The crust stretches and gets thinner so the pressure decreases on the mantle rocks below this causes part of the mantle 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.
Melted rock in the Earth's mantle is called magma.
When rocks are pushed down into the mantle and melt, they become magma. Magma is molten rock located beneath the Earth's surface.
the entire mantle is solid because the pressure is so great the rock are unable to melt.
At convergent boundaries some mantle material can melt and rise through the crust, forming volcanoes.
The crust stretches and gets thinner so the pressure decreases on the mantle rocks below this causes part of the mantle 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.
Melted rock in the Earth's mantle is called magma.
Asthenosphere
Pressure
When rocks are pushed down into the mantle and melt, they become magma. Magma is molten rock located beneath the Earth's surface.
the entire mantle is solid because the pressure is so great the rock are unable to melt.
The mantle cause the mantle to flow.
Rocks melt in the upper mantle due to high temperatures and pressure from the Earth's interior. The increase in temperature lowers the rocks' melting point, allowing them to transform into magma. This process is known as partial melting.
Pressure and temperature are both important factors in the formation of magma. Increasing temperature can cause rocks to melt, forming magma. Pressure can also influence magma formation by affecting how easily rocks can deform and melt. Generally, higher temperatures and lower pressures favor magma formation.
Places where tectonic plates separate are known as divergent boundaries. At these boundary locations, magma rises from the mantle, forming new crust as the plates move apart.