Research paperVolcanic development of small oceanic central volcanoes on the flanks of the East Pacific Rise inferred from narrow-beam echo-sounder surveys
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2022, Treatise on GeomorphologyThe lifecycle of mid-ocean ridge seamounts and their prodigious flank collapses
2020, Earth and Planetary Science LettersCitation Excerpt :Volcanic seamount morphologies exist between two end-members depending principally on the geometry of the magma conduits: (1) point-source whereby magma is extruded from a single central vent; and (2) linear-source where magma is effused along ridges (Schmidt and Schmincke, 2000). Basalts and andesites recovered from seamounts demonstrate long multimillion-year lifecycles (Batiza and Vanko, 1983; Honda et al., 1987; Pringle et al., 1991). Previous work has studied the geomorphology of seamounts thought to represent different stages of development (Vogt and Smoot, 1984; Chaytor et al., 2007; Mitchell and Lofi, 2008; Dziak and Merle, 2016).
Geomorphological features in the southern Canary Island Volcanic Province: The importance of volcanic processes and massive slope instabilities associated with seamounts
2016, GeomorphologyCitation Excerpt :The presence of numerous volcanic cones over The Paps seamount can be explained in terms of magma extrusion that is not channelised through a single point but rather multiple paths towards the seafloor. Hills and small seamounts are developed during short-lived volcanic events, whereas large edifices grow over longer periods, often having multiple volcanic centres (Batiza and Vanko, 1983) as seen by the presence of several cones in The Paps and Echo seamounts. Tropic seamount has a clearly outlined four-peaked star shape.
Wave-planation surfaces in the mid-western East Sea (Sea of Japan): Indicators of subsidence history and paleogeographic evolution of back-arc basin
2013, Marine GeologyCitation Excerpt :In the East Sea back-arc region, widespread extensional tectonics with thermal decay of the stretched lithosphere most likely led to continuous subsidence of flat-topped volcanic edifices after wave planation. Flat-topped volcanic seamounts can also form through the collapse of caldera rim, the infilling of a caldera basin by subsequent volcanic intrusion and extrusion (e.g., Simkin, 1972; Natland, 1976; Batiza and Vanko, 1983; Menard, 1984). These processes are not applicable to the study area, however, because the transparent substratal reflection configuration of the seamounts indicates that they comprise coherent volcanic rocks rather than caldera-rim-collapse or extrusive deposits whose seismic facies is generally chaotic to irregularly stratified (Kim et al., 2011) (Fig. 8).