How Much Does The Earths Crust Weigh?

The Earth's crust weighs approximately 2.6 x 10^22 kilograms (about 2.9 x 10^22 US tons).

Updated June 2026

How Much Does The Earths Crust Weigh?

The short answer: Earth's crust weighs about 2.6 × 10²² kilograms (roughly 2.9 × 10¹⁹ US tons), which is less than 1% of the planet's total mass.

Earth's crust weight by type

The crust is the thin, rocky outer shell we live on, ranging from a few kilometers thick under oceans to tens of kilometers under continents. Its mass is estimated from its volume and the density of crustal rock.

Crust type (example)Typical thickness / density
Oceanic crustabout 5–10 km, ~3,000 kg/m³
Continental crustabout 30–70 km, ~2,700 kg/m³
Combined crust massroughly 2.6 × 10²² kg
Share of Earth's massless than 1%

What affects earth's crust weight

  • Thickness. Continental crust is far thicker than oceanic crust, adding most of the total mass.
  • Rock density. Denser basaltic ocean floor weighs more per cubic meter than lighter granite.
  • Surface coverage. Oceans cover most of Earth, so thin oceanic crust spans a huge area.
  • Boundary definition. Where the crust ends and the mantle begins affects the volume counted.
  • Composition. Lighter silicate minerals make the crust the least dense of Earth's layers.

How earth's crust weight compares

Although enormous in everyday terms, the crust is so thin relative to the planet that it makes up under 1% of Earth's mass, comparable to the skin on an apple.

Frequently asked questions

Why is the crust so light compared to the rest of Earth?
The crust is extremely thin and made of relatively low-density rock. Even though it covers the whole planet, its small thickness keeps its total mass under 1% of Earth.

Is continental or oceanic crust heavier overall?
Continental crust contributes more total mass because it is much thicker, even though oceanic crust is denser per cubic meter. Together they make up the full crustal mass.

How thick is the crust?
Oceanic crust is typically about 5 to 10 kilometers thick, while continental crust can reach 30 to 70 kilometers. This variation is a key factor in estimating its weight.