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Trench: very deep, elongated cavity bordering a continent or an island arc; it forms when one tectonic plate slides beneath another. Ridge: underwater mountain range that criss-crosses the oceans and is formed by rising magma in a zone where two plates are moving apart.

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Ridges are linear features that wind more than 60,000 km around the globe, constituting the major diverging boundaries of Earth’s tectonic plates. Hotspots, on the other hand, are localized regions of abnormally robust magmatism and distinctive geochemical anomalies (Figure 1).

A hot spot is an upwelling of magma from far beneath the Earth’s crust, caused by a disturbance at the boundary between the solid mantle and the liquid outer core of Earth’s interior. Hot spots are, compared to mid-ocean ridges or subduction zones, relatively small and isolated features.

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Since hot rocks are in a more expanded state and then contract as they cool (as they spread away from the ridge), the midocean ridges stand up high above the surrounding seafloor. The seafloor depth increases with distance away from the midocean ridges.

At the deep-sea trenches, two plates converge, with one plate sliding down under the other into the mantle where it is melted. Thus, for each segment of new ocean floor created at the ridges, an equal amount of old oceanic crust is destroyed at the trenches, or so-called subduction zones.

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The Mariana Trench, in the South Pacific Ocean, is formed as the mighty Pacific plate subducts beneath the smaller, less-dense Philippine plate. In a subduction zone, some of the molten material”the former seafloor”can rise through volcanoes located near the trench.

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Oceanic crust formed at spreading ridges is relatively homogeneous in thickness and composition compared to continental crust. On average, oceanic crust is 6″7 km thick and basaltic in composition as compared to the continental crust which averages 35″40 km thick and has a roughly andesitic composition.

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The Mid-Atlantic Ridge runs down the center of the Atlantic Ocean. It spread apart at rates of 2 to 5 cm per year, and at these relatively slow spreading rates, the ridge has a deep rift valley along its crest. The rift valley is 1 to 3 km deep, about the depth and width of the Grand Canyon.

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The continents are embedded in the plates. Many continents occur in the middles of plates, not at their boundaries or edges. Plates also underlie the Earth’s oceans. A single plate often includes both continental and oceanic regions.

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Submarine canyons are so called because they resemble canyons made by rivers on land. Unlike deep-sea trenches, which are found in areas where one tectonic plate slides beneath another, undersea canyons are found along the slopes of most continental margins.

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The Mid-Atlantic Ridge, for instance, is a slow spreading center. It spreads 2-5 centimeters (. 8-2 inches) every year and forms an ocean trench about the size of the Grand Canyon. The East Pacific Rise, on the other hand, is a fast spreading center.

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Coarse lithogenous / terrigenous sediments are dominant near the continental margins as runoff , river discharge, and other processes deposit vast amounts of these materials on the continental shelf (section 12.2).

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Continental arc magmas are more viscous than continental rift magmas. How are island arc and continental arc magmas similar? A. Both are formed near transform boundaries.

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Trenches are formed by subduction, a geophysical process in which two or more of Earth’s tectonic plates converge and the older, denser plate is pushed beneath the lighter plate and deep into the mantle, causing the seafloor and outermost crust (the lithosphere) to bend and form a steep, V-shaped depression.

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The seafloor contains deposits of minerals that we use in everyday life such as copper, zinc, nickel, gold, silver, and phosphorus. These deposits occur as crusts on volcanic and other rocks and as nodules on abyssal plain sediment that are typically about 3 to 10 centimeters (1 to 4 inches) in diameter.

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A seamount is an underwater sea mountain formed by plate tectonics and volcanic activity. Seamounts form near the boundaries of tectonic plates and hotspots (Image 1). Plates force ocean and crust to descend towards Earth’s hot interior as they converge and collide near subduction zones.

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What is the difference between a seamount and a guyot? A seamount is a submerged volcanic peak that hasn’t ever reached ocean’s surface. Guyots are once active, flat, topped volcanoes that used to be above the ocean surface but the tap was eroded away and it is now submerged.

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There may be 30,000 seamounts in the Pacific Ocean alone. Less than 1% have been explored.

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Most seamounts are remnants of extinct volcanoes. Typically, they are cone shaped, but often have other prominent features such as craters and linear ridges and some, called guyots, have large, flat summits.

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Seamounts and knolls are typically formed by volcanic activity. Seamounts rise at least 1,000 meters (about 3,200 feet) above the seafloor, whereas the height of knolls is smaller and ranges from approximately 500 to 1000 meters.

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The material that erupts at spreading centers along the mid-ocean ridge is primarily basalt, the most common rock on Earth. Because this spreading occurs on a sphere, the rate separation along the mid-ocean ridge varies around the globe.

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seamount, large submarine volcanic mountain rising at least 1,000 m (3,300 feet) above the surrounding deep-sea floor; smaller submarine volcanoes are called sea knolls, and flat-topped seamounts are called guyots.

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Deep-sea trenches generally lie seaward of and parallel to adjacent island arcs or mountain ranges of the continental margins. They are closely associated with and found in subduction zones”that is, locations where a lithospheric plate bearing oceanic crust slides down into the upper mantle under the force of gravity.

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As opposed to a flat seafloor, seamounts rise off the ocean bottom and interact with water flowing around them. These water currents can wash off sediment on a seamount, exposing rocks that are ideal habitat for animals that require hard substrate to grow and attach.

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At that point erosion of the volcano and subsidence of the seafloor cause the volcano to gradually diminish. As the volcano sinks and erodes, it first becomes an atoll island and then an atoll. Further subsidence causes the volcano to sink below the sea surface, becoming a seamount and/or a guyot.

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Seamounts have a big effect on the deep-sea environment. They accelerate ocean currents, generate waves, increase upwelling, and amplify tides. These changes improve the food and nutrient supply for filter feeders while removing waste and reducing sediment build-up.

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Seamounts are underwater mountains of volcanic origin that rise from the seafloor. Regarded as hotspots of biological diversity in the ocean, seamounts serve as spawning sites for many species. Marine mammals such as whales and dolphins and large predators such as sharks rely on them to feed and rest during migrations.

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When volcanoes form on the seafloor, they build up over time as they erupt volcanic lava that cools to become basalt. If a volcano does not reach the surface of the ocean, it is called a seamount.

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Because seamounts are isolated from each other they form “undersea islands” creating the same biogeographical interest. As they are formed from volcanic rock, the substrate is much harder than the surrounding sedimentary deep sea floor.

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Seamounts are commonly found near the boundaries of Earth’s tectonic plates and mid-plate near hotspots. At mid-ocean ridges, plates are spreading apart and magma rises to fill the gaps.

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A mid-ocean ridge (or mid-oceanic ridge) is an underwater mountain range, typically having a valley known as a rift running along its axis, formed by plate tectonics. This type of oceanic ridge is characteristic of what is known as an oceanic spreading center.

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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.

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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.

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When a hot spot interacts with a mid-ocean ridge, the affected ridge segments tend to receive a greater-than-normal supply of magma from the mantle, leading to more frequent eruptions, and formation of volcanic edifices right on the ridge.

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The buoyant rise of hot material transports heat to the surface from the deep interior while colder material sinks at subduction zones. Mid-ocean ridges and hot- spots are major expressions of heat dissipation at Earth’s surface, as evidenced by their abundant volcanic activity.

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Mid-ocean ridges occur along divergent plate boundaries, where new ocean floor is created as the Earth’s tectonic plates spread apart. As the plates separate, molten rock rises to the seafloor, producing enormous volcanic eruptions of basalt.

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1 Answer. A mid ocean ridge is a divergent boundary where hot magma from the mantle comes to the surface under the ocean creating mountains and undersea volcanos.

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They are all caused by what we call “hotspot” volcanic activity. This occurs where one of earth’s outer tectonic plates moves over an unusually hot part of the earth’s mantle.

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Ridges are linear features that wind more than 60,000 km around the globe, constituting the major diverging boundaries of Earth’s tectonic plates. Hotspots, on the other hand, are localized regions of abnormally robust magmatism and distinctive geochemical anomalies (Figure 1).

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Why is the mid-ocean ridge topographically elevated above the surrounding ocean floor? Most materials become less dense when heated and increase in density when cooled. Areas along the mid-ocean ridge are hot and therefore lower density and buoyant. They want to “float” and are therefore elevated.

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Since hot rocks are in a more expanded state and then contract as they cool (as they spread away from the ridge), the midocean ridges stand up high above the surrounding seafloor. The seafloor depth increases with distance away from the midocean ridges.

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It formed and evolves as a result of spreading in Earth’s lithosphere”the crust and upper mantle”at the divergent boundaries between tectonic plates. The vast majority of volcanic activity on the planet occurs along the mid-ocean ridge, and it is the place where the crust of the Earth is born.

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Principal characteristics. Oceanic ridges are found in every ocean basin and appear to girdle Earth. The ridges rise from depths near 5 km (3 miles) to an essentially uniform depth of about 2.6 km (1.6 miles) and are roughly symmetrical in cross section. They can be thousands of kilometres wide.

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Definition of mid-ocean ridge : an elevated region with a central valley on an ocean floor at the boundary between two diverging tectonic plates where new crust forms from upwelling magma.

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The age, density, and thickness of oceanic crust increases with distance from the mid-ocean ridge. The magnetism of mid-ocean ridges helped scientists first identify the process of seafloor spreading in the early 20th century.

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The flow of the materials goes through the upper mantle and leaks through the plates of the crust. This makes the temperature near the mid-oceanic ridge becomes warm and the other surface to become cold because as the molten magma continues to push upward, it moves the rocks away from the ridge.

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