cause it will keep going until the lava stop erupting will make the mantle stop
the rock that can flow like a liquid is a mantle because the mantle has two parts. The upper part is the solid rock. The solid rock of the mantle is part is the lithosphere. Below the solid rock, the mantle rock has the ability to flow like a liquid. Most of the mantle is made up of rock that can flow. Sanjida Ahmed 752/753
The mantle consists of two main layers: the upper mantle and the lower mantle. The upper mantle is composed of solid rock that can flow slowly over time. The lower mantle is composed of solid rock under high pressure and temperature conditions.
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 factors that contribute to making rock more rigid in the mantle include high pressure, low temperature, and the composition of the rock itself. These conditions cause the rock to be less able to flow or deform easily, resulting in increased rigidity.
The asthenosphere has plasticity due to the high temperature and pressure conditions present in this region of the Earth's mantle. These conditions allow the rock in the asthenosphere to deform and flow slowly over long periods of time, giving it its plastic behavior.
cause it will keep going until the lava stop erupting will make the mantle stop
cause it will keep going until the lava stop erupting will make the mantle stop
the rock that can flow like a liquid is a mantle because the mantle has two parts. The upper part is the solid rock. The solid rock of the mantle is part is the lithosphere. Below the solid rock, the mantle rock has the ability to flow like a liquid. Most of the mantle is made up of rock that can flow. Sanjida Ahmed 752/753
The mantle consists of two main layers: the upper mantle and the lower mantle. The upper mantle is composed of solid rock that can flow slowly over time. The lower mantle is composed of solid rock under high pressure and temperature conditions.
The mantle cause the mantle to flow.
In the mantle
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 flow of hot rock in earths mantle will stop and Earth's magnetic field will disappear
The factors that contribute to making rock more rigid in the mantle include high pressure, low temperature, and the composition of the rock itself. These conditions cause the rock to be less able to flow or deform easily, resulting in increased rigidity.
The asthenosphere has plasticity due to the high temperature and pressure conditions present in this region of the Earth's mantle. These conditions allow the rock in the asthenosphere to deform and flow slowly over long periods of time, giving it its plastic behavior.
If the Earth's core cools down, the heat flow from the core to the mantle will reduce. This could lead to a decrease in mantle convection and potentially slow down the movement of hot rock in the mantle. This may have implications for processes like plate tectonics and volcanic activity.
Yes, the mantle is made of solid rock that can flow due to its high temperature and pressure. This slow flowing movement of the mantle is known as mantle convection and is responsible for driving plate tectonics.