Because it is compressed down but not hard enough for it to be solid. As well as if it were a runny liquid when the plated moved the world would be doomed.
the inner mantle of the earth is aproximatly 2850km thick.
The outer core of the mantle can be liquid.
The mantle is not a thick paste; it is a layer of the Earth below the crust and above the core. Its consistency is similar to a solid due to high pressure and temperature, but it can flow slowly over longer periods of time, which contributes to plate tectonics and volcanic activity.
The asthenosphere, located in the upper part of the mantle, can flow like a thick liquid due to high temperatures and pressures that allow for the movement of rock over long periods of time.
The Earth's outer core is thicker than the mantle. The outer core is about 2,260 kilometers thick, while the mantle is approximately 2,900 kilometers thick.
Viscous means how thick a LIQUID is and how tightly the particles are packed together if the liquid is thick(less runny) it is more viscous if the liquid is thin(more runny) it is less viscous
the inner mantle of the earth is aproximatly 2850km thick.
you can measure it by dropping a lead ball into the liquid while timing it with a stop watch if it is runny then it is more viscous and when it is thick and not runny it is less viscous.
The mantle
The outer core of the mantle can be liquid.
The answer is the outer core.
The mantle consists of molten rock. Therefore, it made up of a very thick, hot liquid referred to as magma.
It is Mantle or you can say Magma.
Marmite is a thick, sticky paste with a consistency similar to peanut butter. It is not a liquid.
None! Unless you mean the core. The outer core is liquid.
The mantle is not a thick paste; it is a layer of the Earth below the crust and above the core. Its consistency is similar to a solid due to high pressure and temperature, but it can flow slowly over longer periods of time, which contributes to plate tectonics and volcanic activity.
The asthenosphere, located in the upper part of the mantle, can flow like a thick liquid due to high temperatures and pressures that allow for the movement of rock over long periods of time.