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The mantle melts at divergent margins due to decompression melting. As tectonic plates move apart, the pressure on the mantle decreases, causing it to melt and rise to the surface, leading to the formation of new oceanic crust. This process is known as seafloor spreading.

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What causes the rock in the mantle at divergent boundaries to melt?

The crust stretches and gets thinner so the pressure decreases on the mantle rocks below this causes part of the mantle to melt


What causes the rocks in the mantle at divergent boundaries to melt?

Rocks in the mantle at divergent boundaries melt due to the decrease in pressure as tectonic plates move apart. This reduction in pressure lowers the melting point of the rocks, causing them to melt and form magma.


What causes magma to form a divergent plate boundary?

At a divergent plate boundary the crust is thin. This reduces pressure on the upper mantle, lowering the melting point and allowing some rock to melt.


What is a next name for divergent plate margins?

Divergent plate margins are also commonly referred to as "constructive plate boundaries." This term highlights the process by which new crust is formed as tectonic plates move apart, allowing magma from the mantle to rise and solidify. This process is typically associated with mid-ocean ridges and rift valleys.


How does magma form ay divergent boundaries?

Hot mantle rock rises to fill rift zones. When rock rises, a decrease in pressure causes hot mantle rock to melt and form magma.


Is melting of the mantle achieved by decreasing pressure at divergent plate boundaries?

Melting of the mantle at divergent plate boundaries is primarily caused by the decrease in pressure as the tectonic plates move apart. This reduction in pressure lowers the melting point of the mantle rock, allowing it to melt and form magma that can rise to the surface and create new crust. Magmatic activity at divergent boundaries is a key driver of seafloor spreading and plate tectonics.


Why are most volcanoes located near a fault?

Most volcanoes form at either convergent or divergent plate boundaries. Volcanoes at convergent plate boundaries form when one plate slides under another, taking seawater with it. This causes the rock in the mantle to melt as the melting point drops. This new magma can rise to form volcanoes.At divergent plate boundaries the crust is thing, which lowers pressure on the mantle, causing some material to melt.


Why do you find volcanoes at convergent and divergent boundaries but not at transform boundaries?

Convergent and divergent boundaries melt rock in the upper mantle while transform boundaries do not. Convergent boundaries that involve at least one oceanic plate form subduction zones, where an oceanic plate plunges into the mantle. Volatiles carried into the mantle lower the melting point of the rock there, allowing magma to form.At divergent boundaries the crust becomes thinner. This reduces pressure on the upper mantle, thus lowering melting points and generating magma.Transform boundaries have no such means of producing magma.


What causes magma to form at a divergant plate?

At a divergent plate boundary the crust is thin. This reduces pressure on the upper mantle, lowering the melting point and allowing some rock to melt.


How does magma form at convergent and divergent boundaries?

At divergent boundaries, two plates move apart from each other and the space that this creates is filled with new crustal material sourced from molten magma that forms below.


Mafic magma is generated at divergent boundaries because of?

Mafic magma is generated at divergent boundaries because of decompression melting caused by the upwelling of hot mantle material due to the pulling apart of tectonic plates. As the plates move away from each other, the decrease in pressure enables the mantle material to melt and form mafic magma.


Is the main mechanism for melting decompression melting of ultramafic mantle rock?

Yes, the main mechanism for melting in decompression melting involves ultramafic mantle rock. As tectonic plates move apart, the pressure on the mantle rock decreases, allowing it to melt at higher temperatures. This process is primarily responsible for the generation of magma at mid-ocean ridges and other divergent boundaries. The resulting melt is typically basaltic in composition, originating from the ultramafic materials found in the upper mantle.