A Guide to Earth’s Lithosphere
Earth scientists often compare the lithosphere to a thin, solid and brittle eggshell encasing our inner planet.
Others characterize the lithosphere as a thick piece of wood that dries and breaks.
No matter how you want to describe it, the lithosphere is the solid layer we live and play on.
Today, we’re going to explore the lithosphere. Specifically, we’ll examine the crust and the uppermost part of the mantle.
Why do we have a lithosphere? And why is it important? Let’s dive right in.
Why does Earth have a lithosphere?
About 4.5 billion years ago, the Earth was a hellacious scene. Molten lava flowed everywhere. And Earth was constantly being pelted by meteorites during the bombardment period.
But eventually Earth started to cool down. Soon after a dramatic period of Earth heating, Earth’s lithosphere began to form.
Continents began to rise up out of the mantle. The lighter and buoyant rock floated up to form the top lithosphere layer. Then, the heavier material formed the core-mantle boundary region.
The lithosphere is located between the asthenosphere below and the atmosphere above. It consists of the solid crust and uppermost mantle. Then, we break the crust further down into continental and oceanic crust.
What’s the difference between oceanic vs continental crust
The oceanic and continental crust makes up Earth’s upper lithosphere. Oceanic crust is very young in comparison to continental crust. The oldest oceanic crust is 200 million years old . But the oldest continental crust is as old as 4 billion years.
Oceanic crust forms at divergent plate boundaries. For example, oceanic crust forms at the mid-Atlantic Ridge under the Atlantic Ocean.
At these underwater constructive plate boundaries, lava spews out to form new igneous rocks. Because divergent plates move apart, the age of rocks get older away from tectonic plate boundary.
As the name implies, continental crust are the continents we live on. But it also includes the shallow seabed close to shores called continental shelves.
How does the rock cycle change the lithosphere?
Lithosphere rocks sink deep down into Earth at convergent plates. Then, they rise back up as magma. If these existing rocks erode away, they can cement again into sedimentary rocks.
The ocean bottom is mostly igneous rocks. But 75% of the continents are sedimentary rocks. If you look at all the rocks on Earth, 80% are igneous, 15% are metamorphic and 5% are sedimentary rocks.
What role does the lithosphere play in plate tectonics?
Earth has 7 major tectonic plate boundaries and several micro plates. They’re unusually shaped containing both oceanic and continental crust.
The lithosphere is always on the move. Albeit, it’s a slow movement because fastest plate races at 15 centimeters (6 inches) per year. But the slowest plate crawls at only 2.5 cm per year.
Tectonic plates diverge, transform or converge with each other. It’s common to see divergent plates in the ocean bottom as large mountain chains.
On the other hand, convergent boundaries are often at the edges of continents like the Pacific Ring of Fire. These types of tectonic plates have caused some of the largest disasters in history like earthquakes, volcanoes and tsunamis.
What is the density and depth of the lithosphere?
The depth of the lithosphere is tiny in comparison to inside Earth. While continental crust is 30-35 km thick, oceanic crust is even thinner averaging about 5 km in thickness.
In terms of density, the crust is the least dense of all the layers of Earth. Throughout the planet, the average density is about 5.513 g/cm3. But the density of Earth’s crust is about 2.5 g/cm3 because it’s mostly rocks rich in silica.
Overall, Earth’s density steadily increases inwards to the core. If you compare the crust’s density to deep inside the planet, Earth’s inner core has the highest density at 12.9 g/cm3.