The Earth’s Interior
A look At The Inner Earth
the earth's interior can help us to understand earthquakes, volcanoes,
plate tectonics and more about the inner earths natural processes.
In general the earth's interior has been sorted by Gravity.
Heavier elements like iron tend to sink toward the center or core of
the earth. Lighter materials, the silicates, oxygen compounds and water
have risen to become part of the crust. This action has created distinct
layers within the earth and is still in process today.
The Inner Earth is composed of three main parts; the crust, the
mantle, and the core as shown in the diagram of the earth's interior
- The Crust - silicate rocks, primarily granite and basaltOceanic Crust - mostly basaltContinental Crust - igneous, metamorphic, and sedimentary rocks
- The Mantle - iron and magnesium rich silicate rocksUpper MantleLower mantle
- The Core - iron nickel alloyOuter core Inner core
crust of the earth is very slowly growing thicker. Volcanic activity is
continually adding mass to the crust. Though the crust is solid it is
made up of about 12 plates. They are called Tectonic Plates.
These plates are in constant motion. The movement is caused by
convection currents in the mantle. The movement is very slow, averaging
about 2 inches a year. This is about like the growth of your
Earth's Interior - The Mantle
- The crust is about 0.5 % of the earth’s total mass.
- The crust is made up of silicate rocks such as granite and basalt.
- The continental crust is much thicker than the oceanic crust as shown here in the diagram of the earth's crust.
- Oceanic crust
- The crust under the oceans is about 10 km thick and is generally made
up of rock rich in iron and magnesium. These are primarily basalt
formed by volcanic action at the mid ocean ridges. The oceanic crust is
denser than continental crust.
- Continental crust (continental cratons)
- Where there are continents the crust is about 30 to 50 km thick. It
is made up of igneous, metamorphic, and sedimentary rocks. The
continental crust is less dense than the oceanic crust. When the
continental crust collides with oceanic crust through plate movement the
continental crust rides over the top of the oceanic crust while the
oceanic crust is pushed back down towards the mantle.
less is known about the mantle than the crust. The crust we can see,
measure, dig and drill. The mantle is different. We have little direct
contact with the inner earth. We can tell some things about the mantle
by studying volcanoes and what comes out of them.
Much of what we believe is true about the earth's interior comes from studying Seismology.
Seismology began as the study of earthquakes and the seismic waves they
produced. These waves travel through the earth and move at different
speeds in different materials. By studying these waves and how they move
through the inner earth we can learn about the its structure.
The upper mantle
The Lower mantle
- Is made up of rocks rich in magnesium and iron, and poor in silica; mostly peridotites.
- It is about 400 km thick and is much denser than the crust.
- It comprise 10% of the earth’s mass
Earth's Interior - The core
- It is more dense and contains a greater amount of iron than the upper mantle
- It is about 1900 km thick
- It makes up 41% of the earth’s mass
The core is composed primarily of a nickel-iron alloy. There is an outer core that is liquid and an inner core that is solid.
Some points to remember in studying the earth’s interior:
- Outer core Is about 2100 km thick. It makes up about 30 % of the Earth's total mass.
- Inner coreIs about 1300 km thick. It makes up about 2 % of the Earth's total mass.
- There are distinct layers to the earth’s interior.
- Heavier elements tend to sink to the core
- Lighter elements rise toward the surface
- Much more is known about the crust than the mantle and core.
- What we believe is true about the mantle and core comes from studying seismology.
Below you may download a blank copy of the inner earth for students to color and lable.Download a blank copy of The Earth's Interior PDF file here