Three dimensional magnetization structure of the Tofua Arc 12 seamount constrained by magnetization vector inversion. [PDF]
Choi SY +6 more
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Holothuroidea of the Emperor Seamount Chain: Taxonomy, Morphology and Molecular Data. [PDF]
Kremenetskaia A, Dudnik ZI, Gebruk AV.
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SYSU_Topo: a 1-arc-minute global bathymetry from SWOT-derived gravity using the gravity-geological method. [PDF]
Feng W +7 more
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Shark movements between islands in the Revillagigedo Archipelago and connectivity to other islands in the Eastern Tropical Pacific. [PDF]
Lara-Lizardi F +15 more
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Automated underwater image analysis reveals sediment patterns and megafauna distribution in the tropical Atlantic. [PDF]
Mbani B, Greinert J.
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High-capacity nations can unlock momentum for quality marine protection. [PDF]
Favoretto F +10 more
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The role of plume-lithosphere interaction in Hawaii-Emperor chain formation. [PDF]
Xie S +6 more
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Atlas of the Mediterranean seamounts and seamount-like structures
2016Seamounts are relevant seafloor structures, which may have different origins and which feature all the world oceans and they may be defined as hotspots of biodiversity, greatly affecting the productivity of the offshore ecosystems and the distribution of pelagic top predators.
Maurizio Würtz, Marzia Rovere
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Age of Kōko Seamount, Emperor Seamount chain
Earth and Planetary Science Letters, 1973K Ar ages obtained by the conventional isotope-dilution and the 40Ar/39Ar techniques on two sanidine trachytes, four basalts, and a phonolite dredged from the top of Ko¯ko Seamount, 300 km north of the Hawaiian-Emperor bend, show that the seamount is 46.4 ± 1.1 my old.
David A. Clague, G. Brent Dalrymple
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Sea mountains are arguably the most common large geomorphological features on Earth. Most seamounts are volcanic in origin and vary in shape with size. Small volcanic seamounts are simple, typically truncated cones, whereas seamounts taller than 3km have more diverse forms due to multiple volcanic centers, flank rift zones and landsliding.
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