@article {Rubin2012,
	title = {{Volcanic Eruptions in the Deep Sea}},
	journal = {Oceanography},
	volume = {25},
	number = {1},
	year = {2012},
	month = {mar},
	pages = {142{\textendash}157},
	publisher = {OCEANOGRAPHY SOC},
	address = {ROCKVILLE; P.O. BOX 1931, ROCKVILLE, MD USA},
	abstract = {Volcanic eruptions are important events in Earth{\textquoteright}s cycle of magma generation and crustal construction. Over durations of hours to years, eruptions produce new deposits of lava and/or fragmentary ejecta, transfer heat and magmatic volatiles from Earth{\textquoteright}s interior to the overlying air or seawater, and significantly modify the landscape and perturb local ecosystems. Today and through most of geological history, the greatest number and volume of volcanic eruptions on Earth have occurred in the deep ocean along mid-ocean ridges, near subduction zones, on oceanic plateaus, and on thousands of mid-plate seamounts. However, deep-sea eruptions ({\textgreater} 500~m depth) are much more difficult to detect and observe than subaerial eruptions, so comparatively little is known about them. Great strides have been made in eruption detection, response speed, and observational detail since the first recognition of a deep submarine eruption at a mid-ocean ridge 25 years ago. Studies of ongoing or recent deep submarine eruptions reveal information about their sizes, durations, frequencies, styles, and environmental impacts. Ultimately, magma formation and accumulation in the upper mantle and crust, plus local tectonic stress fields, dictate when, where, and how often submarine eruptions occur, whereas eruption depth, magma composition, conditions of volatile segregation, and tectonic setting determine submarine eruption style.},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {1042-8275},
	doi = {10.5670/oceanog.2012.12},
	author = {Rubin, K H and Soule, S A and Chadwick, W W and Fornari, D J and Clague, D A and Embley, R W and Baker, E T and Perfit, M R and Caress, D W and Dziak, R P}
}
@article {Kurras2000,
	title = {{Volcanic morphology of the East Pacific Rise Crest 9 degrees 49{\textquoteright}-52{\textquoteright}: Implications for volcanic emplacement processes at fast-spreading mid-ocean ridges}},
	journal = {Marine Geophysical Researches},
	volume = {21},
	number = {1-2},
	year = {2000},
	month = {feb},
	pages = {23{\textendash}41},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0025-3235},
	doi = {10.1023/A:1004792202764},
	url = {http://dx.doi.org/10.1023/A:1004792202764},
	author = {Kurras, G J and Fornari, D J and Edwards, M H and Perfit, M R and Smith, M C}
}
@article {Fornari1995,
	title = {{Visualizing the deep sea - vehicles and research techniques yield ever-clearer images of the ocean depths}},
	journal = {Oceanus},
	volume = {38},
	number = {1},
	year = {1995},
	pages = {10{\textendash}13},
	keywords = {HOV Alvin (Human Occupied Vehicle), ROV Argo (Remotely Operated Vehicle), ROV Jason (Remotely Operated Vehicle)},
	issn = {0029-8182},
	author = {Fornari, D J and Bowen, A M and Foster, D B}
}
@article {Haymon1993,
	title = {{Volcanic eruption of the mid-ocean ridge along the East Pacific Rise crest at 9 degrees 45-52{\textquoteright}N: Direct submersible observations of seafloor phenomena associated with an eruption event in April 1991}},
	journal = {Earth and Planetary Science Letters},
	volume = {119},
	number = {1-2},
	year = {1993},
	pages = {85{\textendash}101},
	keywords = {HOV Alvin (Human Occupied Vehicle)},
	issn = {0012-821X},
	doi = {10.1016/0012-821X(93)90008-W},
	url = {http://dx.doi.org/10.1016/0012-821X(93)90008-W},
	author = {Haymon, R and Fornari, D J and Von Damm, K L and Lilley, M and Perfit, M and Edmond, J and Shanks, W and Lutz, R and Grebmeier, J M and Carbotte, S and Wright, D and McLaughlin, E and Smith, M and Beedle, N and Olson, E}
}
