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Coral sea region billfish atlas

Plateaus, Troughs and Trenches

This region is one of extremely complex underwater bathymetry. Currents, upwellings of nutrient-rich waters and concentrations of fish, even in the waters closest to the surface, can be profoundly influenced by underwater mountains and valleys a kilometre or more below them. For example, major seasonal concentrations of black marlin occur in oceanic troughs, such as the Queensland Trough and the Okinawa Trough in the East China Sea. Pre-spawning aggregations of striped marlin off eastern Australia are closely associated with surface waters far above deep underwater ridges and seamounts. Broadbill, too, tend to concentrate over and around seamounts.

Geologists have classified bathymetric features by specific names.

Trench a narrow, elongate depression of the deep-sea floor, with steep sides, oriented parallel to the trend of the continent and between the continental margin and the abyssal hills. Such a trench is about two kilometres deeper than the surrounding ocean floor and may be many kilometres deep.
Trough an elongate depression of the sea floor that is wider and shallower than a trench, with less steeply dipping sides; a trough may develop from a trench by becoming filled with sediment.
Basin a depression in the sea floor more or less as long as it is wide.
Ridge an elongate, steep-sided elevation of the ocean floor, having rough topography.
Seamount an elevation of the sea floor, 1000m or higher, either flat-topped (called a guyot) or peaked (called a sea-peak).
Plateau a broad, more or less flat-topped and ill-defined elevation of the sea floor, generally over 200m in elevation.


Major Bathymetric Features

This map shows the major bathymetric features of the Billfish Atlas. Click on the map to view a high resolution image. (1400Kb 1600x1100) Not recommended if you have a slow Internet connection.

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Last updated - 22 August 98

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