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it goes south it goes south
Convective Current
convention current
Heat. See Fourier's Law.
Magma
This material is most often referred to as magma.
Cooler material (magma) shrinks and becomes more dense. Gravity acts on this denser material more strongly because of its greater unit mass (density = Mass/volume). Lighter material rises as the heavier material displaces it below. This produces a the apparent bouyant force.
Pyroclastic material can form with magma of any composition, but it is more likely to form with high-viscosity magma.
Magma is molten material that when cooled forms a solid called igneous rock
It allows for the cycling of magma that is cooler than the rest to sink further down under where it's warmer and the warmer magma to rise up further because it is less dense and get cooler where the cooler magma used to be.
Magma comes from the melting of material in the crust or upper mantle.
Magma
No. Magma is molten rock inside the earth. Soil can contain material from magma. Magma can solidify inside earth or erupt from volcano. The material can then weather away and become a component of soil.
Convection currents in the earth originate in the mantle. The liquid moves in a circle pattern as the hotter magma rises and the cooler magma falls. This can also be observed in any fluid material, gases or liquids.
No. Magma is molten rock that has not erupted. After it erupts it may or may not form pyroclastic material depending on how explosive the eruption is.
This material is most often referred to as magma.
Cooler material (magma) shrinks and becomes more dense. Gravity acts on this denser material more strongly because of its greater unit mass (density = Mass/volume). Lighter material rises as the heavier material displaces it below. This produces a the apparent bouyant force.
Lava and Magma
Magma
magma
Lava and Magma