The mantle is a semi-solid layer made up of hot, flowing rock known as magma that circulates slowly over geologic time scales. While it appears solid, the mantle can still flow and deform over long periods due to high temperatures and pressures. This behavior gives it a paste-like consistency rather than a runny liquid.
The inner mantle is approximately 2,900 kilometers thick. It is composed of solid rock that behaves like a very thick paste over long periods of time.
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 is approximately 2,900 kilometers thick. It is composed of solid rock that behaves like a very thick paste over long periods of time.
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.
None! Unless you mean the core. The outer core is liquid.
Marmite is a thick, sticky paste with a consistency similar to peanut butter. It is not a 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.
how the thin outer crust is floating on the thick liquid mantle, causing the crust to move and form a divergent plate boundary