Kueishan Tao (24°51'N, 121 °55′E) is located at a tectonic junction of the fault system extension of Taiwan and the southern rifting end of the Okinawa Trough. A cluster of over 30 vents, at a water depth of about 10～20 m off the eastern tip of the tao emits hydrothermal fluids and volcanic gases su...
No comments yet
Be the first to share your thoughts!