Hydrothermal vents are analogous to hot springs on land. They are usually found in water between 2,000 and 4,000 m deep; however, shallow water vents have been observed off the coast of New Zealand, Greece, Italy, Papua New Guinea, and the Azores archipelago. The vents are formed when cold (2° C; 35.6° F) seawater seeps into the sea floor, picks up heat and minerals, and then rises up and out of the seafloor, back into the ocean. As the vent water bursts into the ocean, its temperature is greater than 350°C (662°F).
The hottest and most vigorous of the vents are black smokers, named as such for the black plumes they produce. When the scalding hot fluid they release hits the icy cold seawater, minerals in the fluid precipitate out (form into particles), creating a plume that looks just like dark, billowing smoke.
Although it was originally thought that these smoker vents were silent, research has shown that these vents, in fact, generate sound. The vents produce broadband acoustic signals at frequencies of 5-15 Hz with power levels approximately 10-30 dB above the ambient noise level. The vents also produce narrowband tones from 10-250 Hz, at power levels approximately 10-20 dB above the broadband signals. Each vent has a unique acoustic signature and scientists have theorized that this is most likely due to differences in the vent’s physical structures.
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Crone, T. J., Wilcock, W. S. D., Barclay, A. H., & Parsons, J. D. (2006). The Sound Generated by Mid-Ocean Ridge Black Smoker Hydrothermal Vents. PLoS ONE, 1(1), e133. https://doi.org/10.1371/journal.pone.0000133
Hydrothermal Plume Studies, (n.d.). NOAA Vents Program. Retrieved from https://www.pmel.noaa.gov/eoi/plumestudies.html.