Lōʻihi Seamount
Hydrothermal vent geochemistry
Lōʻihi's mid-Pacific location and its well-sustained hydrothermal system contribute to a rich oasis for a microbial ecosystem. Areas of extensive hydrothermal venting are found on Lōʻihi's crater floor and north slope, and along the summit of Lōʻihi itself.

Lōʻihi Seamount

Section Title: Hydrothermal vent geochemistry
Table Section Text: Lōʻihi's mid-Pacific location and its well-sustained hydrothermal system contribute to a rich oasis for a microbial ecosystem. Areas of extensive hydrothermal venting are found on Lōʻihi's crater floor and north slope, and along the summit of Lōʻihi itself.

Vent	Depth	Location	Notes

Pele's	1,000 m (3,281 ft)	Summit	Destroyed 1996

Kapo's	1,280 m (4,199 ft)	Upper South rift	No longer venting

Forbidden	1,160 m (3,806 ft)	Pele's Pit	over 200 °C

Lohiau ("slow")	1,173 m (3,850 ft)	Pele's Pit	77 °C

Pahaku ("rocky")	1,196 m (3,924 ft)	South rift zone	17 °C

Ula ("red")	1,099 m (3,606 ft)	South summit	Diffuse venting

Maximilian	1,249 m (4,098 ft)	West summit flank	Diffuse venting

Naha	1,325 m (4,347 ft)	South rift	23 °C

Sentence(s)

A hydrothermal vent field (Naha Vents) was located in the south rift zone at a depth of 1,325 m.

final_sentence: A hydrothermal vent field (Naha Vents) was located in the south rift zone at a depth of 1,325 m.