All about Mid-Ocean Ridge | Physical Geography | UPSC

All about Mid-Ocean Ridge | Physical Geography | UPSC

The study of ocean floor has been made through various underwater expeditions and explorations. These underwater explorations have shown very contrasting and spectacular features inside the seas and oceans. When there is a Tsunami, everyone will say that it is due to the origin of earthquake below the sea floors. It is also a fact that the Earth’s tectonic processes are happening along the plate boundaries. These boundaries are very distinct lithological portions existing below the seas and oceans. The modern ocean floor maps have provided enormous opportunities to understand these underwater features. They also helped us to know the theories behind the earth’s ongoing tectonic processes.

Ocean’s morphological features vary with reference to their site, location, origin, morphology, lithology and dynamics of the water masses.

• The general profile of oceans include the Continental Shelf, Continental Slope and the Deep Ocean basins. Each one of these have their own variations in spread, depth, slope and hydrodynamics.
• The life in the marine waters depend on the depth, air-sea interactions, radiation, hydrodynamics, morphology and the physico-chemical conditions of the oceans.
• The Circulation of ocean waters, as waves and currents, and the interaction of oceans with the atmosphere, have very significant effects on the weather and climate of the entire globe.
• There are several kinds of distinct and most striking features observed on the ocean bottoms.
• These underwater relief features are very essential to our human understanding about the earth, oceans, oceanic crusts, tectonic processes and their impacts.

Among them, the Mid Ocean ridges are very unique structures.

The Mid Ocean Ridges, as the name implies, exist mostly in the middle of the ocean basins, where the divergent plate boundaries are located. The theory of Plate Tectonics has indicated many major tectonic processes which also include:

• the release of convection currents along Divergent Plate Boundaries,
• the origin of Mid Ocean ridges and
• the spreading of the sea floor.

All these processes are everlasting phenomena on the Planet Earth.

A basic understanding of the Mid Ocean Ridges is necessary not only for oceanographic point of view, but also for general knowledge point of view.

In this post, the following aspects of the Geological Oceanography are highlighted:

1. Ocean Relief features
2. Mid Oceanic Ridges
3. Formation of Oceanic Ridges
4. Distribution of Oceanic Ridges
5. Importance of Ridges.

Major Oceanic Relief features | UPSC – IAS

The painstaking ocean floor mapping Project of Bruce Heezen and Marie Tharp after the Second World War has shown the distinguishing underwater features of the world’s oceans. It is really a thought provoking highly heterogeneous relief system seen below the seas and oceans.

The profile of the oceans has shown innumerable curves, dips, ridges, valleys, mountains, plateaus, trenches, fractures and canyons.

The following major kinds of features have been observed based on the ocean floor expeditions and explorations made during the last 100 years.

They are: – Oceanic abyssal plains,  Oceanic trenches, Oceanic plateaus, Oceanic fracture zones, Seamounts and Mid ocean ridges

• An Abyssal Plain is an underwater plain located on the deep ocean floor. It is usually found at depths between 3000 m and 6000 m. These are the flattest, smoothest and least explored regions on the planet earth. Abyssal plains lie generally between the foot of a continental rise and a mid-ocean ridge.
• Oceanic Trenches are long, narrow topographic depressions of the sea bed. They are the boundary zones of lithospheric plates. An oceanic trench is a type of convergent boundary at which two lithospheric slabs meet. Trenches are generally parallel to the volcanic arcs. Oceanic Trenches extend 3 to 4 km deeper below the level of the surrounding ocean floor. The greatest depth is seen at the Challenger Deep of the Marianas Trench in the northwest Pacific Ocean. It extends upto a depth of 10911 m below the sea level. There are about 30 notable trenches existing in different oceans of the globe.
• An Oceanic Plateau is a large relatively flat region under the marine waters. They rise well above the average level of the seabed. There are about 16 oceanic plateaus existing in different regions of the oceans.
• A seamount is an underwater mountain rising from the ocean floor. It does not reach the water surface. Hence, it is not an island. Some of them are formed from extinct volcanoes. A seamount rises from 1000 m to 4000 m depth of water. There are about 100,000 seamounts existing across the globe.
• Submarine Canyons are long narrow and deep valleys cutting across the continental shelves and slopes. The depth of these Canyons may range from 600m to 3000m.

Among these, the Mid Oceanic Ridges are the most remarkable features existing along the Divergent plate boundaries. These are underwater mountain chains. They are not similar to the mountains of continents. The Mid Oceanic ridges cover about 23% of the earth’s surface. Their origin, extent and distribution are essential aspects to be studied in oceanography and physical geography.

Mid-ocean ridge | UPSC – IAS

One of the most striking features of the ocean floor is the distribution of mid oceanic ridges. These ridges are mountain-like structures standing well above the deep ocean floors. The mid oceanic ridges are, in total, 65,000 km long and cover almost 23% of the earth’s surface. These are considered as the world’s largest mountain ranges existing below marine waters. They exist as chains, in the centre of the oceanic basins. These are rugged features. They stand 1 to 3 km above the deep ocean floors. The most prominent feature of a ridge is its steep-sided central valley called rift valley. A rift valley may be 25 to 50 km wide and 1 to 2 km deep in its profile. The rift valley of a mid oceanic ridge is bordered by rugged mountains with the tallest peaks. These peaks may rise upto 2 km above the sea surface also as seen in some locations. Upwelling of molten mantle rock has created these rift zones.

The mid oceanic ridges are formed along the boundary between two divergent tectonic plates. These zones are tectonically active regions. Hence, small earthquakes occur frequently on crests of mid ocean ridges. These earthquakes coincide with the location of the central rift valleys. They are the most active volcanic regions on the earth.

At the mid oceanic ridges, two plates move away from each other. This process is called as sea-floor spreading and it creates a new seafloor. Ocean basins were formed through such breakup of continents and movement of plates. Thick continental crust was subjected to heat flow from earth’s interior. When the warm mantle expands, the continental crust is domed and stretched away from each other thereby forming the rift valleys. Some form of thermal convection within the asthenosphere appears to create

• New lithosphere at the oceanic ridges and rises. This simultaneously made the old lithosphere back into the mantle to be subducted beneath oceanic trench systems.
• The spreading rates of mid ocean ridges may be 2-3 cm per year. A mid ocean ridge has a steeper and more irregular topography as a result of a low spreading rate. The ridge consists of a high central axial zone, with a narrow crest.
• The mid ocean ridges and rises are offset by rugged fault scars called fracture zones. These linear bands of mountains and troughs intersect all oceanic ridges at intervals in right angles.
• The system of mid-ocean ridges ranks with the continents and ocean basins as one of the three main units exposed at the earth’s surface. They are – the topography, structure, areal extent and geological importance.
• The Mid-Atlantic ridge is the best known example in the world.
• It is 40,000 miles long encircling the whole world.
• The mid-Atlantic Ridge is centrally located between the eastern and western margins of the Atlantic Ocean. It is also about 2000 km wide.
• It is elongated in a general North-South direction and follows a sinuous course roughly parallel to the present coastlines. With reference to areal extent, it is one-third of the entire Atlantic ocean.

Formation of Oceanic ridges | UPSC – IAS

Mid ocean ridges are characteristic of sea floor spreading processes. These are very active zones wherein a new magma is expected to emerge on the ocean floor regularly. There are two processes responsible for the ocean floor spreading

• Mechanism – One is ridge-push and slab-pull process. Ridge-push occurs when the ridge pushes the tectonic plate away from the ridge, often towards the subduction zone. At the subduction zone, slab -pull come into effect. The other process is the mantle conveyor mechanism.

Mid oceanic ridges form new oceanic crusts.

Convection currents from the mantle moves up as magma and leaves through weak zones as volcanic eruptions creating new crust upon cooling. These are called as mid ocean ridge basalts. The rocks making up the crust below the seafloor are youngest at the axis of the ridge. Most oceanic crust in the ocean basins is less than 200 million years old. The crust is in a state of constant renewal at the ocean ridges .

Moving away from the ridges, the depth of the ocean increases progressively. The greatest depths are in the ocean trenches.

Alfred Wegener while proposing the old theory of continental drift in 1912, specified that mid oceanic ridges are continuously tearing open the ocean floors and make the magma to erupt from the deep interior. Later the theory of Plate Tectonics provided a better understanding of the movements of plates, spreading of ocean floors, underwater volcanic eruptions and formation of mid oceanic ridges.

It is also found that 20 volcanic eruptions occur every year along the se mid oceanic ridges. It is also seen that every year about 2.5 sq.km of new sea floor is formed by this process. With a crustal thickness of 1 to 2 km, this amounts to about 4 Cu .Km of new oceanic crust formed every year.

Distribution of Mid-Ocean Ridges in the World | UPSC – IAS

Mid oceanic Ridges are distributed in almost all major oceans of the world. They range from the longest mid Atlantic Ridge of one ocean floor to a small ridge of another ocean.

The Atlantic Ocean has the following notable ridges.

• The Mid Atlantic Ridge is a world famous ridge. It is the longest one in the world. It divides the Atlantic in the middle along the plate boundary. Its alignment is broken near the equator. It starts from Iceland in the north and ends near the Rouvet Island near the Antarctica. The Mid Atlantic Ridge is exactly following the boundary of coastlines and continental margins on both sides of the ocean. It is flanked by many ocean basins.
• The Reykjanes Ridge – The Reykjanes Ridge exists in the Reykjanes Basin near Iceland as the starting point of Mid Atlantic Ridge. Its continuity has been broken by a fracture zone.
• The Madeira Ridge is a small oceanic ridge located near Madeira, west of Morocco.
• The Atlantic Indian Ridge – The Atlantic Indian Ridge is existing at the Southern end of Mid Atlantic Ridge. It is about 2000 km long. It is located along the northern boundary of the Atlantic – Indian Basin.
• The South Scotia Ridge – The South Scotia Ridge is located near the southern tip of south America in the Scotia Sea.
• The Zapiola Ridge – The Zapiola Ridge is a small ridge in the Argentine Basin east of Argentina.
• The America – Antarctica Ridge. The America – Antarctica Ridge is located in the Southern Ocean, North of Antarctica. It has a North East – South West alignment. It is 1500 km long.
• The Astrid Ridge – The Astrid Ridge is a small ridge located in the Lazarev sea of Antarctica. It is at the southern part of Atlantic-Indian Basin.
• The Parnaiba Ridge – The Parnaiba Ridge is a minor ridge located near the equator in the west Atlantic and east of Amazon delta.
• Belem Ridge is yet another one in the Atlantic Ocean.
• The Ceard Ridge –The Ceard Ridge is located in the western end of Atlantic Ocean near the equator.
• The Barracuda Ridge -The Barracuda Ridge is located North of Barbados.
• The Blake Bahama Ridge – The Blake Bahama Ridge is located closer to Bahamas in the West Atlantic.
• The Eirik Ridge – The Eirik Ridge is a minor oceanic ridge located in the North Atlantic existing near the south of Greenland.
• The West Scotia Ridge – The West Scotia Ridge is located in the western parts of Scotia Sea.
• The Newfoundland Ridge – The Newfoundland Ridge is located in the north west Atlantic ocean near Newfoundland.
• The Walvis Ridge –The Walvis Ridge is located in the Southern Atlantic west of Namibia of South Africa.
• The Hatton Ridge – The Hatton Ridge is parallel to Reykjanes Ridge in the Iceland Basin.

The Pacific ocean has the following notable ridges:

• Gorda Ridges are located west of north America near Cascade mountain ranges.
• Kyushu – Palau Ridge is located in the middle of Philippine Sea.
• South Honshu Ridge
• West Norfolk Ridge and Norfolk Ridge are located near the Norfolk Island of Australia.
• Kermadec Ridge is located along the western parts of Southwest Pacific basin.
• Robbie Ridge is located to the southwest of Phoenix islands. It is a north-south trending ridge. It is parallel to the Kermadec trench.
• Hawaiian Ridge is located Northwest of Hawaii.
• Christmas Ridge and Necker Ridge are in the Central Pacific basin southwest of Hawaii.
• Tehuantepec Ridge is located in the Guatemala Basin South of Salina Cruz.
• Colon Ridge exists in southern parts of Guatemala Basin between north and south America in the east pacific.
• Pacific Antarctic Ridge is in the middle of the Southern ocean. It is an east-west trending ridge.
• Nazca Ridge is located west of South America near Peru-Chile trench.
• Society Ridge and Tuamotu Ridge are in the middle of the Pacific ocean near Society islands. It is in the southern Hemisphere.
• Macquarie Ridge is along the boundary between Southern Ocean and the Tasman Sea and South of New Zealand.
• Caroline Ridge is located near the Challenger Deep of Marianas Trench.
• Galapagos Ridge is located west of South America near Andes.

The Ridges of Indian Ocean are the following:

• Ninety East Ridge. It is a north-south trending ridge located in the middle of Cocos Basin and Mid-Indian Basin. It starts from the Andaman Sea in the North and extends upto the Broken Ridge in the South. It runs parallel to the longitude 90 degrees E.
• Investigator Ridge is located in the southeastern parts of Cocos basin and east of Cocos islands.
• Chain Ridge is located northeast of Somali Basin and North of Seychelles.
• Amirantle Ridge is near the Seychelles, south of Somali basin.
• Davie Ridge is located in the Mozambique Channel between Mozambique and Madagascar.
• Murray Ridge is in the Arabian Sea, east of Oman.
• Carlsberg Ridge is located south of Arabian Sea and northeast of Somali basin.
• Sheba Ridge is located in the Gulf of Aden extending from the red Sea.
• Atlantic Indian Ridge is in the south of Africa in the Atlantic-Indian basin.
• Southwest Indian Ridge is located in the southwest parts of Indian ocean. It is trending along NE-SW direction.
• Mid Indian Ridge is a Northwest to Southeast trending ridge in the middle of Indian Ocean.
• Broken Ridge is an east-west trending ridge located to the west of Perth basin.
• Southeast Indian Ridge is an east-west trending ridge located in the southeast parts of Indian Ocean.
• Hartog Ridge is in the western parts of Perth basin west of Australia.
• East Indiaman Ridge is near the Broken Ridge west of the Perth Basin.

Significance of Oceanic Ridge | UPSC – IAS

The alignments of the ridges have some common trends. The ridges are structurally displaced due to transform faults. Their alignments are cut across by a series of transform faults. The horizontal displacement along these zones bring more opportunities to expose the crustal weaknesses. The length of volcanic vents or pipes may be shortened and due to this more convection currents may emanate rapidly. Due to this, the rising of magma could be more easy.

• When there is subduction along the convergent boundaries, we get ocean trenches. Below the zones of subduction, the materials get crushed and may be melted. This zone of crushing is known as benioff zone. The scientists believe that the volcanic island arcs are formed from magmas produced by the partial melting of the descending and/or the overriding plate. Considerable volcanic activity worldwide is the result of subduction.
• Benioff is the zone which normally creates the focus for earthquakes and subsequently generate tsunamis from the oceans. Ocean ridges are the spreading centers. The ocean floor is mountainous and uneven, much like Earth’s surface.
• Sea-floor spreading is driven by the crust formation along these mid-ocean ridges. They are like meandering undersea mountain ranges. They span on the Earth like the seams of a baseball. Oceanic crust is continually produced by magma welling up along the centerlines of the mid-ocean ridges. This new crust flows away from the ridgeline in two symmetric sheets, one on each side. The rate of sea-floor spreading resulting from this process is from 1–20 cm/yr, depending on the particular mid-ocean ridge.
• Oceanography is one of the interesting subjects of earth sciences. Studying the underwater features are challenging tasks. The processes behind these features are challenging us though we are far away from them. Let us see the other important ones in the forthcoming modules.

FAQs about Oceanic floor and Mid – Oceanic Ridge

What are the features of continental shelf?

• Continental shelf is the broad, relatively shallow submarine platform that forms a border to a continent. It extends from the coast to depths of 100 – 200 m. Continental shelves average about 65 km in width. They exists almost everywhere. They are simply a continuation of the continental landmass. Continental shelves are usually covered with a layer of sand, silts, and silty muds. Their surfaces feature small hills and ridges that alternate with shallow depressions and valley-like troughs. In a few cases, steep-walled V-shaped submarine canyons cut deeply into both the shelf and the slope below.

What are abyssal plains?

• An Abyssal Plain is an underwater plain located on the deep ocean floor. It is usually found at depths between 3000 m and 6000 m. These are the flattest, smoothest and least explored regions on the planet earth. Abyssal plains lie generally between the foot of a continental rise and a mid-ocean ridge.
• The abyssal plains lying at depths of 5000- 6000 m are nearly flat. This is mainly due to sedimentation. They are found mostly in the Atlantic and are absent in the eastern Indian and most of the Pacific ocean floors. If there are no plains, then there may be oceanic trenches. Trenches are long narrow depressions in the ocean floor. They reach a depth of about 7000m to 11000 m below sea level. they occupy 1% of the surface of the earth

What is meant by a continental rise?

• A continental rise is merely a general region where the floor of the deep ocean basin rises to a greater and steeper slope. At the base of continental slope, the topographic gradient decreases to 1° (or) less and the ocean enters into the abyssal plains or hills.
• This portion of the sea floor is known as continental rise. This is a product of deposition by turbidity current, underwater landslides and many other processes. The lower portion of continental slopes normally grade into the continental rise. They do not have any sharply defined boundaries.

What are mid-ocean ridges?

• One of the most striking features of the ocean floor is the distribution of mid oceanic ridges. These ridges are mountain-like structures standing well above the deep ocean floors. The mid oceanic ridges are, in total, 65,000 km long and cover almost 23% of the earth’s surface.
• These are considered as the world’s largest mountain ranges existing below marine waters. They exist as chains, in the centre of the oceanic basins. These are rugged features. They stand 1 to 3 km above the deep ocean floors.
• The mid-ocean ridges and rises are formed in zones of tension where plates diverge. The mountains of ocean ridges are not similar to the mountains of continents. The ocean
• ridges are composed entirely of basalts and are not deformed by any folding. The ridges are of two types as active spreading centre ridge and rise and inactive, aseismic ridge. The active spreading ridges are about 1000 km wide and 1 to 2 km high. Oceanic ridges are traversed by series of fractures with steep sides running perpendicular to ridges (or) rises.

What are oceanic trenches?

• Oceans have three more important features like Oceanic Trenches, Plains, and Ridges. The deepest part of the oceans have shown V-shaped trenches running for thousands of kilometers in length with a width of hundreds of kilometers and extend upto a depth of 3 to 4 km.
• There are numerous Ocean Trenches inside the water masses, beyond continental rise. The greatest depths of oceans can be seen only in the form of ocean trenches. These are steep sided, long narrow and hollow portions. They may be 300-500 km in length and 30-100 km wide with a depth of 6 km.
• Initially, their sides slope at 4 to 8° and then goes upto 16° to depths more than 10 km. For those parts of a depression which exceed 6000 m in depth, the term Ocean deep is used. Ocean trenches are formed due to subduction of the oceanic crust. The faults which transect these ridges are called as Transform faults.

What are island arcs?

• Island arcs are curved chain of volcanic islands. They are generally convex towards the open sea. Due to this nature, they are called as Arcs. There are hundred and thousands of extinct volcanoes in the ocean floors.
• These regions are seismically active zones. Island arcs are topographically and structurally continuous features. These are formed when two oceanic plates converge and collide. The melting of the descending plate rises upwards as an extended magma, to form the islands. Most of these eruptions are unnoticed.

What are seamounts?

• Seamounts and Guyots are some more unique features of the ocean basins. Seamounts are isolated steep sided submarine volcanic mounts. The base of the seamount is on the seafloor and its summit doesn’t reach the water surface (if it did, it would be an island). There are thousands of seamounts located throughout the world’s oceans.
• They may be 2-100 km wide and < 1 km high above the sea floor. Very rarely, they rise above the sea level as seen in Hawaii islands. Seamounts are made by extrusion of lavas piped upward in stages. Seamounts provide evidences and data on the movements of tectonic plates on which they ride.
• The trend of a seamount chain traces the direction of motion of the lithospheric plate over a more or less fixed heat source in the underlying asthenosphere part of the Earth’s mantle.

What are Guyots?

• Guyots are flat-topped seamounts. Guyot is a truncated seafloor volcano occurring as a flat-topped mountain which does not reach the sea surface. Guyots are thought to be associated with hot spots.
• The flat-top is created due to wave action. They are named after the Swiss-American geographer and geologist Arnold Henry Guyot.
• A guyot is also known as a tablemount. It occurs as a flat top mountain over 200 meters below the surface of the sea. The diameters of these flat summits can exceed 10 km. Guyots are most commonly found in the Pacific Ocean. Their flatness is due to erosion by waves, winds, and atmospheric processes. The steepness gradient of most guyots is about 20 degrees.

What are submarine canyons?

• As the name implies Submarine Canyons are deep narrow valleys of the continents extending inside the oceans. A submarine canyon is a steep-sided valley on the sea floor of the continental slope. Many submarine canyons are found as extensions to large rivers; however there are some that have no such association. Canyons cutting the continental slopes have been found at depths greater than 2 km below sea level.
• They are formed by powerful turbidity currents, volcanic and earthquake activity. Many submarine canyons continue as submarine channels across continental rise areas and may extend for hundreds of kilometers. Submarine canyons serve as major conduits for transporting sediment from land and the shelf to the deep-sea floor.
• Undersea canyons are prominent erosional features along both the U.S. Pacific and Atlantic continental margins. Similarly, the distinction between submarine canyons and submarine erosional channels is not straightforward. Thus, alternative terms, such as gullies, channels, troughs, trenches, fault valleys, and sea valleys, have been used for submarine canyons.
• A submarine canyon may begin as a river pours into the ocean, eroding a channel in the shallow continental shelf. But much of the carving may be done by torrents of muddy water stirred up by storms, earthquakes, or other big events.

What are the characteristics of Mid-Atlantic Ridge?

• The Mid Atlantic Ridge is a world famous ridge. It is the longest one in the world. It divides the Atlantic in the middle along the plate boundary. Its alignment is broken near the equator. It starts from Iceland in the north and ends near the Rouvet Island near the Antarctica.
• The Mid Atlantic Ridge is exactly following the boundary of coastlines and continental margins on both sides of the ocean. It is flanked by many ocean basins. The Reykjanes Ridge exists in the Reykjanes Basin near Iceland as the starting point of Mid Atlantic Ridge. Its continuity has been broken by a fracture zone.

What is meant by Seafloor spreading?

• Seafloor spreading is a process that occurs at mid-ocean ridges, where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge. Seafloor spreading helps explain continental drift in the theory of plate tectonics. At the mid oceanic ridges, two plates move away from each other. This process is called as sea-floor spreading and it creates a new sea floor.
• Ocean basins were formed through such breakup of continents and movement of plates. Thick continental crust was subjected to heat flow from earth’s interior. When the warm mantle expands, the continental crust is domed and stretched away from each other thereby forming the rift valleys.
• Some form of thermal convection within the asthenosphere appears to create new lithosphere at the oceanic ridges and rises. This simultaneously made the old lithosphere back into the mantle to be subducted beneath oceanic trench systems.

What are rift valleys?

• A rift valley is a long valley formed along a rift in the earth’s crust due to the gradual sinking of land between two parallel series of faults.
• A rift valley may be 25 to 50 km wide and 1 to 2 km deep in its profile. The rift valley of a mid oceanic ridge is bordered by rugged mountains with the tallest peaks. These peaks may raise upto 2 km above the sea surface also as seen in some locations. Upwelling of molten mantle rock has created these rift zones.