The crust and the upper part of the mantle are the solid part of the Earth called the lithosphere.
The lower mantle is a solid layer that extends from about 660 to 2,900 kilometers below the Earth's surface. While it can flow very slowly over geological time scales, it behaves more like a solid due to high pressure and temperature conditions.
Scientists believe Earth's inner core is solid because of seismic waves from earthquakes that travel through the core, the behavior of seismic waves, and the way in which they are reflected or refracted. This information suggests that the inner core behaves more like a solid than a liquid. Additionally, studies of the Earth's magnetic field and the behavior of seismic shear waves also support the idea of a solid inner core.
The Earth's mantle is primarily solid but behaves like a viscous fluid over geological time scales. It consists of solid rock that can flow slowly due to high temperatures and pressures. This semi-solid state allows for convection currents, which drive plate tectonics. Therefore, while it is not liquid in the conventional sense, its properties allow it to move and deform like a fluid.
: Separation of a solid accompanied by little or no macroscopic plastic deformation. Typically, brittle fracture occurs by rapid crack propagation with less expenditure of energy than for ductile fracture. :
The lithosphere, which includes the rigid outermost layer of the Earth's mantle, is responsible for the movement and formation of tectonic plates. These plates float on the semi-fluid asthenosphere below and interact with each other at plate boundaries, leading to processes like subduction and spreading.
No. It behaves as a solid.
an amorphasolid
No, the Earth's inner core is solid due to high pressure despite its high temperatures. The outer core, which is liquid, is responsible for generating Earth's magnetic field through convection currents.
Solid cannot shape of a container but if you look at something like sand it is still a solid though it behaves like a liquid.
The mantle is a semi-solid layer of Earth located below the crust and above the core. It behaves like a solid over short time scales but can flow like a slow, viscous fluid over long time scales, causing tectonic plate movement.
Yes, xenon is a gas at room temperature and pressure, so it does not have a definitive brittle or ductile property like solid materials.
The earth's magnetic properties are due to its molten iron core.
The lower mantle is a solid layer that extends from about 660 to 2,900 kilometers below the Earth's surface. While it can flow very slowly over geological time scales, it behaves more like a solid due to high pressure and temperature conditions.
The asthenosphere is a semi-fluid layer within the Earth's mantle. It behaves more like a solid over short time scales, but can flow slowly over long periods of time due to high temperatures and pressure.
The wood is solid but the lead can be crushed into finite pieces. the lead is still solid eventhough it behaves like a liquid as the atom of the crushed lead is aranged like a solid.
Fluorine is a gas at room temperature and does not exhibit typical solid state properties like brittleness. As a gas, fluorine is not arranged in a lattice structure like solid materials, so it does not have the same mechanical properties that would make it brittle.
The asthenosphere can deform in a ductile manner (i.e. it behaves like a very viscous fluid - imagine very, very, very thick treacle) unlike the overlying lithosphere which behaves as a brittle material and so fractures into separate fragments known as plates.