Solid rock can flow under extreme conditions of temperature and pressure, typically occurring deep within the Earth's crust. When subjected to high temperatures, rock can behave like a viscous fluid over geological timescales, allowing it to deform and flow. This process is facilitated by mechanisms such as ductile deformation, where minerals in the rock rearrange themselves without breaking, often occurring in tectonic settings like subduction zones or during the formation of mountain ranges. Additionally, the presence of fluids can enhance this flow by reducing friction and facilitating the movement of rock.
In the mantle
The solid rock in the asthenosphere has the ability to flow like honey because of the high temperatures and pressures in this region. This combination causes the rock to deform and flow plastically over long timescales, similar to how honey can flow slowly under the right conditions.
Yes, the solid rock of the asthenosphere can flow over long periods of time under high heat and pressure conditions, behaving in a plastic-like manner. This flow allows for the movements of tectonic plates that shape the Earth's surface.
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.
Yes. A rock has a definite shape and volume, and does not flow.
yes because it is a solid that can move
Solid rock cannot flow because its particles are locked into a fixed position due to strong intermolecular forces. However, hot liquid rock can flow because its particles have enough energy to move past each other and change position, allowing it to flow like a fluid.
plasticity
In the mantle
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
Impermeable. The pores in solid rock are too small for water to flow through.
The solid rock in the asthenosphere has the ability to flow like honey because of the high temperatures and pressures in this region. This combination causes the rock to deform and flow plastically over long timescales, similar to how honey can flow slowly under the right conditions.
The mantle cause the mantle to flow.
Yes, the solid rock of the asthenosphere can flow over long periods of time under high heat and pressure conditions, behaving in a plastic-like manner. This flow allows for the movements of tectonic plates that shape the Earth's surface.
Solid rock does not flow because its atoms and molecules are densely packed in a fixed position, preventing them from moving past one another. This rigid structure gives rock its solid and stable form, making it resistant to flowing like a liquid. Additionally, the high pressure and temperature required to deform rock into a flowing state are typically not present in nature at the Earth's surface.
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.
Water cannot pass through a solid rock because the rock's structure is tight and does not have spaces for the water to flow through. The pores in the rock are too small for water molecules to move through.