The more dense plate subducts (goes under) the less dense plate.
For example if continental and oceanic crust collide oceanic crust will go underneath the continental.
When two tectonic plates collide, the outcome of which plate comes out on top largely depends on their relative densities and compositions. Generally, the denser oceanic plate tends to subduct beneath the lighter continental plate, leading to the formation of features like ocean trenches and volcanic arcs. In cases where two continental plates collide, neither plate subducts easily, and instead, they can crumple and fold, leading to the creation of mountain ranges. Ultimately, the specific geological circumstances and material properties of the plates involved will dictate the result of the collision.
Mountains form where continental and oceanic plates collide by the actions of the plates upon one another. Often one plate pushes up and over the other one, and the upper one creates a row of mountains.
When two plates collide, a thrust fault forms. This type of fault occurs when one tectonic plate is forced over the top of another plate, causing the rocks to break and slide in a horizontal direction. Thrust faults are common in regions where compression is predominant, such as at convergent plate boundaries.
This process typically occurs at subduction zones where two tectonic plates converge, with one plate being forced beneath the other into the Earth's mantle. This can result in the formation of volcanic arcs and deep ocean trenches.
The tectonic plates are sitting on molten lava. Due to convection currents the plates are moved around and can crash into each other causing earthquakes. Convection currents occur because of the core. The core of the earth is really hot. Therefore, it heats the molten rock near it and this rises. As it gets to the top it cools down and therefore sinks. This creates a circular current.
The density of the plates and the angle of the collision can determine which plate comes out on top when two plates collide. The denser plate tends to sink beneath the less dense plate, while the angle of collision can influence the direction of movement. Additionally, the presence of features like oceanic crust and continental crust can also impact which plate is subducted.
Subduction.
The subduction zone.
how much are top plates
Mountains form where continental and oceanic plates collide by the actions of the plates upon one another. Often one plate pushes up and over the other one, and the upper one creates a row of mountains.
When two plates collide, a thrust fault forms. This type of fault occurs when one tectonic plate is forced over the top of another plate, causing the rocks to break and slide in a horizontal direction. Thrust faults are common in regions where compression is predominant, such as at convergent plate boundaries.
No, earthquakes happen as the result of Earth's tectonic plates moving. Tectonic plates are what make up the lithosphere, the top layer of the crust. When the plates move, they either rub against each other, called "shearing", collide with each other, "compression", or they move away from each other, "tension". As the plates move, the rumbling earthquake occurs.
the plates float on top of the upper mantle
This process typically occurs at subduction zones where two tectonic plates converge, with one plate being forced beneath the other into the Earth's mantle. This can result in the formation of volcanic arcs and deep ocean trenches.
When the tectonic plates push up that's when a volcano erupts and the lava comes out. The volcano changes because the top of it will have to repair itself.
No the tectonic plates are on top of the crust.
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