Layers of the Earth

Layers of the Earth
The four main layers of the Earth are the crust, mantle, outer core, and inner core.

The Earth, like an onion, consists of several concentric layers, each with its own unique set of properties and characteristics. The four primary layers are the crust, the mantle, the outer core, and the inner core. However, geologists subdivide these layers into a complex structure that better describes the Earth’s intricate composition and behavior. Let’s start with the basic four-layer model before delving into greater detail.

The 4 Basic Layers of the Earth

The Crust

The crust is the Earth’s outermost layer and it’s where we live. It has an irregular thickness, varying from about 5 km beneath the oceans (oceanic crust) to about 30 km beneath the continents (continental crust). The crust mainly consists of lighter rocks, such as basalt in the oceanic crust and granite in the continental crust.

The Mohorovičić discontinuity, often referred to as the Moho, is the boundary between the Earth’s crust and the mantle. Named after the Croatian seismologist Andrija Mohorovičić who discovered it in 1909, the Moho occurs from 5 to 10 kilometers beneath the ocean floor to about 20 to 70 kilometers beneath continental interiors.

The significance of the Moho discontinuity lies in the change in seismic wave velocities that it represents. Seismic waves from earthquakes travel at different speeds depending on the material they move through. Mohorovičić noted that seismic waves speed up abruptly below certain depths. This observation led him to conclude that Earth has a layered structure. The Moho represents the transition from the relatively low-density crust to the higher-density mantle.

The Mantle

Beneath the crust lies the mantle, extending to a depth of about 2,900 km. It contains silicate rocks that are rich in iron and magnesium. There are two sections of the mantle: the upper mantle, which is more rigid and behaves elastically on short time scales, and the lower mantle, which is solid but flows on geological timescales.

The Outer Core

The outer core extends from 2,900 km to about 5,150 km beneath the Earth’s surface. It mainly consists of liquid iron and nickel. The motion within this layer generates the Earth’s magnetic field.

The Inner Core

The inner core is the central part of the Earth. It extends from a depth of about 5,150 km to the Earth’s center at about 6,371 km. Although it is very hot, the inner core is solid due to the immense pressure at this depth. It’s composed primarily of iron, with minor amounts of nickel and other lighter elements.

Detailed Layer Model of the Earth

For a more intricate understanding of the Earth’s structure, geologists divide the layers of the Earth a bit differently, based on their physical and chemical properties.

1. The Lithosphere

The lithosphere, about 10 to 200 km thick, includes the uppermost mantle and the crust. It’s rigid and breaks under stress, which is why it’s broken up into tectonic plates. The lithosphere varies in thickness, being thinner at oceanic ridges and thicker beneath older oceanic and continental regions.

2. The Asthenosphere

Beneath the lithosphere, from about 100 to 350 km, lies the asthenosphere. The asthenosphere is the part of the upper mantle that exhibits plastic (or ductile) behavior. The tectonic plates slide around on top of this layer. It’s composed of similar material to the rest of the upper mantle – mainly peridotite, a rock rich in silicate minerals.

3. The Mesosphere

Below the asthenosphere and extending to about 2,900 km is the mesosphere or lower mantle. The mesosphere is a region of strong, rigid rocks that deform slowly under the intense heat and pressure. It’s composed of silicate minerals that change in structure with depth due to increasing pressure.

4. The Outer Core

The outer core spans from 2,900 to about 5,150 km deep. The convection currents within this liquid layer create the Earth’s magnetosphere through a dynamo effect.

5. The Inner Core

The inner core extends from 5,150 km to the center of the Earth at about 6,371 km. In recent years, it has been suggested that the inner core itself may have an inner-inner core with distinct physical properties, but this remains an area of active research.

Physical Properties of the Earth’s Layers

Each of these layers has unique physical properties, including temperature, pressure, density, and composition. The crust and uppermost mantle (lithosphere) are cool and rigid, while the asthenosphere is partially molten and plastic. Deeper in the Earth, temperatures and pressures rise dramatically. The core, for example, has temperatures similar to the Sun’s surface and pressures more than 3 million times atmospheric pressure.

The Earth’s density also increases with depth, from around 2.2 g/cm³ in the crust to over 13 g/cm³ in the core. This density gradient is due to both increasing pressure and changes in composition.

In terms of composition, the crust is mostly silicate rocks and oxygen, while the core is largely iron and nickel. The mantle, which comprises the majority of Earth’s volume, is predominantly composed of silicate minerals rich in iron and magnesium.

10 Facts About the Layers of the Earth

Now, let’s explore ten interesting facts about the layers of the Earth:

  1. Thickest Layer: The mantle is the thickest layer of the Earth, accounting for about 84% of the Earth’s volume. It extends approximately 2,900 kilometers beneath the crust, which makes it nearly twice the thickness of the Earth’s outer and inner cores combined.
  2. Pressure: The pressure of the inner core at the Earth’s center is extreme. Estimates place it at over 3.5 million times greater than the pressure at sea level.
  3. Temperature: The temperature of the core is similar to that of the Sun’s surface, around 5,500 degrees Celsius.
  4. Dynamo Effect: The Earth’s magnetic field results from the convection of liquid iron and nickel in the outer core, a phenomenon known as the dynamo effect.
  5. Oceanic vs. Continental Crust: Oceanic crust is thinner and denser than continental crust. The average thickness of oceanic crust is 5 km, while continental crust averages around 35 km.
  6. Crust Composition: The crust is primarily composed of silicate rocks. The oceanic crust is mainly basalt, and the continental crust is primarily granite.
  7. Tectonic Plates: The Earth’s lithosphere is broken into variously sized “tectonic plates.” It’s the movement of these plates that causes earthquakes, volcanic activity, and the creation of mountain ranges.
  8. Asthenosphere Behavior: Despite being solid, the asthenosphere flows over geologic time scales, which assists the movement of the tectonic plates of the lithosphere.
  9. Core Composition: The core is primarily composed of iron, with smaller amounts of nickel and other lighter elements. It’s also believed that there might be “oceans” of liquid iron in the core.
  10. Inner Core Anomaly: Recent studies suggest that the inner core itself may have an “inner inner core” with distinctive physical properties, although this is still a topic of ongoing research.

Layers of the Earth Worksheet


  • Engdahl, E.R.; Flinn, E.A.; Massé, R.P. (1974). “Differential PKiKP travel times and the radius of the inner core”. Geophysical Journal International. 39 (3): 457–463. doi:10.1111/j.1365-246x.1974.tb05467.x
  • Harris, P. (1972). “The Composition of the Earth“. In Gass, I. G.; et al. (eds.). Understanding the Earth: A Reader in the Earth Sciences. Horsham: Artemis Press for the Open University Press. ISBN 978-0-85141-308-2.
  • Haynes, William M.; David R., Lide; Bruno, Thomas J., eds. (2017). CRC Handbook of Chemistry and Physics (97th ed.). Boca Raton, Florida: CRC Press. ISBN 978-1-4987-5429-3.
  • O’Reilly, Suzanne Y.; Griffin, W.L. (December 2013). “Moho vs crust–mantle boundary: Evolution of an idea”. Tectonophysics. 609: 535–546. doi:10.1016/j.tecto.2012.12.031
  • Rogers, N., ed. (2008). An Introduction to Our Dynamic Planet. Cambridge University Press and The Open University. ISBN 978-0-521-49424-3.