Apparently rigid rock can indeed flow, given enough time. And with the appropriate applied forces of course.
In the south island of New Zealand where I live, the land has shrunk in an E - W direction by about 150cm over a length of about 200 km, in the 150 years of survey history. That is about 5mm per year per 100km. This is all plastic flow, and is building the local mountains higher.
If you look at a sedimentary sequence, you'll often see folds in the rock.
Hard crystalline rocks such as granite do not deform as easily. Sandstone and mud-stone are more easily deformed.
A solid is a state of matter that does not have the ability to flow. It has a definite shape and volume, with its particles arranged in a fixed pattern.
Matter can exist in various states, including solid, liquid, and gas, which can determine its ability to flow. For example, liquids and gases have the ability to flow, while solids generally do not flow in the same manner. The ability of a substance to flow is influenced by factors such as temperature, pressure, and molecular structure.
The state of matter that has the ability to flow is the liquid state. In liquids, particles are close together but not rigidly fixed in place, allowing them to move past each other and flow.
Solid rock has the ability to flow over long periods of time under high temperatures and pressures, a process known as rock deformation or creep. This flow occurs on a microscopic scale due to the movement of mineral grains within the rock. The resulting deformation can lead to the folding, faulting, and other structural changes in the Earth's crust.
Viscosity is a term used to describe a fluid's ability to resist flow. Fluids with high viscosity flow more slowly, while fluids with low viscosity flow more easily.
yes because it is a solid that can move
plasticity
A solid is a state of matter that does not have the ability to flow. It has a definite shape and volume, with its particles arranged in a fixed pattern.
A solid compound will not have the properties of fluidity (ability to flow) and compressibility (ability to significantly decrease in volume under pressure).
Matter can exist in various states, including solid, liquid, and gas, which can determine its ability to flow. For example, liquids and gases have the ability to flow, while solids generally do not flow in the same manner. The ability of a substance to flow is influenced by factors such as temperature, pressure, and molecular structure.
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.
liquid and gas because they both have an ability to flow
The Earth's mantle is solid but has the ability to flow over long periods of time due to high temperature and pressure. This slow flowing movement is known as mantle convection and is responsible for the movement of tectonic plates.
A solid is a substance that cannot be compressed because its particles are closely packed together in a fixed arrangement. Solid substances also cannot flow, as their particles do not have the ability to move past each other easily.
The property of particles in a solid that sand or sugar grains do not show is the ability to flow and conform to the shape of their container. Sand and sugar grains have a fixed shape and volume, whereas particles in some solids have the ability to flow and change shape.
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.
The lithosphere is solid rock composed of the Earth's crust and uppermost portion of the mantle. While it is mostly solid, under certain conditions and over long periods of time, it can exhibit some degree of flow or deformation due to tectonic forces. This slow movement is known as lithospheric flow or creep.