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From Wikipedia, the free encyclopedia

Location of the Mariana Trench
The Mariana Trench is the deepest known part of the world's oceans, and the lowest elevation of the surface of the Earth's crust. It is located in the western Pacific Ocean, to the east of the Mariana Islands. The trench is about 2,550 kilometres (1,580 mi) long but has a mean width of only 69 kilometres (43 mi). It reaches a maximum depth of about 11,033 metres (36,198 ft) at the Challenger Deep, a small slot-shaped valley in its floor, at its southern end.[1]
Part of the Izu-Bonin-Mariana Arc system, the trench forms the boundary between two tectonic plates, where the western edge of the Pacific Plate is subducted beneath the small Mariana Plate. Because the Pacific plate is the largest of all the tectonic plates on Earth, crustal material at its western edge has had a long time since formation (up to 170 million years) to compact and become very dense; hence its great height-difference relative to the higher-riding Mariana Plate, at the point where the Pacific Plate crust is subducted. This deep area is the Mariana trench proper. The movement of these plates is also responsible for the formation of the Mariana Islands.
At the bottom of the trench, where the plates meet, the water column above exerts a pressure of 108.6 megapascals (15,750 psi), over one thousand times the standard atmospheric pressure at sea level. If Mount Everest, the highest mountain on Earth at 8,848 metres (29,029 ft), were set in the deepest part of the Mariana Trench, there would be 2,076 metres (6,811 ft) of water left above it.[1]
Because the Earth is not a perfect sphere, the trench is not the part of the seafloor closest to the center of the Earth - parts of the Arctic Ocean seabed are at least 13,000 meters closer to the center than the Challenger Deep seafloor.


Measurement and study

The Pacific plate is subducted below the Mariana Plate, creating the Mariana trench, and (further on) the arc of the Mariana islands, as water trapped in the plate is released and explodes upward to form island volcanoes.
The trench was first sounded during the Challenger expedition (December 1872 – May 1876), which recorded a depth of 9,636 m (31,614 feet).
Challenger II surveyed the trench using echo sounding, a much more precise and vastly easier way to measure depth than the sounding equipment and drag lines used in the original expedition. During this survey, the deepest part of the trench was recorded when the Challenger II measured a depth of 5,960 fathoms (10,900 meters, 35,760 ft) at 11°19′N 142°15′E / 11.317°N 142.25°E / 11.317; 142.25,[2] known as the Challenger Deep.[1]
In 1957, the Soviet vessel Vityaz reported a depth of 11,034 meters (36,200 ft), dubbed the Mariana Hollow.[3] (Although this claim was made by the Soviets in 1957, the finding has not been repeated by subsequent mapping expeditions using more accurate and modern equipment.)[citation needed]
In 1962, the surface ship M.V. Spencer F. Baird recorded a maximum depth of 10,915 meters (35,840 ft), using precision depth gauges.[2]
In 1984, the Japanese sent the Takuyō (拓洋), a highly specialized survey vessel, to the Mariana Trench and collected data using a narrow, multi-beam echo sounder; they reported a maximum depth of 10,924 metres, also reported as 10,920 metres ± 10 metres.[2][4]
On 1 June 2009 sonar mapping of the Challenger Deep by the Simrad EM120 sonar multibeam bathymetry system for deep water (300 - 11.000 meters) mapping aboard the RV Kilo Moana (mothership of the Nereus vehicle), has indicated a spot with a depth of 10,971 m (35,994 ft). The sonar system uses phase and amplitude bottom detection, with an accuracy of better than 0.2% of water depth across the entire swath (implying the depth figure is accurate to less than ± 11 meters).[5][6]
In 2003, a spot was found along the Mariana Trench, the depth of which is around the same depth as the Challenger Deep, possibly even deeper. It was discovered while scientists from the Hawaii Institute of Geophysics and Planetology were completing a survey around Guam; they used a sonar mapping system towed behind the research ship to conduct the survey. This new spot was named the HMRG (Hawaii Mapping Research Group) Deep, after the group of scientists who discovered it.[7]


January 23, 1960: Trieste just before the dive
The Swiss-designed, Italian-built, United States Navy bathyscaphe Trieste reached the bottom at 1:06 p.m. on January 23, 1960, with U.S. Navy Lieutenant Don Walsh and Jacques Piccard on board.[1] Iron shot was used for ballast, with gasoline for buoyancy.[1] The onboard systems indicated a depth of 11,521 meters (37,799 ft), but this was later revised to 10,916 meters (35,814 ft).[8] At the bottom, Walsh and Piccard were surprised to discover soles or flounder about 30 cm (1 ft) long,[9] as well as a shrimp.[1] According to Piccard, "The bottom appeared light and clear, a waste of firm diatomaceous ooze".[9]
Only three descents have ever been achieved. The first was the manned descent by Trieste in 1960. This was followed by the unmanned ROVs Kaikō in 1995 and Nereus in 2009. These three expeditions directly measured very similar depths of 10,902 to 10,916 meters.

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Up to date as of January 15, 2010

Definition from Wiktionary, a free dictionary



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Proper noun

Mariana Trench
  1. A submarine trench in the North Pacific Ocean, noted for having the deepest known point on Earth.


  • Marianas Trench

See also

Simple English

The Mariana Trench (or Marianas Trench) is the deepest known submarine trench. It is also the deepest known location on Earth itself. It is located next to the Mariana Islands, and has a depth of roughly 10,923 m. The trench is near Guam.

The deepest part of the trench, known as the Challenger Deep, has a depth of 10,923 meters (35,838 feet). The Challenger Deep has been reached twice by submersibles, namely the Bathyscaphe Trieste on 23 January 1960 and the Japanese Kaiko, an unmanned robotic deep-sea probe on 24 March 1995.

Kaiko was lost as sea in 2003, and to date there is no surviving probe or submersible strong enough to withstand the immense pressures of the Challenger Deep.

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