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EspañolMID-OCEAN RIDGE
(Redirected from Ocean ridge)
A 'mid-ocean ridge' or 'mid-oceanic ridge' is an underwater mountain range, formed by plate tectonics. This uplifting of the ocean floor occurs when convection currents rise in the mantle beneath the oceanic crust and create magma where two tectonic plates meet at a divergent boundary. The mid-ocean ridges of the world are connected and form a single global mid-oceanic ridge system that is part of every ocean, making the mid-oceanic ridge system the longest mountain range in the world. The continuous mountain range is 65,000 km (40,000 miles) long and the total length of the system is 80,000 km (50,000 miles)[1].
Mid-ocean ridges are geologically active, with new magma constantly emerging onto the ocean floor and into the crust at and near rifts along the ridge axes. The crystallized magma forms new crust of basalt and gabbro.
The rocks making up the crust below the sea floor are youngest at the axis of the ridge and age with increasing distance from that axis. New magma of basalt composition emerges at and near the axis because of decompression melting in the underlying Earth's mantle.
The oceanic crust is made up of rocks much younger than the Earth itself: most oceanic crust in the ocean basins is less than 200 million years old. The crust is in a constant state of 'renewal' at the ocean ridges. Moving away from the mid-ocean ridge, ocean depth progressively increases; the greatest depths are in ocean trenches. As the oceanic crust moves away from the ridge axis, the peridotite in the underlying mantle cools and becomes more rigid. The crust and the relatively rigid peridotite below it make up the oceanic lithosphere.
There are two processes, ridge-push and slab-pull, thought to be responsible for the spreading seen at mid-ocean ridges, and there is some uncertainty as to which is dominant. Ridge-push occurs when the weight of the ridge pushes the rest of the tectonic plate away from the ridge, often towards a subduction zone. At the subduction zone, "slab-pull" comes into effect. This is simply the weight of the tectonic plate being subducted (pulled) below the overlying plate dragging the rest of the plate along behind it.
The other process proposed to contribute to the formation of new oceanic crust at mid-ocean ridges is the "mantle conveyor" (see image). However, there have been some studies which have shown that the upper mantle (asthenosphere) is too plastic (flexible) to generate enough friction to pull the tectonic plate along. Moreover, unlike in the image above, mantle upwelling that causes magma to form beneath the ocean ridges appears to involve only the mantle above about 400 km depth, as deduced from seismic tomography and from studies of the seismic discontinuity at about 400 km. The relatively shallow depths from which the upwelling mantle rises below ridges are more consistent with the "slab-pull" process.
The rate at which the mid-ocean ridge creates new material is known as the spreading rate, and is generally measured in mm/yr. The common subdivisions of spreading rate are fast, medium and slow, whose values are generally >100 mm/yr, ~60 mm/yr, and <20 mm/yr respectively. The spreading rate of the north Atlantic Ocean is 10 mm/yr, while in the Pacific region, it is 40-60 mm/yr.
The mid-ocean ridge systems form new oceanic crust. As crystallized basalt extruded at a ridge axis cools below Curie points of appropriate iron-titanium oxides, magnetic field directions parallel to the Earth's magnetic field are recorded in those oxides. The orientations of the field in the oceanic crust record preserve a record of directions of the Earth's magnetic field with time. Because the field has reversed directions at irregular intervals throughout its history, the pattern of reversals in the ocean crust can be used as an indicator of age. Likewise, the pattern of reversals together with age measurements of the crust is used to help establish the history of the Earth's magnetic field.
Because a mid-ocean ridge is submerged at very deep depths in the ocean, its existence was not even known until the 1950s, when it was discovered through surveys of the ocean floor conducted by research ships.
More specifically, the ''Vema'', a ship of the Lamont-Doherty Geological Observatory of Columbia University, traversed the Atlantic Ocean, recorded data about the ocean floor from the ocean surface. A team lead by Marie Tharp and Bruce Heezen analyzed the data and concluded that there was an enormous mountain chain running along the middle of the Atlantic. The mountain range was named the Mid-Atlantic Ridge; it remains the most famous part of the mid-ocean ridge.
At first, it was thought to be a phenomenon specific to the Atlantic Ocean, because nothing like such a massively-long undersea mountain chain had ever been discovered before. However, as surveys of the ocean floor continued to be conducted around the world, it was discovered that every ocean contained parts of the mid-ocean ridge.
Alfred Wegener proposed the theory of continental drift in 1912. However, the theory was dismissed by geologists because there was no mechanism to explain how continents could plow through ocean crust, and the theory became largely forgotten.
Following the discovery of the mid-ocean ridge in the 1950s, geologists faced a new task: explaining how such an enormous geological structure could have formed. In the 1960s, geologists discovered and began to propose mechanisms for sea floor spreading. Plate tectonics was a suitable explanation for sea floor spreading, and the acceptance of plate tectonics by the majority of geologists resulted in a major paradigm shift in geological thinking.
★ Atlantic-Indian Ridge
★ East Pacific Rise
★ Explorer Ridge
★ Gakkel Ridge (Mid-Arctic Ridge)
★ Gorda Ridge
★ Juan de Fuca Ridge
★ Mid-Atlantic Ridge
★ Mid-Indian Ridge
★ Nazca Ridge
★ Pacific-Antarctic Ridge
★ Reykjanes Ridge
★ Central Indian Ridge
★ Southeast Indian Rise
★ Southwest Indian Ridge
★ Phoenix Ridge
★ Izanagi Ridge
★ Kula Ridge
★ Farallon Ridge
★ Bellingshausen Ridge
★ Iceland
★ Oceanic trench
★ plate tectonics
★ list of landforms
★ Ridge push
★ Slab pull
★ Oceanic Crust
1. Cambridge Encyclopedia 2005
★ An explanation of relevant tectonic forces
Oceanic Ridge
Oceanic crust is formed at an oceanic ridge, while the lithosphere is subducted back into the asthenosphere at trenches.
A 'mid-ocean ridge' or 'mid-oceanic ridge' is an underwater mountain range, formed by plate tectonics. This uplifting of the ocean floor occurs when convection currents rise in the mantle beneath the oceanic crust and create magma where two tectonic plates meet at a divergent boundary. The mid-ocean ridges of the world are connected and form a single global mid-oceanic ridge system that is part of every ocean, making the mid-oceanic ridge system the longest mountain range in the world. The continuous mountain range is 65,000 km (40,000 miles) long and the total length of the system is 80,000 km (50,000 miles)[1].
| Contents |
| Description |
| Formation processes |
| Discovery |
| Impact |
| List of oceanic ridges |
| List of ancient oceanic ridges |
| See also |
| Notes |
| External link |
Description
Mid-ocean ridges are geologically active, with new magma constantly emerging onto the ocean floor and into the crust at and near rifts along the ridge axes. The crystallized magma forms new crust of basalt and gabbro.
The rocks making up the crust below the sea floor are youngest at the axis of the ridge and age with increasing distance from that axis. New magma of basalt composition emerges at and near the axis because of decompression melting in the underlying Earth's mantle.
The oceanic crust is made up of rocks much younger than the Earth itself: most oceanic crust in the ocean basins is less than 200 million years old. The crust is in a constant state of 'renewal' at the ocean ridges. Moving away from the mid-ocean ridge, ocean depth progressively increases; the greatest depths are in ocean trenches. As the oceanic crust moves away from the ridge axis, the peridotite in the underlying mantle cools and becomes more rigid. The crust and the relatively rigid peridotite below it make up the oceanic lithosphere.
Formation processes
There are two processes, ridge-push and slab-pull, thought to be responsible for the spreading seen at mid-ocean ridges, and there is some uncertainty as to which is dominant. Ridge-push occurs when the weight of the ridge pushes the rest of the tectonic plate away from the ridge, often towards a subduction zone. At the subduction zone, "slab-pull" comes into effect. This is simply the weight of the tectonic plate being subducted (pulled) below the overlying plate dragging the rest of the plate along behind it.
The other process proposed to contribute to the formation of new oceanic crust at mid-ocean ridges is the "mantle conveyor" (see image). However, there have been some studies which have shown that the upper mantle (asthenosphere) is too plastic (flexible) to generate enough friction to pull the tectonic plate along. Moreover, unlike in the image above, mantle upwelling that causes magma to form beneath the ocean ridges appears to involve only the mantle above about 400 km depth, as deduced from seismic tomography and from studies of the seismic discontinuity at about 400 km. The relatively shallow depths from which the upwelling mantle rises below ridges are more consistent with the "slab-pull" process.
The rate at which the mid-ocean ridge creates new material is known as the spreading rate, and is generally measured in mm/yr. The common subdivisions of spreading rate are fast, medium and slow, whose values are generally >100 mm/yr, ~60 mm/yr, and <20 mm/yr respectively. The spreading rate of the north Atlantic Ocean is 10 mm/yr, while in the Pacific region, it is 40-60 mm/yr.
The mid-ocean ridge systems form new oceanic crust. As crystallized basalt extruded at a ridge axis cools below Curie points of appropriate iron-titanium oxides, magnetic field directions parallel to the Earth's magnetic field are recorded in those oxides. The orientations of the field in the oceanic crust record preserve a record of directions of the Earth's magnetic field with time. Because the field has reversed directions at irregular intervals throughout its history, the pattern of reversals in the ocean crust can be used as an indicator of age. Likewise, the pattern of reversals together with age measurements of the crust is used to help establish the history of the Earth's magnetic field.
Discovery
Because a mid-ocean ridge is submerged at very deep depths in the ocean, its existence was not even known until the 1950s, when it was discovered through surveys of the ocean floor conducted by research ships.
More specifically, the ''Vema'', a ship of the Lamont-Doherty Geological Observatory of Columbia University, traversed the Atlantic Ocean, recorded data about the ocean floor from the ocean surface. A team lead by Marie Tharp and Bruce Heezen analyzed the data and concluded that there was an enormous mountain chain running along the middle of the Atlantic. The mountain range was named the Mid-Atlantic Ridge; it remains the most famous part of the mid-ocean ridge.
At first, it was thought to be a phenomenon specific to the Atlantic Ocean, because nothing like such a massively-long undersea mountain chain had ever been discovered before. However, as surveys of the ocean floor continued to be conducted around the world, it was discovered that every ocean contained parts of the mid-ocean ridge.
Impact
Plates in the crust of the earth, according to the plate tectonics theory
Alfred Wegener proposed the theory of continental drift in 1912. However, the theory was dismissed by geologists because there was no mechanism to explain how continents could plow through ocean crust, and the theory became largely forgotten.
Following the discovery of the mid-ocean ridge in the 1950s, geologists faced a new task: explaining how such an enormous geological structure could have formed. In the 1960s, geologists discovered and began to propose mechanisms for sea floor spreading. Plate tectonics was a suitable explanation for sea floor spreading, and the acceptance of plate tectonics by the majority of geologists resulted in a major paradigm shift in geological thinking.
List of oceanic ridges
★ Atlantic-Indian Ridge
★ East Pacific Rise
★ Explorer Ridge
★ Gakkel Ridge (Mid-Arctic Ridge)
★ Gorda Ridge
★ Juan de Fuca Ridge
★ Mid-Atlantic Ridge
★ Mid-Indian Ridge
★ Nazca Ridge
★ Pacific-Antarctic Ridge
★ Reykjanes Ridge
★ Central Indian Ridge
★ Southeast Indian Rise
★ Southwest Indian Ridge
List of ancient oceanic ridges
★ Phoenix Ridge
★ Izanagi Ridge
★ Kula Ridge
★ Farallon Ridge
★ Bellingshausen Ridge
See also
★ Iceland
★ Oceanic trench
★ plate tectonics
★ list of landforms
★ Ridge push
★ Slab pull
★ Oceanic Crust
Notes
1. Cambridge Encyclopedia 2005
External link
★ An explanation of relevant tectonic forces
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