Tu banner alternativo

Mount Azumaya

Nowadays, Mount Azumaya is a topic that is on everyone's lips and that has gained great relevance in today's society. From its origins to the present, Mount Azumaya has been the object of interest and debate, generating multiple opinions and positions on the matter. In this article, we will explore in depth all aspects related to Mount Azumaya, analyzing its implications, repercussions and possible solutions. From a critical and objective perspective, we will approach this topic from different angles, with the aim of shedding light on its importance and influence on our daily lives. Along the following lines, we will delve into the fascinating world of Mount Azumaya, discovering its impact in different fields and its role in shaping the reality that surrounds us.

Tu banner alternativo
Mount Azumaya
四阿山
Highest point
Elevation2,354 m (7,723 ft)
Listing100 Famous Japanese Mountains
Coordinates36°32′30″N 138°24′47″E / 36.54167°N 138.41306°E / 36.54167; 138.41306
Naming
English translationarbour mountain
Language of nameJapanese
Pronunciation[azumajasaɴ]
Geography
Geology
Mountain typeStratovolcano
Climbing
Easiest routeHike
Relief Map

Mount Azumaya (四阿山, Azumaya-san) is a stratovolcano in Japan. The 2,354-metre-high (7,723 ft) peak lies on the border of Nagano Prefecture and Gunma Prefecture. There exist alternative spellings of the mountain's name, like: 吾妻山 and 吾嬬山 which is read as "Agatsuma-yama" (Mount Agatsuma). In the village Tsumagoi, the mountain is spelled 吾妻山.

The mountain should not be confused with Mount Azumaya (四阿屋山, Azumaya-san) of which there are two, one in Nagano Prefecture and the other in Saitama Prefecture. Though the reading is the same, the name written in Kanji differs from the mountain in this article.

Outline

Mount Azumaya was formed between 900,000 and 300,000 years ago by andesite lava flowing out of a stratovolcano. An eruption 340,000 years ago formed a caldera of circa 3 kilometers in diameter. Through erosion the mountain has arrived at its present form with several peaks. Azumaya Volcano (四阿火山, Azumaya-kazan) is the general term for the following peaks lying roughly on a circle: Mount Neko (根子岳, Neko-dake), Mount Azumaya, Mount Urakura (浦倉山, Urakura-yama), Mount Kimyō (奇妙山, Kimyō-san).

The famous Sugadaira Kōgen ski area is found on the mountain's southwest (Nagano-) side. Also on the Gunma-side there exists a ski area. In addition, north of the mountain lies Yonakodaibakufu (米子大瀑布) which is one of Japan's Top 100 Waterfalls.

Main ascent routes

The mountain is well connected with several hiking trails:

  • Sugadai-bokujō (菅平牧場) - Mount Neko (根子岳, Neko-dake) - Mount Azumaya
  • Azumaya Kōgen (四阿高原) - Mount Azumaya
  • Torii Ridge (鳥居峠, toriitōge) - Mount Azumaya
  • Palcall Tsumagoi (パルコール嬬恋) - Mount Azumaya
The gondola (Gondola Palcabin (ゴンドラパルキャビン)) from Palcall Tsumagoi is also operating during the summer season and can be used to climb the mountain

Mountain in the vicinity

  • Mount Neko (根子岳, Neko-dake) (2,207m)
Mount Azumaya
  • Mount Azumaya from Mount Neko, autumn
    Mount Azumaya from Mount Neko, autumn
  • Mount Azumaya from Mount Neko, spring
    Mount Azumaya from Mount Neko, spring
  • Summit of Mount Azumaya, late winter
    Summit of Mount Azumaya, late winter
  • Mount Neko (left) and Mount Azumaya, spring
    Mount Neko (left) and Mount Azumaya, spring

See also

Media related to Mount Azumaya at Wikimedia Commons

Wikious
Boobota
Sagapedia