The mantle is primarily composed of silicate minerals, which are classified as igneous rocks.

The Mohorovičić discontinuity, or Moho, separates the Earth's crust from the underlying mantle.

The mantle extends from the base of the crust to about 2,900 km deep.

The Mohorovičić discontinuity (Moho) is located at an average depth of about 30 km beneath the Earth's surface.

The temperature at the boundary between the Earth's crust and mantle is approximately 1,000°C.

The temperature at the Earth's inner core is estimated to be around 5000°C to 6000°C.

The temperature of the Earth's mantle ranges from about 1,000 °C to 3,000 °C as you go deeper.

The temperature of the Earth's outer core ranges from approximately 4,000 to 6,000 degrees Celsius.

The Earth's crust varies in thickness, averaging about 30-50 km under continents and about 5-10 km under oceans.

The average density of the Earth is about 5.5 g/cm³, which is higher than the density of the crust.

The temperature at the Earth's inner core is estimated to be around 6000°C.

The Earth's mantle is mainly composed of silicate minerals, which include olivine and pyroxene.

The Earth's crust is primarily composed of oxygen, which combines with silicon to form silicate minerals.

The Earth's crust is primarily composed of basalt (oceanic crust) and granite (continental crust).

The inner core is primarily composed of solid iron, along with some nickel.

The outer core is primarily composed of liquid iron and nickel, which is crucial for generating the Earth's magnetic field.

Seismic waves generated by earthquakes are the primary method used to study the Earth's interior structure.

The Earth's magnetic field is primarily generated by the flow of molten iron in the outer core.

Tectonic plates move primarily due to convection currents in the mantle, which are caused by the heat from the Earth's core.

The outer core is in a liquid state, composed mainly of molten iron and nickel.

The layer directly beneath the Earth's crust is the mantle.

The Outer Core is the only layer of the Earth that is in a liquid state.

The Outer Core is primarily composed of molten iron and nickel, which is responsible for Earth's magnetic field.

The movement of liquid iron in the Outer Core generates the Earth's magnetic field.

The Earth's crust is where tectonic activity occurs, as it is divided into tectonic plates.

The Mantle, particularly the asthenosphere, is responsible for the movement of tectonic plates.

The movement of molten iron in the outer core generates the Earth's magnetic field.

The mantle is responsible for volcanic activity as it contains magma that can rise to the surface through the crust.

The Inner Core is solid and composed mainly of iron and nickel, despite the high temperatures.

The crust is the outermost layer of the Earth and is solid, composed mainly of silicate rocks.