Deposit Type:
PMS, polymetallic massive sulfides
Notes on Vent Field Description:
inactive sulfide deposits, Fe oxide gossans, low-temperature Fe oxide and silica chimneys, and Fe-Mn crusts (up to 150 m explored dimensions); this location is off-axis to the east
Notes Relevant to Biology:
Year and How Discovered (if active, visual confirmation is listed first):
Discovery References (text):
[(abstract says active and inactive explored by submersible Mir) Lisitsyn et al., A HYDROTHERMAL FIELD IN THE RIFT ZONE OF THE MANUS BASIN, BISMARCK SEA, International Geology Review, 35, 105-126, 1993]