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The deepest section, called the China Sea Basin, has a maximum depth of 16,457 feet (5,016 m).
The lake is 360 miles long but never more than 50 miles wide; it has a maximum depth of 2,310 feet.
With a mean surface elevation of 579 feet (176 m) above sea level, the lake has a maximum depth of 923 feet (281 m).
It is 55 miles (90 km) long north to south and 30 miles across the mouth and has a maximum depth of 72 feet (22 metres).
The Okinawa Trough, its deepest section, extends alongside the Ryukyu Island chain and has a maximum depth of 8,912 feet (2,717 m).
The bay is about 150 miles (240 km) long and 20 40 miles (32 64 km) wide and has a maximum depth of 400 feet (120 metres).
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It is the oldest existing freshwater lake on Earth (20 million–25 million years old), as well as the deepest continental body of water, having a maximum depth of 5,315 feet (1,620 metres).
Quaternary deposits in the Aomori plain have a maximum depth of ~800 m (Tomidokoro 1996), while surface Holocene deposits have a maximum depth of 10 20 m (Kubo et al. 2006).
Measurements were performed in the Helgoland Harbour at the end of the south-mole, where the water column had a maximum depth of around 9 m.
The ejecta comprised 66% fine sand (100 250 μm) and 20% medium sand (250 500 μm) and had a maximum depth of 40 cm.
The initial depth of the oceanic mixed layer was determined from oceanic reanalysis data by defining the mixed layer as reaching a depth at which the density was no more than 0.25 kg m−3 higher than the density at the surface and having a maximum depth of 200 m.
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CEO of Professional Science Editing for Scientists @ prosciediting.com