Omote Myogi

...The mountain has been severely eroded, and the location of the eruption center of the volcanic rocks and the original topography are completely unknown, so it is inappropriate to call it a volcano. There are two parts to Myogi: Omote Myogi, which has a sawtooth ridge extending from Mt. Kondo (1,104m) to Mt. Hakuun (1,081m) to the northeast and Mt. Kinkei (856m) to the southwest, and Ura Myogi, which stretches from Mt. Yakiyu (1,162m) to Mt. Sendagi (997m). Omote Myogi in particular is called Mt. Myogi. On the steep mountainside, strangely shaped rocks called stone pillars, stone gates, and cannon rocks can be seen, and in autumn, when the entire mountain is colored with autumn leaves, the scenery is outstanding.

*Some of the terminology explanations that refer to "Omote Myogi" are listed below.

Source | Heibonsha World Encyclopedia 2nd Edition | Information

…山体は激しく浸食され，火山岩の噴出中心位置や原地形がまったく不明で，火山と呼ぶのは不適当である。金洞（こんどう）山(1104m)から北東に白雲山(1081m)，南西に金鶏山(856m)と鋸歯状の尾根が連なる表妙義と，谷急（やきゆう）山(1162m)から千駄木山(997m)に至る裏妙義があるが，とくに表妙義を妙義山という。急峻な山腹には石柱，石門，大砲岩などと呼ばれる奇岩怪石が見られ，全山が紅葉に彩られる秋の景観にすぐれる。…

※「表妙義」について言及している用語解説の一部を掲載しています。

出典｜株式会社平凡社世界大百科事典 第２版について | 情報