Just below the crust we find the mantle.
The asthenosphere is found beneath the lithosphere, which is the outermost layer of Earth. It is part of the upper mantle and is located at depths between 80 to 200 km below the Earth's surface. The asthenosphere is semi-molten and plastic in nature, allowing the lithospheric plates above it to move and interact.
Scientists know that continental crust is less dense than the layer below it due to seismic data collected from earthquakes. Seismic waves travel faster through denser materials, so the variation in wave velocities within the Earth's layers helps scientists determine their relative densities. Additionally, studies of rock samples from both the continental crust and the layer below it have confirmed this density difference.
The zone between the core and crust of the Earth is the mantle. It is a layer of solid rock that extends about 1,800 miles (2,900 kilometers) below the Earth's surface. The mantle is made up of silicate minerals and is responsible for convection currents that drive plate tectonics.
The continental crust is typically 20 to 30 miles thick. It is the outermost layer of the Earth's surface that forms the continents we live on.
The atmosphere, therefore, consists of gases that envelop the Earth. The lithosphere refers to the rocks of the Earth’s surface and upper mantle, or the depth of the plates. As you go higher in the atmosphere, the mixture of the gases changes.
the layer inside the earth that is right above the astroshpere and right below the crust
The crust of the earth is located right at the top which a thick layer
The mantle is a layer of rock below the Earth's crust that moves due to convection currents caused by heat from the core. The core is the Earth's innermost layer made of iron and nickel. The mantle interacts with the crust through tectonic plate movements that can cause earthquakes, volcanic eruptions, and the formation of mountain ranges.
The asthenosphere is found beneath the lithosphere, which is the outermost layer of Earth. It is part of the upper mantle and is located at depths between 80 to 200 km below the Earth's surface. The asthenosphere is semi-molten and plastic in nature, allowing the lithospheric plates above it to move and interact.
Groundwater.
The mantle is that part of the Earth between the crust and the outer core. It's upper boundary is at the base of the crust at a depth below the surface which can vary between 7 and 35 km. It extends all the way to the Earth's outer core at a depth of around 2890 km.the Earths mantle is located between the crust and outer core of the Earth. it is the thickest layer.
I'm studying the earths layers and it's right after the lithosphere which is right underneath the crust I'm studying the earths layers and it's right after the lithosphere which is right underneath the crust I'm studying the earths layers and it's right after the lithosphere which is right underneath the crust
Scientists know that continental crust is less dense than the layer below it due to seismic data collected from earthquakes. Seismic waves travel faster through denser materials, so the variation in wave velocities within the Earth's layers helps scientists determine their relative densities. Additionally, studies of rock samples from both the continental crust and the layer below it have confirmed this density difference.
Its the very upper layer of the Earth's atmosphere right below the exosphere which is essentially space.
The mantle is the source of molten rock. This molten material can, if the tectonics are right, penetrate up through the solid outer mantle and the crust to deliver lava, which is molten rock (magma) that has reached the surface of the earth.
The zone between the core and crust of the Earth is the mantle. It is a layer of solid rock that extends about 1,800 miles (2,900 kilometers) below the Earth's surface. The mantle is made up of silicate minerals and is responsible for convection currents that drive plate tectonics.
Sounds right to me. Also remember that the earth's crust is thicker under the continents (land) than under the ocean where it becomes thinner.