Sentence examples for rise seamount from inspiring English sources

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The dataset on nematode diversity (Species Richness) consists of 161 samples (new and literature data) collected with multicores and box cores in different ecosystems (open slope, canyon, rise, seamount, and deep basin) along the entire deep Mediterranean Sea from the western to the eastern basin at depths ranging from 204 m to 4,000 m [57], [59], [61], [64], [68], [148], [170].

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The seamount chain extends a long distance toward the Corner Rise Seamounts and the Mid-Atlantic Ridge system, possibly serving as a series of faunal stepping-stones.

These lavas exhibit forms characteristic of early, submerged preshield-stage eruptive episodes, from when the volcano was still a rising seamount that had not yet breached the ocean surface, and their surface exposure is unusual, as in most other volcanoes such lavas would have since been buried by more recent flows.

[48] Hannington and Scott[49] used mineral equilibria to model the decrease in log f(O2) from -32 to -43 as the fluid cooled from 350 to 180°C at 21°N East Pacific Rise and Axial Seamount.

Large ancient volcanoes are found singly or in rows in the basins; these rise to form seamounts and, occasionally, islands.

Numerous seamounts rise from the basin floor, some of which are volcanic; their peaks, often flat (called tablemounts, or guyots), are capped with coral.

"The seamounts rise from seafloor depths of approximately 4,800 metres to up to 130 metres from the surface (more than twice the height of Mount Kosciuszko), and are home to deep water shark species that are only found in Australia".

Davidson Seamount rises approximately 2400 m off the surrounding abyssal plain.

Located in the Dutch Windward Islands about 250 km east of Puerto Rico, it is a flat-topped seamount rising 1800 m from the surrounding sea floor.

Located in the Dutch Windward Islands about 250 km SE of Puerto Rico, Saba Bank is a flat-topped seamount rising 1.8 km from the surrounding sea floor (Figure 1).

Monad Shoal is a seamount rising 250 m from the sea floor in the Visayan Sea (N 11° 19' 06.7″, E 124° 11' 31.9″), eight kilometers due east from Malapascua Island, Cebu, in the Philippines (Figure 1).

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