:Suiyo Seamount

{{short description|Submarine volcano off the eastern coast of Japan, at the southern tip of the Izu Islands}}

{{Infobox Seamount

| name = Suiyo Seamount

| depth = {{convert|1418|m|ft|0|abbr=on}}{{Cite gvp|284093|Suiyo Seamount|10 October 2010}}

| height = ~{{convert|1400|m|ft|0|abbr=on|sigfig=2}}

| pushpin_map = Pacific Ocean

| map_caption =

| photo =

| photo_alt =

| photo_caption =

| photo_size =

| summit_area =

| translation =

| language =

| pronunciation =

| location =

| group =

| coordinates = {{coord|28|36|0|N|140|38|0|E|type:mountain_region:JP|display=inline, title}}

| country = Izu Islands, Japan

| type = Seamount (submarine volcano)

| volcanic_group = Shichiyo Seamounts

| range = Izu–Ogasawara Trench

| age =

| last_activity =

| last_eruption =

| discovered =

| discovered_by =

| first_visit =

}}

Suiyo Seamount is a seamount (submarine volcano) off the eastern coast of Japan, directly south of Torishima and Sofugan volcano at the southern tip of the Izu Islands. The volcano is one of the Shichiyo Seamounts, a small group of submarine volcanoes named after different days of the week ("Suiyo" means "Wednesday" in Japanese).

Suiyo consists of a basaltic to dacitic submarine caldera and lava dome, and rises about {{convert|1400|m|ft|-1|abbr=on|sigfig=2}} from its base on the sea floor to within {{convert|1418|m|ft|0|abbr=on}} of the surface. Suiyo has a prominent summit caldera, {{convert|1.5|km|mi|1|abbr=on}} wide and {{convert|500|m|ft|-1|abbr=on|sigfig=2}} deep.

The volcano's excised (weathered) structure suggests that it is of older age then some of the other volcanoes in the group. Suiyo is covered by a thick sediment cap, a feature that collects over a long span of inactivity, and fault patterns and valleys have been observed on its flanks.{{cite journal|title=Submarine topography of seamounts on the volcanic front of Izu–Ogasawara (Bonin) Arc|journal=Bulletin of the Geological Society of Japan|year=1991|volume=42|issue=12|pages=703–743|url=http://www.gsj.jp/Pub/Bull/vol_42/42-12_03.pdf|accessdate=10 October 2010|author1=Makoto Yuasa |author2=Fumitoshi Murakami |author3=Eiji Saito |author4=Kazuaki Watanabe |name-list-style=amp |publisher=Geological Society of Japan}}

Suiyo Seamount is associated with a magnetic anomaly: ocean-floor surveys of it and the surrounding area found that a large negative rock body existed to the east of the seamount, while positive bodies existed to the northwest and south. The reasons for this complex anomaly, which also exists in several other nearby seamounts, are unknown, but is suggested to be the result of interactions between different magnetic fields of different ages.

A burst of hydrothermal activity was observed in July 1991, raising water temperatures at the vent to {{convert|290|C|F|-1|abbr=on}}; following the event, the volcano, until then thought extinct, was reclassified as active by the Japan Meteorological Agency. A bathymetric survey of the volcano found sulfur-oxidizing microbes to be predominant, and concluded that Suiyo Seamount was a natural "incubator" for this bacterial type.{{cite journal|title=Two Bacteria Phylotypes Are Predominant in the Suiyo Seamount Hydrothermal Plume|journal=Applied and Environmental Microbiology|date=February 2004|volume=70|issue=2|pages=1190–1198|doi=10.1128/AEM.70.2.1190-1198.2004|url= |author1=Michinari Sunamura |author2=Yowsuke Higashi |author3=Chiwaka Miyako |author4=Jun-ichiro Ishibashi |author5=Akihiko Maruyama |name-list-style=amp |publisher=American Society for Microbiology|pmc=348851 |pmid=14766605}}