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the asthenosphere and the lithosphere contain molten material.
a molten rock
They are highly molten, weak, capable of flowing.
Matter in the Asthenosphere is in the molten or semi-molten state. This is because its temperatures can peak at 3,000 degrees Celsius. Its composition consists of magnesium and iron silicates. The Asthenosphere plays a key role in the movement of tectonic plates.
There is no ocean of molten rock underneath the continents. Tectonic plates, both oceanic and continental, move on top of the ductile asthenosphere.
the asthenosphere and the lithosphere contain molten material.
the asthenosphere and the lithosphere contain molten material.
a molten rock
They are highly molten, weak, capable of flowing.
The asthenosphere is composed of very hot, ductile ultramafic rock and is believed to be roughly 5% molten.
a molten rock
The continental plates float on asthenosphere, molten rock (lava).
The continental plates float on asthenosphere, molten rock (lava).
It is the asthenosphere. Because the lithosphere is a part of the crust and mantle. So that makes the asthenosphere underneath it because it is hard rock...
It starts with molten material [magma], when volcanic activity starts the molten material turns into igneous rock.
More felsic than the original chemistry of the rock that was partially melted
Matter in the Asthenosphere is in the molten or semi-molten state. This is because its temperatures can peak at 3,000 degrees Celsius. Its composition consists of magnesium and iron silicates. The Asthenosphere plays a key role in the movement of tectonic plates.