Supercontinents or how we are all going to the Arctic

When Earth was born…

Around 4.5 billion years ago, Earth was born from a turbulent accretion disk of celestial gases and clouds of dust with help from gravity, the glue to hold everything together.

An accretion disk

Soon after that, Earth was bathed in some serious celestial showers made of asteroids, meteorites and comets (The Late Heavy Bombardment). Our neighbor rocky planets like Mars and Venus had the same fate too. In one occasion, an astray asteroid called Theia collided with Earth, and here came our Moon.

Heavy bombardment from outer space

At first, the only thing going on Earth was just a vast ocean of magma and maybe several tremendous tides. These tides were much more enormous than today because Earth was much closer to the Moon.

Then there were some tectonics activities as well. As a result, some crusts were formed and some maybe were submerged into the magma ocean. The tectonics was busy but stagnant in terms of creating stable crusts because of the super hot magma ocean then(drip tectonics).

Then it started to moving around…

Little by little, some crusts were finally formed as Earth was cooling. Oceans were shaped too. Then continental drift kicked in as plate tectonics.

Basically, there are 3 types of relative movement between plates:

  • Divergence: plates move away from each other. As a result, the crust at the plate boundary is stretched out and become thinner. Then the crust pressure against the underlying upper mantle(Asthenosphere) slowly declines. Hence the solid but plastic mantle rock below becomes molten partially to create a magma chamber due to decompression melting. In the end, the crust pressure is unable to balance against the pressure of the rising magma. Consequently, magma rises up to or near the surface and can lead to volcanic activities.
A divergent bounday
  • Convergence: plates collide into each other. 2 things can happen. If both plates are continental crusts, they will mostly crush into each other and stack up into mountains. If one of the plates is an oceanic crust, the denser and heavier one (mostly the oceanic crust) will sink down into the other one and create a subduction zone. As a result, some water from the oceanic crust is mixed and burned up with the underlying mantle rock due to flux-induced melting. A magma chamber is formed, which gives rise to volcanic activities.
A convergent bounday
  • Transformation: plates can slide past each other. When this happens, rocks at the boundary is pulverized into pieces and create a linear ridge(fault zone). Earthquakes are common during this period.
A transform boundary

Tectonics is thought to be caused by multiple forces. The biggest one probably is from the mantle due to the unceasingly moving up and down of the super hot mantle rock because of heat convection. The second biggest one may be the force created by the slab pull from the subduction zone.

Then came the Supercontinents…

For some times in the past, all those plates gather into a giant continent — a super-continent.

Sometimes, that super-continent clumped around the Equator. Other times, it began to break into smaller chunks and then drifted away again in order to gather again some time in the future. This activity of drifting away and clumping into each other has been making many changes to the topology of Earth.

Super-continent Columbia

There was many super-continents in the past. One was formed around 2.1 billion years ago called Columbia. Then it broke up and formed again the super-continent Rodinia around 1.2 billion years ago. And then it broke up again to create another Pangaea around 250 million years ago.

Pangaea, our latest super-continent

Some scientists suggest that there is actually a Super-continent cycle that happens every few hundreds of million years. But what will happen in the next few million years is anyone’s guess.

How do we know?

There are many evidence that prove tectonic plates are a real thing.

  • Continental boundaries of South America and Africa can fit together just like a jigsaw puzzle. It may not be a coincidence.
  • There are some similar species of flora and fauna that lived at the same time in very different locations, which means their locations must have been next to each other sometime in the past.
  • The mid-ocean ridges are the result of the sea floor spreading, which means some plates are moving away from each other.

So where are we going?

Scientists really do not know exactly how the face of Earth ages.

The tectonic plates can either keep drifting away as they’re doing now. And then we would have ended up clumping into one giant mass the other way around(extroversion). Hence there would be only the mighty Atlantic surrounding us. The Pacific Ocean may have been gone completely then.

Or all the plates can turn around sometime in the future and start to rush into each other(introversion). The Atlantic Ocean would be closed and the Pacific Ocean would embrace all of us then.

Some strange ideas are also put forward that we may all go north and get together to set bonfires through harsh winters of the Arctic(orthoversion).

Amasia, a future super-continent according to orthoversion




software engineer with passion about science

Love podcasts or audiobooks? Learn on the go with our new app.

The IoT and Bees: a Technology That Could Save Our Future

Science and the New Age

Planck and The Fine-Tuned Universe that Wasn’t

Nuclear Fusion, Episodes I and II

How Minecraft Explains why Elephants aren’t Teaching us Quantum Mechanics

Adding Film To The Science Syllabus (Part 1)

Nuclear Fusion — Does China Have Another Approach?

Carbon dioxide-eating microbes: synthetic biology can initiate sustainable industrial revolution…

Get the Medium app

A button that says 'Download on the App Store', and if clicked it will lead you to the iOS App store
A button that says 'Get it on, Google Play', and if clicked it will lead you to the Google Play store
Đạt Đạt

Đạt Đạt

software engineer with passion about science

More from Medium

Beyond Lithium: A Systematic Search for Candidate Materials for Calcium-Ion Batteries

A Systematic Search for Candidate Materials for Calcium-Ion Batteries

This octopus-cell is inside your body

NASA space station officials weigh in on remaining in orbit until 2030

This Week In Rocket History: SRE-1 by ISRO