As the oceanic plate descends below 700 km into the mantle, it undergoes increasing temperatures and pressures, which can cause dehydration and partial melting of the subducted material. This process leads to the release of fluids that can trigger volcanic activity in the overlying mantle. The plate continues to sink deeper, eventually becoming part of the mantle's convective flow, where it may contribute to mantle dynamics and the formation of new geological features. Over time, the plate may eventually be assimilated into the mantle, altering its composition and properties.
When ocean crust and mantle are subducted, the oceanic crust descends into the mantle, where it eventually reaches a depth where it melts due to the high temperatures and pressures. This molten material can rise back to the surface through volcanic activity, forming island arcs or volcanic mountain ranges. The subducting crust can also undergo partial melting, which can alter the composition of the mantle wedge above the subduction zone.
The Earth some times oceanic crust is formed by the process of mid oceanic ridges. this process occurs when magma comes from the mantle and cool below oceanic body & form new crust.
At mid-ocean ridges, such as the Atlantic Rise and Pacific Rise. As two plates move apart the crust is stretched and thinned, causing less pressure on the mantle immediately below. Due to this drop in pressure the mantle undergoes "decompressional melting" allowing magma to form. This magma is less dense than the surrounding mantle and rises at the mid-ocean ridges, cooling and forming new oceanic crust.
When a continental plate collides with an oceanic plate, the denser oceanic plate will be subducted beneath the less dense continental plate due to the difference in density. This process can result in the formation of deep ocean trenches, volcanic arcs, and mountain ranges. Additionally, earthquakes and tsunamis can occur as a result of the intense tectonic activity in these zones.
The mantle is below the plates.
When ocean crust and mantle are subducted, the oceanic crust descends into the mantle, where it eventually reaches a depth where it melts due to the high temperatures and pressures. This molten material can rise back to the surface through volcanic activity, forming island arcs or volcanic mountain ranges. The subducting crust can also undergo partial melting, which can alter the composition of the mantle wedge above the subduction zone.
The Earth some times oceanic crust is formed by the process of mid oceanic ridges. this process occurs when magma comes from the mantle and cool below oceanic body & form new crust.
The Earth some times oceanic crust is formed by the process of mid oceanic ridges. this process occurs when magma comes from the mantle and cool below oceanic body & form new crust.
Oceanic plates sink because they are denser than the underlying mantle, due to cooling and becoming more compact over time. In contrast, other plates float because they are less dense than the mantle material below, allowing them to remain buoyant on top.
when oceanic crust and continental crust collide, the oceanic crust sinks down beneath the continental crust. this is called subduction.
At mid-ocean ridges, such as the Atlantic Rise and Pacific Rise. As two plates move apart the crust is stretched and thinned, causing less pressure on the mantle immediately below. Due to this drop in pressure the mantle undergoes "decompressional melting" allowing magma to form. This magma is less dense than the surrounding mantle and rises at the mid-ocean ridges, cooling and forming new oceanic crust.
The Earth's mantle is below the crust. The layers of the Earth form concentric spheres. Below the mantle is the core.
Typically the less dense continental plate would stay afloat while the denser oceanic plate would be submerged below. This can result in volcanic eruptions at the subduction zone due to oceanic crust undergoing increased pressure and temperatures as it descends below the continental crust.
is the temperature if the stiffer mantle above or below its melting point
Yes, when older, colder oceanic plates sink below younger, warmer plates in a process called subduction, the density of the older plate increases as it is subjected to higher pressures and temperatures in the Earth's mantle. This increase in density allows the plate to sink into the mantle.
Mantle Is The Below Layer Of The Crust In Earth.
The part of the mantle below the lithosphere is called the Asthenosphere.