the two layers of rock that made up of mantle is the solid rock and liquid rock
crust and mantle
Crust and mantle
The two layers of the Earth that are made of rock are the crust and the mantle. The crust is the outermost layer and is composed of solid rock, while the mantle lies just below the crust and consists of solid rock that is capable of flowing over long periods of time.
The two layers of Earth that are made of rock are the crust and the mantle. The crust is the outermost layer, consisting of solid rock that forms the continents and ocean floors. Beneath the crust, the mantle is composed of semi-solid rock that flows slowly over geological time. Together, these layers play a crucial role in tectonic activity and the Earth's geology.
The crust and the mantle are the two layers of the Earth that are made predominantly of rocks. The crust is the outermost layer and is divided into continental and oceanic crust, while the mantle lies beneath the crust and is composed of solid rock.
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.
Crust and mantle
The two layers beneath the Earth's crust are the mantle and the core. The mantle is a layer of hot, solid rock that extends about 1,800 miles below the crust, while the core is made up of a liquid outer core and a solid inner core composed of iron and nickel.
The other two layers of the Earth are the mantle and the core. The mantle is primarily composed of silicate minerals, while the core is mostly made of iron and nickel.
In the mantle,we have two layers of solid rock with heated flowing rock between them.
The lithosphere is made up of two layers: the crust and the uppermost part of the mantle. The crust is the outermost layer of the lithosphere and is composed of solid rock, while the upper mantle beneath it is also solid but more ductile.
The mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is further divided into the lithosphere and the asthenosphere. The lithosphere is rigid and made up of the crust and the upper part of the mantle, while the asthenosphere is semi-molten and capable of flowing.