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Mount Aso

Volcano in Kumamoto Prefecture, Japan

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阿蘇山広域空撮画像 阿蘇山 広域空撮画像。
Sonata / Sonata at ja.wikipedia · CC BY-SA 3.0

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Through Volcano, Sea level and Ramsar site

Geography

The central cone group of Aso consists of five peaks, often called the "Five Mountains of Aso" (阿蘇五岳): Mt. Neko, Mt. Taka (also called Takadake or Taka-Dake), Mt. Naka (also called Nakadake or Naka-Dake), Mt. Eboshi, and Mt. Kishima (also called Kishimadake or Kishima-Dake). The highest point is the summit of Mt. Taka, at 1,592 m above sea level. The crater of Mt. Naka, the west side of which is accessible by road, contains an active volcano which continuously emits smoke and has occasional eruptions. Only the northernmost crater (the first crater) has been active for the last 70 years—1974, 1979, 1984–1985, 1989–1991, 2009, 2011, 2015, 2016 and 2021.

The present Aso Caldera formed as a result of four huge caldera eruptions occurring over a range of 90,000–300,000 years ago. The caldera, one of the largest in the world, contains the city of Aso as well as Takamori and Minamiaso. The caldera extends about 18 km east to west and about 25 km north to south. Viewpoints from the somma overlooking the caldera are perched upon lava formed before the volcanic activity which created the present caldera. Ejecta from the huge caldera eruption 90,800 years ago covers more than 600 km3 and roughly equals the volume of Mount Fuji; with a pyroclastic flow plateau that covered a significant part of Kyushu.

Volcanic ash from Mount Aso and Mount Kujū plays a crucial role in maintaining and replenishing the tidal flats of the Ariake Sea, which are among the largest in Japan. Several of the flats have been designated as Ramsar sites. The ash is carried from the volcanoes to the coastline by the Chikugo River, which has its source located on Aso as well.

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