@article {RN176,
	title = {Quantification of eruption dynamics on the north rift at Axial Seamount, Juan de Fuca Ridge},
	journal = {Geochemistry Geophysics Geosystems},
	year = {2020},
	type = {Journal Article},
	abstract = {Quantifying eruption dynamics in submarine environments is challenging. During the 2015 eruption of Axial Seamount, the formation of hummocky mounds along the north rift was accompanied by tens of thousands of impulsive acoustic signals generated by the interaction of lava and seawater. A catalog of these sounds was integrated with detailed seafloor mapping to better understand eruptive processes in time and space. Mounds grew over a period of 28 days with average extrusion rates of 22 to 45 m3 s-1. The most distant mounds, ~9.5 to 15.5 km down rift from the caldera, grew primarily over the first few days of the eruption. The focus of eruptive activity then retreated ~5 km toward the caldera where it was sustained. Mounds are constructed as a series of superimposed lobes formed through alternating periods of flow inflation, generating up to 30-m-thick hummocks, and periods of flow advancement, with <0.02 m s-1 average speeds typically observed.},
	doi = {10.1029/2020gc009136},
	url = {https://app.dimensions.ai/details/publication/pub.1129829964},
	author = {Le Saout, M. and Bohnenstiehl, D. R. and Paduan, J. B. and Clague, D. A.}
}
@article {RN223,
	title = {High-Resolution AUV Mapping and Targeted ROV Observations of Three Historic Lava Flows at Axial Seamount},
	journal = {Oceanography},
	volume = {30},
	number = {4},
	year = {2017},
	pages = {82-99},
	type = {Journal Article},
	abstract = {The lava flows produced by eruptions at Axial Seamount in 1998, 2011, and 2015 were mapped at 1 m resolution from autonomous underwater vehicles (AUVs) developed at the Monterey Bay Aquarium Research Institute (MBARI). A portion of the flows erupted in 2011 and 2015 are defined by pre- and post-eruption AUV surveys. Data processing software, also developed at MBARI, precisely coregisters pre- and post-eruption surveys to allow construction of difference maps by subtracting a pre-eruption grid from a post-eruption grid. Such difference maps are key to extracting detailed information about eruptive processes and emplacement of the lava flows. All three eruptions began on the east side of the caldera, and each produced ~25 {\texttimes} 106 m3 of thin channelized flows (with sheet lava channels, lobate lava interiors with pillars, and distal inflated pillow lobes) in the caldera and on the upper south or north rifts. The 1998 and 2011 eruptions propagated down the south rift, and the 2015 eruption propagated down the north rift. The 2011 and 2015 eruptions formed shallow grabens surrounding new non-eruptive open fissures on the east rim of the caldera and produced thick hummocky flows on upper to mid rifts, and the 2011 eruption also produced a thick hummocky flow on the lower south rift. Future eruptions at Axial Seamount will likely follow this pattern, regardless of which rift is the locus of the eruption.},
	issn = {1042-8275},
	doi = {10.5670/oceanog.2017.426},
	author = {Clague, D. A. and Paduan, J. B. and Caress, D. W. and Chadwick, W. W. and Le Saout, M. and Dreyer, B. M. and Portner, R. A.}
}
@article {RN226,
	title = {Voluminous eruption from a zoned magma body after an increase in supply rate at Axial Seamount},
	journal = {Geophysical Research Letters},
	volume = {43},
	number = {23},
	year = {2016},
	pages = {12,063-12,070},
	type = {Journal Article},
	abstract = {Axial Seamount is the best monitored submarine volcano in the world, providing an exceptional window into the dynamic interactions between magma storage, transport, and eruption processes in a mid-ocean ridge setting. An eruption in April 2015 produced the largest volume of erupted lava since monitoring and mapping began in the mid-1980s after the shortest repose time, due to a recent increase in magma supply. The higher rate of magma replenishment since 2011 resulted in the eruption of the most mafic lava in the last 500{\textendash}600 years. Eruptive fissures at the volcano summit produced pyroclastic ash that was deposited over an area of at least 8 km2. A systematic spatial distribution of compositions is consistent with a single dike tapping different parts of a thermally and chemically zoned magma reservoir that can be directly related to previous multichannel seismic-imaging results.},
	issn = {0094-8276},
	doi = {https://doi.org/10.1002/2016GL071327},
	url = {https://doi.org/10.1002/2016GL071327},
	author = {Chadwick Jr, W. W. and Paduan, J. B. and Clague, D. A. and Dreyer, B. M. and Merle, S. G. and Bobbitt, A. M. and Caress, D. W. and Philip, B. T. and Kelley, D. S. and Nooner, S. L.}
}
