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why do volcanoes form at subduction zones

Introduction Subduction zones are convergent boundaries where at least one of the tectonic plates is an oceanic crust. The new oceanic crust that forms in spreading centers is recycled in these zones. Subducting oceanic plate The oceanic crust melts as it descends into the lithosphere and upper mantle. Subducting plates ring the Pacific Ocean creating volcanic arcs and megathrust earthquakes
beneath a continental plate. USGS Converging crustal plates Subduction areas develop when a continental crust converges with an oceanic crust. The heavier oceanic crust bends and begins moving downward toward the upper mantle. Recent studies indicate that the subducting plate is pulled downward by gravity. Oceanic plate begins to melt The water soaked leading edge of the plate begins melting as it moves deeper into the Earth until it is recycled in the upper mantle. Molten rock collects in magma chambers of the overriding plate. The magma, molten rock, is lighter and less dense than the surrounding rock so it is buoyant. The magma feeds the volcanoes that form in subduction zones. Volcanic arcs form A volcanic arc of stratovolcanoes forms on the overriding plate. These volcanoes do not erupt as frequently as shield volcanoes that form over hot spots. The two largest volcanic eruptions of the 20th century were stratovolcanoes in these zones. Two oceanic plate converge If two oceanic plates converge the heavier and denser of the two plates subducts into the upper mantle. The Aleutian Islands in Alaska have formed as the Pacific Plate subducts beneath the North American Plate.


Megathrust earthquakes Great megathrust earthquakes that create tsunamis are associated where subduction of plates take place. As the subducting plate moves beneath the overriding plate they become locked. Pressure builds until the rocks fracture along the fault line. Oceanic fault lines In these zones the fault lines are hundreds of miles long. The 9. 5 Chilean earthquake and the 9. 2 Alaskan earthquake were both subduction megathrust earthquakes. Generally only very large megathrust earthquakes produce tsunamis. Learn more about this long trench which parallels the Aleutian Islands. Learn more about redoubt volcano located on the Cook Inlet of Alaska. Find out how and where volcanic arcs form on the Pacific Ring of Fire. Learn more about the Ring of Fire volcanoes that form in subduction zones. Find out why the Pacific Ring of Fire has so many of these zones. Learn more about the Ring of Fire which is home to towering volcanoes and great earthquakes. The links on our home page include information about volcanoes, science activities, plate tectonics, the rock cycle and much more. Check out Myrna Martin's award winning textbooks, e-books, videos and rock sets. The Ring of Fire Science Bookstore covers a wide range of earth science topics. A subduction zone is the biggest crash scene on Earth. These boundaries mark the collision between two of the planet s tectonic plates. The plates are pieces of crust that slowly move across the planet s surface over millions of years.


Where two meet at a subduction zone, one bends and slides underneath the other, curving down into the mantle. (The mantle is the hotter layer under the crust. ) Tectonic plates can transport both continental crust and oceanic crust, or they may be made of only one kind of crust. Oceanic crust is denser than continental crust. At a subduction zone, the oceanic crust usually sinks into the mantle beneath lighter continental crust. (Sometimes, oceanic crust may grow so old and that dense that it collapses and , scientists think. ) If the same kind of crust collides, such as continent-continent, the plates may crash together without subducting and crumple together like crashing cars. The massive mountain chain was created this way, when India slammed into Asia. Scientists first identified subduction zones in the 1960s, by locating earthquakes in the descending crust. Now, new instruments can precisely track the shifting tectonic plates. We can see very clear pictures of how the plates move, mostly due to GPS data, said Vasily Titov, director of National Oceanic and Atmospheric Administration s Center for Tsunami Research in Seattle, Washington. Subduction zones occur all around the edge of the Pacific Ocean, offshore of Washington, Canada, Alaska, Russia, Japan and Indonesia. Called the Ring of Fire, these subduction zones are responsible for the world s biggest earthquakes, the most terrible tsunamis and some of the worst volcanic eruptions.


Earthquakes Shoving two massive slices of Earth s crust together is like rubbing two pieces of sandpaper against each other. The crust sticks in some places, storing up energy that is released in earthquakes. The massive scale of subduction zones means they can cause enormous earthquakes. The largest earthquakes ever recorded were on subduction zones, such as a magnitude 9. 5 in Chile in 1960 and a magnitude 9. 2 in Alaska in 1964. Subduction zones are huge boundaries, so they generate very large earthquakes, Titov told Live Science. Why are subduction zone earthquakes the biggest in the world? The main reason is size. The size of an earthquake is related to the that causes it, and subduction zone faults are the longest and widest in the world. The Cascadia subduction zone offshore of Washington is about 620 miles (1,000 kilometers) long and about 62 miles (100 km) wide. Smaller earthquakes also strike all along the descending plate, also called a slab. Seismic waves from these temblors and tremors , similar to a medical CT scan. The quakes reveal that the sinking slab tends to bend at an angle between 25 to 45 degrees from Earth s surface, though some are flatter or steeper than this. Sometimes, the slabs may tear, like a gash in wrinkled paper. Pieces of the sinking plate can also break off and fall into the mantle, or get stuck and founder. Credit: USGS. Tsunamis Subduction zones are usually along coastlines, so tsunamis will always be generated close to where people live, Titov said.


There s a silver lining there, he said. If these earthquakes happened underneath a city, the city would have no chance. But the bad news is sometime a tsunami is generated. When subduction zone earthquakes hit, Earth s crust flexes and snaps like a freed spring. For earthquakes larger than a magnitude 7. 5, this can cause a , a giant sea wave, by suddenly moving the seafloor. However, not all subduction zone earthquakes will cause tsunamis. Also, some earthquakes trigger tsunamis by sparking underwater landslides. Whatever their cause, the by government agencies such as NOAA in countries around the Pacific Ocean. Tsunamis may strike in minutes for coastal areas near an earthquake, or hours later, after the waves travel across the sea. Volcanoes As a tectonic plate slides into the mantle, the hotter layer beneath Earth s crust, the heating releases fluids trapped in the plate. These fluids, such as seawater and carbon dioxide, rise into the upper plate and can partially melt the overlying crust, forming magma. And magma (molten rock) often means volcanoes. Looking at the Pacific Ring of Fire reveals the link between subduction zones and volcanoes. Inland of each subduction zone is a chain of spouting volcanoes called a , such as Alaska s Aleutian Islands. The Toba volcanic eruption in Indonesia, the largest volcanic eruption in the past 25 million years, was from a subduction zone volcano. Email or follow her. Follow us,. Additional resources

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