The mariana trench or marianas trench[1]

is the deepest part of the worlds oceans.It is located in the western pacific ocean,to the east of the mariana islands.The trench is about 2,550 kilometres (1,580mi) long with an average width 69 kilometres (43mi) . by wikipedia.

People can cout how many kilometres in sky how deep is the marana trench

The trench is not the part of the seafloor closest to the center of the Earth. This is because the Earth is not a perfect sphere; its radius is about 25 kilometres (16 mi) less at the poles than at the equator.[5] As a result, parts of the Arctic Ocean seabed are at least 13 kilometres (8.1 mi) closer to the Earth's center than the Challenger Deep seafloor.

Xenophyophores have been found in the trench by Scripps Institution of Oceanography researchers at a record depth of 10.6 km (6.6 mi) below the sea surface.[6] On 17 March 2013, researchers reported data that suggested microbial life forms thrive within the trench.[7][8]

Contents

  [hide] 

he Mariana Trench is named for the nearby Mariana Islands (in turn named Las Marianas in honor of Spanish Queen Mariana of Austria, widow of Philip IV of Spain). The islands are part of the island arc that is formed on an over-riding plate, called the Mariana Plate (also named for the islands), on the western side of the trench.

Geology[edit]

The Pacific plate is subducted beneath 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 Mariana Trench is part of the Izu-Bonin-Mariana subduction system that forms the boundarybetween two tectonic plates. In this system, the western edge of one plate, the Pacific Plate, issubducted (i.e., thrust) beneath the smaller Mariana Plate that lies to the west. Crustal material at the western edge of the Pacific Plate is some of the oldest oceanic crust on earth (up to 170 million years old), and is therefore cooler and more dense; hence its great height difference relative to the higher-riding (and younger) Mariana Plate. The deepest area at the plate boundary is the Mariana Trench proper.

The movement of the Pacific and Mariana plates is also indirectly responsible for the formation of theMariana Islands. These volcanic islands are caused by flux melting of the upper mantle due to release of water that is trapped in minerals of the subducted portion of the Pacific Plate.

Measurements[edit]

See also: Challenger Deep

The trench was first sounded during the Challenger expedition in 1875, which recorded a depth of 4,475 fathoms (8.184 km; 26,850 ft).[9] In 1877 a map was published called Tiefenkarte des Grossen Ozeans by Petermann, which showed a Challenger Tief at the location of that sounding. In 1899 USS Nero, a converted collier, recorded a depth of 5269 fathoms (9,636 m, 31,614 ft).[10] 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 (10.90 km; 35,760 ft) at 11°19′N 142°15′E, known as the Challenger Deep.[11]

In 1957, the Soviet vessel Vityaz reported a depth of 11,034 m (36,201 ft), dubbed the Mariana Hollow.[3]

In 1962, the surface ship M.V. Spencer F. Baird recorded a maximum depth of 10,915 m (35,840 ft), using precision depth gauges.

In 1984, the Japanese survey vessel Takuyō (拓洋) collected data from the Mariana Trench using a narrow, multi-beam echo sounder; it reported a maximum depth of 10,924 m (35,840 ft), also reported as 10,920 m (35,830 ft) ±10 m (33 ft),.[12]

Remotely Operated Vehicle KAIKO reached the deepest area of Mariana trench and made the deepest diving record of 10,911 m (35,797 ft) on March 24, 1995.[13]

During surveys carried out between 1997 and 2001, a spot was found along the Mariana Trench that had depth similar to that of 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.[14]

On 1 June 2009 sonar mapping of the Challenger Deep by the Simrad EM120 sonar multibeam bathymetry system for deep water, i.e. depths of 300–11,000 m (980–36,000 ft) 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 ± 22 metres).[15][16]

In 2011, it was announced at the American Geophysical Union Fall Meeting that a US Navy hydrographic ship equipped with a multibeam echosounder conducted a survey which mapped the entire trench to 100 m (330 ft) resolution.[2] The mapping revealed the existence of four rocky outcrops thought to be formerseamounts.[17]

The Mariana Trench is a site chosen by researchers at Washington University and the Woods Hole Oceanographic Institution in 2012 for a seismic survey to investigate the subsurface water cycle. Using both ocean-bottom seismometers and hydrophones the scientists are able to map structures as deep as 60 mi (97 km) beneath the surface.[18]

Descents[edit]

The bathyscaphe Trieste (designed by Auguste Piccard), the first manned vehicle to reach the bottom of the Marianas Trench.[19]

Four descents have been achieved. The first was the manned descent by Swiss-designed, Italian-built, United States Navy-owned bathyscaphe Trieste which reached the bottom at 1:06 pm on 23 January 1960, with Don Walsh and Jacques Piccardon board.[11][20] Iron shot was used for ballast, with gasoline for buoyancy.[11] The onboard systems indicated a depth of 11,521 m (37,799 ft), but this was later revised to 10,916 m (35,814 ft).[21] The depth was estimated from a conversion ofpressure measured and calculations based on the water density from sea surface to seabed.[20]

This was followed by the unmanned ROVs Kaikō in 1996 and Nereus in 2009. The first three expeditions directly measured very similar depths of 10,902 to 10,916 m (35,768 to 35,814 ft).

The fourth was made by Canadian film director James Cameron in 2012. On 26 March, he reached the bottom of the Mariana Trench in the submersible vessel Deepsea Challenger.[22][23][24]

In July 2015, members of the National Oceanic and Atmospheric Administration, Oregon State University, and the Coast Guard submerged a hydrophone into the deepest part of the Mariana Trench, the Challenger Deep. Never having deployed one past a mile, the titanium-shelled hydrophone was designed to withstand the immense pressure 7 miles under.[25]Although researchers were unable to retrieve the hydrophone until November, the data capacity was full within the first 23 days. After months of analyzing the sounds, the experts were surprised to pick up natural and man-made sounds such as boats, earthquakes, a typhoon, and baleen whales.[26] Due to the mission's success, the researchers plan to deploy a second hydrophone in 2017 for an extended period of time.

Planned descents[edit]

As of February 2012, at least two other teams are planning piloted submarines to reach the bottom of the Mariana Trench. These include: Triton Submarines, a Florida-based company that designs and manufactures private submarines, for which a crew of three will take 120 minutes to reach the seabed;[27] and DOER Marine, a marine technology company, based near San Francisco and set up in 1992, for which a crew of two or three will take 90 minutes to reach the seabed.[28]

Life[edit]

The expedition conducted in 1960 claimed to have observed (with great surprise because of the high pressure) large creatures living at the bottom, such as aflatfish about 30 cm (1 ft) long,[21] and shrimp.[29] According to Piccard, "The bottom appeared light and clear, a waste of firm diatomaceous ooze".[21] Many marine biologists are now skeptical of the supposed sighting of the flatfish, and it is suggested that the creature may instead have been a sea cucumber.[30][31]

During the second expedition, the unmanned vehicle Kaikō collected mud samples from the seabed.[32] Tiny organisms were found to be living in those samples.

In July 2011, a research expedition deployed untethered landers, called dropcams, equipped with digital video and lights to explore this region of the deep sea. Amongst many other living organisms, some gigantic single-celled amoebas with a size of more than 4 in (10 cm), belonging to the class of xenophyophores were observed.[33] Xenophyophores are noteworthy for their size, their extreme abundance on the seafloor and their role as hosts for a variety of organisms.

In December 2014, a new species of snailfish was discovered at a depth of 8,145 m (26,722 ft), breaking the previous record for the deepest living fish seen on video.[34] Several other new species were also filmed, including huge crustaceans known as supergiants.[34]

Possible nuclear waste disposal site[edit]

Like other oceanic trenches, the Mariana Trench has been proposed as a site for nuclear waste disposal,[35][36] in the hope that tectonic plate subduction occurring at the site might eventually push the nuclear waste deep into the Earth's mantle. However, ocean dumping of nuclear waste is prohibited by international law.[35][36][37] Furthermore, plate subduction zones are associated with very large megathrust earthquakes, the effects of which are unpredictable and possibly adverse to the safety of long-term disposal.[36] Also, disposal of nuclear wastes may cause havoc in the hadopelagic ecosystems.

See also[edit]

This article is about the deep sea trench. For the Canadian band named after the geological formation, see Marianas Trench (band).

Location of the Mariana Trench

The Mariana Trench or Marianas Trench[1] is the deepest part of the world's oceans. 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 with an average width of 69 kilometres (43 mi). It reaches a maximum-known depth of 10,994 m (± 40 m) or 6.831 mi (36,070 ± 131 ft) at a small slot-shaped valley in its floor known as the Challenger Deep, at its southern end,[2] although some unrepeated measurements place the deepest portion at 11,034 metres (36,201 ft).[3]

At the bottom of the trench the water column above exerts a pressure of 1,086 bars (15,750 psi) (over 1000 times the standard atmospheric pressure at sea level). At this pressure, the density of water is increased by 4.96%, making 95 litres of water under the pressure of the Challenger Deep contain the same mass as 100 litres at the surface. The temperature at the bottom is 1 to 4 °C.[4]

The trench is not the part of the seafloor closest to the center of the Earth. This is because the Earth is not a perfect sphere; its radius is about 25 kilometres (16 mi) less at the poles than at the equator.[5] As a result, parts of the Arctic Ocean seabed are at least 13 kilometres (8.1 mi) closer to the Earth's center than the Challenger Deep seafloor.

Xenophyophores have been found in the trench by Scripps Institution of Oceanography researchers at a record depth of 10.6 km (6.6 mi) below the sea surface.[6] On 17 March 2013, researchers reported data that suggested microbial life forms thrive within the trench.[7][8]

Contents

  [hide] 

ariana Trench

From Wikipedia, the free encyclopedia

This article is about the deep sea trench. For the Canadian band named after the geological formation, see Marianas Trench (band).

Location of the Mariana Trench

The Mariana Trench or Marianas Trench[1] is the deepest part of the world's oceans. 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 with an average width of 69 kilometres (43 mi). It reaches a maximum-known depth of 10,994 m (± 40 m) or 6.831 mi (36,070 ± 131 ft) at a small slot-shaped valley in its floor known as the Challenger Deep, at its southern end,[2] although some unrepeated measurements place the deepest portion at 11,034 metres (36,201 ft).[3]

At the bottom of the trench the water column above exerts a pressure of 1,086 bars (15,750 psi) (over 1000 times the standard atmospheric pressure at sea level). At this pressure, the density of water is increased by 4.96%, making 95 litres of water under the pressure of the Challenger Deep contain the same mass as 100 litres at the surface. The temperature at the bottom is 1 to 4 °C.[4]

The trench is not the part of the seafloor closest to the center of the Earth. This is because the Earth is not a perfect sphere; its radius is about 25 kilometres (16 mi) less at the poles than at the equator.[5] As a result, parts of the Arctic Ocean seabed are at least 13 kilometres (8.1 mi) closer to the Earth's center than the Challenger Deep seafloor.

Xenophyophores have been found in the trench by Scripps Institution of Oceanography researchers at a record depth of 10.6 km (6.6 mi) below the sea surface.[6] On 17 March 2013, researchers reported data that suggested microbial life forms thrive within the trench.[7][8]

Contents

  [hide] 

Mariana Trench

From Wikipedia, the free encyclopedia

  (Redirected from Mariana trench)

This article is about the deep sea trench. For the Canadian band named after the geological formation, see Marianas Trench (band).

Location of the Mariana Trench

The Mariana Trench or Marianas Trench[1] is the deepest part of the world's oceans. 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 with an average width of 69 kilometres (43 mi). It reaches a maximum-known depth of 10,994 m (± 40 m) or 6.831 mi (36,070 ± 131 ft) at a small slot-shaped valley in its floor known as the Challenger Deep, at its southern end,[2] although some unrepeated measurements place the deepest portion at 11,034 metres (36,201 ft).[3]

At the bottom of the trench the water column above exerts a pressure of 1,086 bars (15,750 psi) (over 1000 times the standard atmospheric pressure at sea level). At this pressure, the density of water is increased by 4.96%, making 95 litres of water under the pressure of the Challenger Deep contain the same mass as 100 litres at the surface. The temperature at the bottom is 1 to 4 °C.[4]

The trench is not the part of the seafloor closest to the center of the Earth. This is because the Earth is not a perfect sphere; its radius is about 25 kilometres (16 mi) less at the poles than at the equator.[5] As a result, parts of the Arctic Ocean seabed are at least 13 kilometres (8.1 mi) closer to the Earth's center than the Challenger Deep seafloor.

Xenophyophores have been found in the trench by Scripps Institution of Oceanography researchers at a record depth of 10.6 km (6.6 mi) below the sea surface.[6] On 17 March 2013, researchers reported data that suggested microbial life forms thrive within the trench.[7][8]

Contents

  [hide] 

Names[edit]

The Mariana Trench is named for the nearby Mariana Islands (in turn named Las Marianas in honor of Spanish Queen Mariana of Austria, widow of Philip IV of Spain). The islands are part of the island arc that is formed on an over-riding plate, called the Mariana Plate (also named for the islands), on the western side of the trench.

Geology[edit]

The Pacific plate is subducted beneath 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 Mariana Trench is part of the Izu-Bonin-Mariana subduction system that forms the boundarybetween two tectonic plates. In this system, the western edge of one plate, the Pacific Plate, issubducted (i.e., thrust) beneath the smaller Mariana Plate that lies to the west. Crustal material at the western edge of the Pacific Plate is some of the oldest oceanic crust on earth (up to 170 million years old), and is therefore cooler and more dense; hence its great height difference relative to the higher-riding (and younger) Mariana Plate. The deepest area at the plate boundary is the Mariana Trench proper.

The movement of the Pacific and Mariana plates is also indirectly responsible for the formation of theMariana Islands. These volcanic islands are caused by flux melting of the upper mantle due to release of water that is trapped in minerals of the subducted portion of the Pacific Plate.

Measurements[edit]

See also: Challenger Deep

The trench was first sounded during the Challenger expedition in 1875, which recorded a depth of 4,475 fathoms (8.184 km; 26,850 ft).[9] In 1877 a map was published called Tiefenkarte des Grossen Ozeans by Petermann, which showed a Challenger Tief at the location of that sounding. In 1899 USS Nero, a converted collier, recorded a depth of 5269 fathoms (9,636 m, 31,614 ft).[10] 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 (10.90 km; 35,760 ft) at 11°19′N 142°15′E, known as the Challenger Deep.[11]

In 1957, the Soviet vessel Vityaz reported a depth of 11,034 m (36,201 ft), dubbed the Mariana Hollow.[3]

In 1962, the surface ship M.V. Spencer F. Baird recorded a maximum depth of 10,915 m (35,840 ft), using precision depth gauges.

In 1984, the Japanese survey vessel Takuyō (拓洋) collected data from the Mariana Trench using a narrow, multi-beam echo sounder; it reported a maximum depth of 10,924 m (35,840 ft), also reported as 10,920 m (35,830 ft) ±10 m (33 ft),.[12]

Remotely Operated Vehicle KAIKO reached the deepest area of Mariana trench and made the deepest diving record of 10,911 m (35,797 ft) on March 24, 1995.[13]

During surveys carried out between 1997 and 2001, a spot was found along the Mariana Trench that had depth similar to that of 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.[14]

On 1 June 2009 sonar mapping of the Challenger Deep by the Simrad EM120 sonar multibeam bathymetry system for deep water, i.e. depths of 300–11,000 m (980–36,000 ft) 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 ± 22 metres).[15][16]

In 2011, it was announced at the American Geophysical Union Fall Meeting that a US Navy hydrographic ship equipped with a multibeam echosounder conducted a survey which mapped the entire trench to 100 m (330 ft) resolution.[2] The mapping revealed the existence of four rocky outcrops thought to be formerseamounts.[17]

The Mariana Trench is a site chosen by researchers at Washington University and the Woods Hole Oceanographic Institution in 2012 for a seismic survey to investigate the subsurface water cycle. Using both ocean-bottom seismometers and hydrophones the scientists are able to map structures as deep as 60 mi (97 km) beneath the surface.[18]

Descents[edit]

The bathyscaphe Trieste (designed by Auguste Piccard), the first manned vehicle to reach the bottom of the Marianas Trench.[19]

Four descents have been achieved. The first was the manned descent by Swiss-designed, Italian-built, United States Navy-owned bathyscaphe Trieste which reached the bottom at 1:06 pm on 23 January 1960, with Don Walsh and Jacques Piccardon board.[11][20] Iron shot was used for ballast, with gasoline for buoyancy.[11] The onboard systems indicated a depth of 11,521 m (37,799 ft), but this was later revised to 10,916 m (35,814 ft).[21] The depth was estimated from a conversion ofpressure measured and calculations based on the water density from sea surface to seabed.[20]

This was followed by the unmanned ROVs Kaikō in 1996 and Nereus in 2009. The first three expeditions directly measured very similar depths of 10,902 to 10,916 m (35,768 to 35,814 ft).

The fourth was made by Canadian film director James Cameron in 2012. On 26 March, he reached the bottom of the Mariana Trench in the submersible vessel Deepsea Challenger.[22][23][24]

In July 2015, members of the National Oceanic and Atmospheric Administration, Oregon State University, and the Coast Guard submerged a hydrophone into the deepest part of the Mariana Trench, the Challenger Deep. Never having deployed one past a mile, the titanium-shelled hydrophone was designed to withstand the immense pressure 7 miles under.[25]Although researchers were unable to retrieve the hydrophone until November, the data capacity was full within the first 23 days. After months of analyzing the sounds, the experts were surprised to pick up natural and man-made sounds such as boats, earthquakes, a typhoon, and baleen whales.[26] Due to the mission's success, the researchers plan to deploy a second hydrophone in 2017 for an extended period of time.

Planned descents[edit]

As of February 2012, at least two other teams are planning piloted submarines to reach the bottom of the Mariana Trench. These include: Triton Submarines, a Florida-based company that designs and manufactures private submarines, for which a crew of three will take 120 minutes to reach the seabed;[27] and DOER Marine, a marine technology company, based near San Francisco and set up in 1992, for which a crew of two or three will take 90 minutes to reach the seabed.[28]

Life[edit]

The expedition conducted in 1960 claimed to have observed (with great surprise because of the high pressure) large creatures living at the bottom, such as aflatfish about 30 cm (1 ft) long,[21] and shrimp.[29] According to Piccard, "The bottom appeared light and clear, a waste of firm diatomaceous ooze".[21] Many marine biologists are now skeptical of the supposed sighting of the flatfish, and it is suggested that the creature may instead have been a sea cucumber.[30][31]

During the second expedition, the unmanned vehicle Kaikō collected mud samples from the seabed.[32] Tiny organisms were found to be living in those samples.

In July 2011, a research expedition deployed untethered landers, called dropcams, equipped with digital video and lights to explore this region of the deep sea. Amongst many other living organisms, some gigantic single-celled amoebas with a size of more than 4 in (10 cm), belonging to the class of xenophyophores were observed.[33] Xenophyophores are noteworthy for their size, their extreme abundance on the seafloor and their role as hosts for a variety of organisms.

In December 2014, a new species of snailfish was discovered at a depth of 8,145 m (26,722 ft), breaking the previous record for the deepest living fish seen on video.[34] Several other new species were also filmed, including huge crustaceans known as supergiants.[34]

Possible nuclear waste disposal site[edit]

Like other oceanic trenches, the Mariana Trench has been proposed as a site for nuclear waste disposal,[35][36] in the hope that tectonic plate subduction occurring at the site might eventually push the nuclear waste deep into the Earth's mantle. However, ocean dumping of nuclear waste is prohibited by international law.[35][36][37] Furthermore, plate subduction zones are associated with very large megathrust earthquakes, the effects of which are unpredictable and possibly adverse to the safety of long-term disposal.[36] Also, disposal of nuclear wastes may cause havoc in the hadopelagic ecosystems.

See also[edit]

Mariana Trench

From Wikipedia, the free encyclopedia

  (Redirected from Mariana trench)

This article is about the deep sea trench. For the Canadian band named after the geological formation, see Marianas Trench (band).

Location of the Mariana Trench

The Mariana Trench or Marianas Trench[1] is the deepest part of the world's oceans. 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 with an average width of 69 kilometres (43 mi). It reaches a maximum-known depth of 10,994 m (± 40 m) or 6.831 mi (36,070 ± 131 ft) at a small slot-shaped valley in its floor known as the Challenger Deep, at its southern end,[2] although some unrepeated measurements place the deepest portion at 11,034 metres (36,201 ft).[3]

At the bottom of the trench the water column above exerts a pressure of 1,086 bars (15,750 psi) (over 1000 times the standard atmospheric pressure at sea level). At this pressure, the density of water is increased by 4.96%, making 95 litres of water under the pressure of the Challenger Deep contain the same mass as 100 litres at the surface. The temperature at the bottom is 1 to 4 °C.[4]

The trench is not the part of the seafloor closest to the center of the Earth. This is because the Earth is not a perfect sphere; its radius is about 25 kilometres (16 mi) less at the poles than at the equator.[5] As a result, parts of the Arctic Ocean seabed are at least 13 kilometres (8.1 mi) closer to the Earth's center than the Challenger Deep seafloor.

Xenophyophores have been found in the trench by Scripps Institution of Oceanography researchers at a record depth of 10.6 km (6.6 mi) below the sea surface.[6] On 17 March 2013, researchers reported data that suggested microbial life forms thrive within the trench.[7][8]

Contents

  [hide] 

Names[edit]

The Mariana Trench is named for the nearby Mariana Islands (in turn named Las Marianas in honor of Spanish Queen Mariana of Austria, widow of Philip IV of Spain). The islands are part of the island arc that is formed on an over-riding plate, called the Mariana Plate (also named for the islands), on the western side of the trench.

Geology[edit]

The Pacific plate is subducted beneath 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 Mariana Trench is part of the Izu-Bonin-Mariana subduction system that forms the boundarybetween two tectonic plates. In this system, the western edge of one plate, the Pacific Plate, issubducted (i.e., thrust) beneath the smaller Mariana Plate that lies to the west. Crustal material at the western edge of the Pacific Plate is some of the oldest oceanic crust on earth (up to 170 million years old), and is therefore cooler and more dense; hence its great height difference relative to the higher-riding (and younger) Mariana Plate. The deepest area at the plate boundary is the Mariana Trench proper.

The movement of the Pacific and Mariana plates is also indirectly responsible for the formation of theMariana Islands. These volcanic islands are caused by flux melting of the upper mantle due to release of water that is trapped in minerals of the subducted portion of the Pacific Plate.

Measurements[edit]

See also: Challenger Deep

The trench was first sounded during the Challenger expedition in 1875, which recorded a depth of 4,475 fathoms (8.184 km; 26,850 ft).[9] In 1877 a map was published called Tiefenkarte des Grossen Ozeans by Petermann, which showed a Challenger Tief at the location of that sounding. In 1899 USS Nero, a converted collier, recorded a depth of 5269 fathoms (9,636 m, 31,614 ft).[10] 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 (10.90 km; 35,760 ft) at 11°19′N 142°15′E, known as the Challenger Deep.[11]

In 1957, the Soviet vessel Vityaz reported a depth of 11,034 m (36,201 ft), dubbed the Mariana Hollow.[3]

In 1962, the surface ship M.V. Spencer F. Baird recorded a maximum depth of 10,915 m (35,840 ft), using precision depth gauges.

In 1984, the Japanese survey vessel Takuyō (拓洋) collected data from the Mariana Trench using a narrow, multi-beam echo sounder; it reported a maximum depth of 10,924 m (35,840 ft), also reported as 10,920 m (35,830 ft) ±10 m (33 ft),.[12]

Remotely Operated Vehicle KAIKO reached the deepest area of Mariana trench and made the deepest diving record of 10,911 m (35,797 ft) on March 24, 1995.[13]

During surveys carried out between 1997 and 2001, a spot was found along the Mariana Trench that had depth similar to that of 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.[14]

On 1 June 2009 sonar mapping of the Challenger Deep by the Simrad EM120 sonar multibeam bathymetry system for deep water, i.e. depths of 300–11,000 m (980–36,000 ft) 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 ± 22 metres).[15][16]

In 2011, it was announced at the American Geophysical Union Fall Meeting that a US Navy hydrographic ship equipped with a multibeam echosounder conducted a survey which mapped the entire trench to 100 m (330 ft) resolution.[2] The mapping revealed the existence of four rocky outcrops thought to be formerseamounts.[17]

The Mariana Trench is a site chosen by researchers at Washington University and the Woods Hole Oceanographic Institution in 2012 for a seismic survey to investigate the subsurface water cycle. Using both ocean-bottom seismometers and hydrophones the scientists are able to map structures as deep as 60 mi (97 km) beneath the surface.[18]

Descents[edit]

The bathyscaphe Trieste (designed by Auguste Piccard), the first manned vehicle to reach the bottom of the Marianas Trench.[19]

Four descents have been achieved. The first was the manned descent by Swiss-designed, Italian-built, United States Navy-owned bathyscaphe Trieste which reached the bottom at 1:06 pm on 23 January 1960, with Don Walsh and Jacques Piccardon board.[11][20] Iron shot was used for ballast, with gasoline for buoyancy.[11] The onboard systems indicated a depth of 11,521 m (37,799 ft), but this was later revised to 10,916 m (35,814 ft).[21] The depth was estimated from a conversion ofpressure measured and calculations based on the water density from sea surface to seabed.[20]

This was followed by the unmanned ROVs Kaikō in 1996 and Nereus in 2009. The first three expeditions directly measured very similar depths of 10,902 to 10,916 m (35,768 to 35,814 ft).

The fourth was made by Canadian film director James Cameron in 2012. On 26 March, he reached the bottom of the Mariana Trench in the submersible vessel Deepsea Challenger.[22][23][24]

In July 2015, members of the National Oceanic and Atmospheric Administration, Oregon State University, and the Coast Guard submerged a hydrophone into the deepest part of the Mariana Trench, the Challenger Deep. Never having deployed one past a mile, the titanium-shelled hydrophone was designed to withstand the immense pressure 7 miles under.[25]Although researchers were unable to retrieve the hydrophone until November, the data capacity was full within the first 23 days. After months of analyzing the sounds, the experts were surprised to pick up natural and man-made sounds such as boats, earthquakes, a typhoon, and baleen whales.[26] Due to the mission's success, the researchers plan to deploy a second hydrophone in 2017 for an extended period of time.

Planned descents[edit]

As of February 2012, at least two other teams are planning piloted submarines to reach the bottom of the Mariana Trench. These include: Triton Submarines, a Florida-based company that designs and manufactures private submarines, for which a crew of three will take 120 minutes to reach the seabed;[27] and DOER Marine, a marine technology company, based near San Francisco and set up in 1992, for which a crew of two or three will take 90 minutes to reach the seabed.[28]

Life[edit]

The expedition conducted in 1960 claimed to have observed (with great surprise because of the high pressure) large creatures living at the bottom, such as aflatfish about 30 cm (1 ft) long,[21] and shrimp.[29] According to Piccard, "The bottom appeared light and clear, a waste of firm diatomaceous ooze".[21] Many marine biologists are now skeptical of the supposed sighting of the flatfish, and it is suggested that the creature may instead have been a sea cucumber.[30][31]

During the second expedition, the unmanned vehicle Kaikō collected mud samples from the seabed.[32] Tiny organisms were found to be living in those samples.

In July 2011, a research expedition deployed untethered landers, called dropcams, equipped with digital video and lights to explore this region of the deep sea. Amongst many other living organisms, some gigantic single-celled amoebas with a size of more than 4 in (10 cm), belonging to the class of xenophyophores were observed.[33] Xenophyophores are noteworthy for their size, their extreme abundance on the seafloor and their role as hosts for a variety of organisms.

In December 2014, a new species of snailfish was discovered at a depth of 8,145 m (26,722 ft), breaking the previous record for the deepest living fish seen on video.[34] Several other new species were also filmed, including huge crustaceans known as supergiants.[34]

Possible nuclear waste disposal site[edit]

Like other oceanic trenches, the Mariana Trench has been proposed as a site for nuclear waste disposal,[35][36] in the hope that tectonic plate subduction occurring at the site might eventually push the nuclear waste deep into the Earth's mantle. However, ocean dumping of nuclear waste is prohibited by international law.[35][36][37] Furthermore, plate subduction zones are associated with very large megathrust earthquakes, the effects of which are unpredictable and possibly adverse to the safety of long-term disposal.[36] Also, disposal of nuclear wastes may cause havoc in the hadopelagic ecosystems.

See also[edit]

The Mariana Trench is named for the nearby Mariana Islands (in turn named Las Marianas in honor of Spanish Queen Mariana of Austria, widow of Philip IV of Spain). The islands are part of the island arc that is formed on an over-riding plate, called the Mariana Plate (also named for the islands), on the western side of the trench.

Geology[edit]

The Pacific plate is subducted beneath 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 Mariana Trench is part of the Izu-Bonin-Mariana subduction system that forms the boundarybetween two tectonic plates. In this system, the western edge of one plate, the Pacific Plate, issubducted (i.e., thrust) beneath the smaller Mariana Plate that lies to the west. Crustal material at the western edge of the Pacific Plate is some of the oldest oceanic crust on earth (up to 170 million years old), and is therefore cooler and more dense; hence its great height difference relative to the higher-riding (and younger) Mariana Plate. The deepest area at the plate boundary is the Mariana Trench proper.

The movement of the Pacific and Mariana plates is also indirectly responsible for the formation of theMariana Islands. These volcanic islands are caused by flux melting of the upper mantle due to release of water that is trapped in minerals of the subducted portion of the Pacific Plate.

Measurements[edit]

See also: Challenger Deep

The trench was first sounded during the Challenger expedition in 1875, which recorded a depth of 4,475 fathoms (8.184 km; 26,850 ft).[9] In 1877 a map was published called Tiefenkarte des Grossen Ozeans by Petermann, which showed a Challenger Tief at the location of that sounding. In 1899 USS Nero, a converted collier, recorded a depth of 5269 fathoms (9,636 m, 31,614 ft).[10] Challenger II surveyed the trench using echo sounding, a much more precise and vastly easier