This combined layer is called the lithosphere, which includes the crust and the uppermost solid portion of the mantle. It varies in thickness beneath the oceans and continents, with the oceanic lithosphere being thinner and denser than the continental lithosphere. The lithosphere is divided into large plates that move and interact with each other, causing geological phenomena like earthquakes and volcanic eruptions.
The mantle is composed primarily of silicate minerals rich in magnesium and iron. It is approximately 2,900 kilometers thick and is located between the Earth's crust and the core.
No, the Earth's crust makes up less than 1% of the Earth's mass. The crust is the thin, outermost layer of the Earth, while the majority of the Earth's mass is in the mantle and core.
The mantle is the largest layer in the Earth's interior.
Earth's tectonic plates float on the semi-fluid layer of the mantle called the asthenosphere. These plates move and interact with each other due to the convective currents in the molten mantle beneath them.
The crust is the outermost layer of the Earth, which is thin and solid. It is divided into continental crust (underneath land) and oceanic crust (underneath oceans). In contrast, the mantle is the layer beneath the crust and is primarily composed of solid rock that flows slowly over long periods of time.
The very top of Earth's mantle is known as the lithosphere. It is a rigid layer that consists of both the uppermost part of the mantle and the crust above it. The lithosphere is broken into tectonic plates that float on the semi-fluid asthenosphere beneath it.
The Earth's crust and the uppermost part of the mantle together form the lithosphere. The lithosphere is a rigid outer layer of the Earth that is divided into tectonic plates which float on the semi-fluid asthenosphere beneath them.
The crust and the very top of the mantle make up the lithosphere, which is the outermost layer of the Earth. The lithosphere is divided into several tectonic plates that move and interact with each other at plate boundaries.
the earths mantle is very hot were cornstarch is not hot at all
the earths mantle is very hot were cornstarch is not hot at all
The mantle is composed primarily of silicate minerals rich in magnesium and iron. It is approximately 2,900 kilometers thick and is located between the Earth's crust and the core.
No, the Earth's crust makes up less than 1% of the Earth's mass. The crust is the thin, outermost layer of the Earth, while the majority of the Earth's mass is in the mantle and core.
The continents "float" on the liquid mantle of the Earth because the metals that make up the mantle are very dense. The continents move when magma is pushed through the crust of the Earth in places like the Mid-Atlantic Ridge. The continents "float" on the liquid mantle of the Earth because the metals that make up the mantle are very dense. The continents move when magma is pushed through the crust of the Earth in places like the Mid-Atlantic Ridge.
The mantle is the largest layer in the Earth's interior.
The lithosphere includes the crust and the very top of the mantle. The lithosphere is cool and brittle.
The earths mantle is less dense and it's very hot.
the earths mantle is very hot were cornstarch is not hot at all