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less dense than the solid material around it
No. Magma varies in density, but it will be less dense than a solid rock of the same composition.
Because magma is less dense than the surrounding solid rock, it is forced upward toward the surface. When magma reaches the surface and flows from volcanoes, it is called lava.
When it is heated it becomes less dense (i.e. lighter). The more dense (i.e. heavier) magma sinks while the less dense magma rises to the top. It will eventually cool again causing a convection current within the mantle.
Cooler material is more dense and hotter material is less. This means that plates become more dense as they cool.
Liquid magma is more dense than the solid material around it.
Magma?
less dense than the solid material around it
yes
No. Magma varies in density, but it will be less dense than a solid rock of the same composition.
yes
The magma originates from the melting, subducting oceanic crust. The more dense of the oceanic crusts is forced below the less dense oceanic crust, and the presence of water makes it melt in the high temperature environment of the upper mantle. As the molten material is less dense than the surrounding material, it will attempt to rise toward the surface which may result in volcanism.
Because magma is less dense than the surrounding solid rock, it is forced upward toward the surface. When magma reaches the surface and flows from volcanoes, it is called lava.
When it is heated it becomes less dense (i.e. lighter). The more dense (i.e. heavier) magma sinks while the less dense magma rises to the top. It will eventually cool again causing a convection current within the mantle.
Magma is less dense than the surrounding rock; as such, it will rise toward the surface.
Cooler material is more dense and hotter material is less. This means that plates become more dense as they cool.
Magma is less dense than rock and is buoyant due to this density difference. It will seek out any weaknesses in the rock above it to reach the surface.