal schists during the Paleozoic (250,000,000 years ago). Rila's alpine relief was formed during the Pleistocene by a series of glacial periods. During the most recent, so-called Würm glaciation, 10-12,000 years ago the permanent snow line was at 2,100 m above sea level. Above this line glaciers radically changed the existing relief, carving out deep cirques, sharp pyramid-shaped peaks, rock pinnacles, various valleys, moraines and other typical glacial formations.

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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