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Specifically, 1) the number of species found only on seamounts 2) number of species found only on a particular seamount chain, 3) the number of species found only on individual seamounts, 4) the number of species restricted to a particular habitat on a seamount, and 5) the number of species found in a single sample, among replicate samples, on a single seamount chain.
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Sites A, B, and C are located on the flank of a seamount, on the flank of a dip, and on the flank between two seamounts and two dips, respectively.
We calculated MT responses for 11 periods (from 177 to 56,234 seconds) at three points: Site A is located on the flank of a seamount, site B on the flank of a dip, and site C on the flank between two seamounts and two dips.
Something perhaps a seamount on the sinking plate pinned the high-slip patch of fault in place for 500 or 1000 years, they argue, while patches around it failed repeatedly in smaller quakes.
On the other hand, other seismic surveys (Ranero and von Huene 2000, Bangs et al. 2006, and Mochizuki et al. 2008) and a laboratory study (Dominguez et al. 2000) suggested that interplate coupling is weak on a subducting seamount due to elevated pore pressure.
In this paper we present a seamount classification based on "biologically meaningful" physical variables for which global-scale data are available.
Lōihi is a seamount, or underwater volcano, on the flank of Mauna Loa, the Earth's largest shield volcano.
One way the organisers hope to entice users is by putting instruments on Axial Seamount, an underwater volcano about 480km west of Oregon that could erupt at any time.
We ranked species abundance overall and among habitat types according to their rarity, determined from the number of observations of a species on Davidson Seamount and in nearby Monterey Canyon.
This study focuses on two seamounts, a submarine volcano (cratered seamount – CSM) and a non-volcano (SM2) in the Andaman Back arc Basin (ABB), and the basin itself.
In southwest Japan, likewise, a highly reflective low-velocity layer dips c. 7°NW below Shikoku Island, down-dip from a subducting seamount on the inner wall of the Nankai Trough, defining the subduction interface that ruptured in the 1946 Mw8.1 Nankaido megathrust earthquake.
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