Shōwa-shinzan

Shōwa-shinzan (昭和新山, Shōwa-shinzan) is a volcanic lava dome in the Shikotsu-Toya National Park, Hokkaido, Japan, next to Mount Usu. The mountain was created between 28 December 1943 and September 1945.[2] Initially, a series of strong earthquakes shook the area, and wheat fields were rapidly uplifted. Lava broke through the surface and the current peak was created. The peak is now 398 m (1,306 ft) tall, and still actively smoking.

Shōwa-shinzan
昭和新山
Shōwa-shinzan (September 2008)
Highest point
Elevation398 m (1,306 ft) [1]
Prominence211 m (692 ft) [1]
Parent peakMount Usu
ListingList of mountains and hills of Japan by height
List of volcanoes in Japan
Coordinates42°32′33″N 140°51′52″E 
Naming
English translationNew Mountain of the Shōwa Era
Language of nameJapanese
Geography
LocationHokkaidō, Japan
Parent rangeNasu Volcanic Zone
Topo mapGeographical Survey Institute 25000:1 壮瞥, 25000:1 虻田, 50000:1 虻田
Geology
Mountain typeLava dome
Volcanic arc/beltNortheast Japan Arc
Last eruption1945
Viewed from Mount Usu

The name Shōwa-shinzan means "Shōwa new mountain", as it formed during the reign of Emperor Hirohito, known as the Shōwa period. When Shōwa-shinzan first appeared, the Japanese authorities were worried that it might be interpreted as an unlucky wartime omen, and its existence was kept secret. Much of the information about peak's formation during these years comes from local postmaster Masao Mimatsu, who kept detailed measurements of its progress.

Shōwa-shinzan
Toya Caldera
Location
Shōwa-shinzan during its formative year in October 1944

Volcanic activity timeline

Generally, the volcanic activity of Shōwa-shinzan can be divided into three main phases as recorded by Masao Mimatsu.[2]

Phase 1, Pre-Eruption Phase (28 December 1943 – 22 June 1944)

On 28 December 1943, earthquakes starting to occur frequently around Mount Usu, with occurrences of more than 200 times per day on some days. The hypocenter in the early days was located in the vicinity of Lake Tōya. As the year entered 1944, the hypocenter started to move toward the eastern part of the base of Mount Usu and this resulted in the protuberance of the overlying ground. Eventually the protuberance started to spread to the north, reaching up to heights of 50 meters in some areas. The Sōbetsu riverbed also started to rise, and many fissures started to appear in the surrounding farmlands. The longest fissure recorded was about 600 meters long. On 22 June 1944, there were about 250 earthquakes in one day, and accordingly the protuberance of the ground rose by 150 centimeters in one day.[2]

Phase 2, Eruption Phase (23 June 1944 – 31 October 1944)

On 23 June 1944 at 0815 hours, smoke started to come out of the fissures and shortly after a huge eruption followed accompanied by a thunderous roar. On 2 July 1944, the eruption became even more vigorous, and a phreatomagmatic eruption occurred. On 7 July 1944, a pyroclastic surge accompanied the eruption. The surge managed to reach the northern bank of Lake Tōya, burning forests and houses in the process. By the end of October 1944, Masao Mimatsu recorded a total of seven craters, seventeen major eruptions and countless minor ones. Furthermore, centimeters of volcanic ash from the eruption had been found deposited up to one kilometer away from the volcano, while the protuberance of the ground continued. From July 1944 to August 1944, the protuberance grew by two meters on some days.[2]

Phase 3, Post Eruption Phase (1 November 1944 – September 1945)

Within this phase all eruption activity stopped completely and a lava dome began to take shape. The lava dome continued to take shape until September 1945, when earthquake activity finally seemed to come to a halt. The birth of Shōwa-shinzan was finally complete. Even so, the volcano continues to emit smoke even until today.[2]

See also

References
  1. Geographical Survey Institute topographic map 壮瞥, last access 28 May 2008
  2. 神沼克伊,小山悦郎 日本の火山を科学する　日本列島津々浦々、あなたの身近にある108の活火山とは？ ソフトバンククリエイティブ 2011. ISBN 978-4797361308.
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