is a
submarine volcano located about 450 kilometers south of
Tokyo
Tokyo, officially the Tokyo Metropolis, is the capital of Japan, capital and List of cities in Japan, most populous city in Japan. With a population of over 14 million in the city proper in 2023, it is List of largest cities, one of the most ...
on the Izu-Ogasawara Ridge in the
Izu Islands. Volcanic activity has been detected there since 1869. Since then it has undergone more
eruptions, the most powerful of which resulted in the appearance and disappearance of a small
island
An island or isle is a piece of land, distinct from a continent, completely surrounded by water. There are continental islands, which were formed by being split from a continent by plate tectonics, and oceanic islands, which have never been ...
.
The name Myōjin-shō derives from a fishing boat, ''No.11 Myōjin-Maru'' of
Yaizu City,
Shizuoka Prefecture
is a Prefectures of Japan, prefecture of Japan located in the Chūbu region of Honshu. Shizuoka Prefecture has a population of 3,555,818 and has a geographic area of . Shizuoka Prefecture borders Kanagawa Prefecture to the east, Yamanashi Pref ...
, the crew of which first witnessed the major volcanic eruption of 1952.
Eruption of 1952-1953

The volcanic eruption from 1952 to 1953 was one of its biggest eruptions on record, with the repetitious appearance and disappearance of an island, which at one point reached over ten metres above sea level, before sinking after a major volcanic eruption in September 1953. On September 24, 1952, a survey vessel,
''Kaiyo Maru No. 5'' of the
Hydrographic Department of the Maritime Safety Agency, was destroyed by the volcano, with the loss of its crew of 31 (including the nine scientists studying the eruption). Consequently, the Department developed ''Manbou'' (Sunfish), an unmanned radio operating survey boat, and has used it for the research of dangerous sea areas such as submarine volcanoes.
This was the first time that volcanic activity had been detected using the
SOFAR channel.
[
"Transpacific detection of Myojin volcanic explosions by underwater sound"]
Survey of 1998-1999
In 1998 and 1999, the Hydrography Department conducted comprehensive sea bottom surveys around Myōjin-shō, using the state-of-the-art survey vessel ''Shoyo'' and ''Manbou II'', the second generation ''Manbou''. As a result of these surveys, a detailed picture of the
seabed topography around Myōjin-shō was made for the first time.
''Manbou II'' conducted the survey of the sea area within a radius of 3
nautical mile
A nautical mile is a unit of length used in air, marine, and space navigation, and for the definition of territorial waters. Historically, it was defined as the meridian arc length corresponding to one minute ( of a degree) of latitude at t ...
s (about 5.4 kilometers) of Myōjin-shō. ''Shoyo'' conducted the survey of the sea area within a radius of about 10 nautical miles (about 18.5 kilometers) but farther than the area of the radius of . ''Manbou II'' works by the order of preprogrammed instructions and measures depth and water temperature. Bathymetric survey of ''Manbou II'' was carried out by using the "PRD-601" echo sounder at intervals of 0.2 nautical miles (about 370 meters). ''Shoyo'' conducted a comprehensive survey including the geological and geophysical surveys of sea bottom.
Bathymetric survey of ''Shoyo'' was carried out by using a "Seabeam 2112" echo sounder at intervals of 0.5 nautical miles (about 930 meters).
Structure
Previously, Myōjin-shō was considered to be the central cone of a double volcano with the
Bayonnaise Rocks (rocks of 9.9 meters in height above the sea level) as a portion of the
somma (Mita, 1949). As a result of the survey, however, the authors found that both Myōjin-shō and the Bayonnaise Rocks are cones on the somma of a double volcano. The foot of this double volcano lies 1,400 to 1,500 meters in depth and the size is about 30 by 25 kilometers east-west, north-south. The somma is almost a circle in the diameter of 7 by 9 kilometers and the height is 1,000 – 1,400meters.
The diameter of the caldera floor is 5.6 kilometers and about 1,100 meters in depth. The central cone is a high formerly known as
Takane-shō, 328 metres below sea level.
Myōjin-shō is a post caldera cone formed in the northeastern part of the somma of the double volcano. It is a single conical cone and its height is 550 meters with the shallowest depth 50 meters. A record that suggests a gushing of bubbles near the summit was obtained and micro-earthquakes were observed near Myōjin-shō, showing that the volcano is still active, although at a low level
Gallery
1952 eruption
File:Myojin-sho_19520917.jpg, Myōjin-shō, 1952
File:Myojinsho.JPG, Myōjin-shō, 1952
References
External links
Survey of Myojin-sho
{{DEFAULTSORT:Myojin-sho
Izu Islands
Seamounts of the Pacific Ocean
Ephemeral islands
Natural disasters in Japan
1952 natural disasters
Postwar Japan
Former islands from the last glacial maximum