Yonaguni Knoll IV
id:
yonaguni-knoll-iv-269-8289456
title:
Yonaguni Knoll IV
text:
Yonaguni Knoll IV is a seamount in the Okinawa Trough, east of Taiwan. It lies at about 745 metres (2,444 ft) depth and formed through Quaternary volcanism that yielded dacitic and rhyolitic magmas. The seamount is hydrothermally active, with numerous sites that are colonized by mussels and other marine animals. A submarine underground "lake" of liquid carbon dioxide has been identified at Yonaguni Knoll IV.
brand slug:
wiki
category slug:
encyclopedia
description:
Seamount in the Okinawa Trough, east of Taiwan
original url:
https://en.wikipedia.org/wiki/Yonaguni_Knoll_IV
date created:
date modified:
2023-12-10T21:07:14Z
main entity:
{"identifier":"Q107572293","url":"https://www.wikidata.org/entity/Q107572293"}
image:
fields total:
13
integrity:
14