In the early 20th century, a meteorologist named Alfred Wegener observed striking similarities between the coasts of Africa and South America. These observations led him to propose a controversial new theory: perhaps these and many other continents had once been connected in a single, gigantic landmass. Wegener’s Theory of Continental Drift directly contradicted the popular opinion that Earth’s continents had remained steady for millennia, and it took almost 50 years for his advocates to convince the larger scientific community.
Today, we know something even more exciting—Pangea was only the latest in a long lineage of supercontinents, and it won’t be the last. Continental Drift laid the foundation for our modern theory of plate tectonics, which states that Earth’s crust is made of vast, jagged plates that shift over a layer of partially molten rock called the mantle. These plates only move at rates of around 2.5 to 10 centimeters per year, but those incremental movements shape the planet’s surface.
To determine when a new supercontinent will emerge, we need to predict where these plates are headed. One approach here is to look at how they’ve moved in the past. Geologists can trace the position of continents over time by measuring changes in Earth’s magnetic field. When molten rock cools, its magnetic minerals are “frozen” at a specific point in time. So by calculating the direction and intensity of a given rock’s magnetic field, we can discover the latitude at which it was located at the time of cooling.
However, this approach has serious limitations. For one thing, a rock’s magnetic field doesn’t tell us the plate’s longitude, and the latitude measurement could be either north or south. Worse still, this magnetic data gets erased when the rock is reheated, like during continental collisions or volcanic activity. So geologists need to employ other methods to reconstruct the continents’ positions. Dating local fossils and comparing them to the global fossil record can help identify previously connected regions. The same is true of cracks and other deformations in the Earth’s crust, which can sometimes be traced across plates.
Using these tools, scientists have pieced together a relatively reliable history of plate movements, and their research revealed a pattern spanning hundreds of millions of years. What’s now known as the Wilson Cycle predicts how continents diverge and reassemble. And it currently predicts the next supercontinent will form 50 to 250 million years from now. We don’t have much certainty on what that landmass will look like. It could be a new Pangea that emerges from the closing of the Atlantic. Or it might result from the formation of a new Pan-Asian ocean.
While its shape and size remain a mystery, we do know these changes will impact much more than our national borders. In the past, colliding plates have caused major environmental upheavals. When the Rodinia supercontinent broke up circa 750 million years ago, it left large landmasses vulnerable to weathering. This newly exposed rock absorbed more carbon dioxide from rainfall, eventually removing so much atmospheric CO2 that the planet was plunged into a period called Snowball Earth.
Over time, volcanic activity released enough CO2 to melt this ice, but that process took another 4 to 6 million years. Meanwhile, when the next supercontinent assembles, it’s more likely to heat things up. Shifting plates and continental collisions could create and enlarge cracks in the Earth’s crust, potentially releasing huge amounts of carbon and methane into the atmosphere. This influx of greenhouse gases would rapidly heat the planet, possibly triggering a mass extinction. The sheer scale of these cracks would make them almost impossible to plug, and even if we could, the resulting pressure would just create new ruptures.
Fortunately, we have at least 50 million years to come up with a solution here, and we might already be onto something. In Iceland, recently conducted trials were able to store carbon in basalt, rapidly transforming these gases into stone. So it’s possible a global network of pipes could redirect vented gases into basalt outcrops, mitigating some of our emissions now and protecting our supercontinental future.
Recreate the supercontinent Pangea by cutting out shapes of the current continents from a world map. Try to fit them together based on their coastlines and geological evidence. This activity will help you visualize how the continents may have once been connected.
Use an online plate tectonics simulation tool to observe how tectonic plates move over time. Experiment with different settings to see how the movement of plates can lead to the formation of mountains, earthquakes, and volcanic activity. This will give you a hands-on understanding of the dynamic nature of Earth’s crust.
Conduct a classroom experiment to map the magnetic field of different rocks. Use a compass to measure the direction of the magnetic field in each rock sample. This activity will help you understand how geologists use magnetic data to trace the historical positions of continents.
Examine fossil samples from different continents and try to match them based on similarities. Create a chart that shows which continents were likely connected based on the fossil evidence. This will help you understand how paleontologists use fossils to reconstruct past continental arrangements.
Participate in a debate on the potential environmental impacts of future continental shifts. Research and present arguments on how these changes could affect climate, biodiversity, and human life. This activity will encourage you to think critically about the long-term consequences of geological processes.
Continental drift – The gradual movement of the continents across the earth’s surface due to the movement of tectonic plates. – The theory of continental drift suggests that the continents were once joined together in a single landmass called Pangaea.
Theory – A well-substantiated explanation of some aspect of the natural world that is based on a body of facts and evidence. – The theory of evolution is widely accepted by scientists as the best explanation for the diversity of life on Earth.
Supercontinents – Large landmasses formed by the collision and aggregation of multiple continents. – The most recent supercontinent, known as Pangea, existed around 300 million years ago.
Plate tectonics – The theory that Earth’s outer shell is divided into several plates that glide over the mantle, causing geological events such as earthquakes and the formation of mountains. – Plate tectonics explains how the movement of tectonic plates can create volcanic activity along the Ring of Fire.
Crust – The outermost layer of the Earth, composed mainly of solid rock. – The Earth’s crust is thinnest beneath the oceans and can be several kilometers thick beneath mountain ranges.
Mantle – The layer of the Earth between the crust and the core, consisting of hot, semi-solid rock. – Convection currents in the mantle are responsible for the movement of tectonic plates.
Magnetic field – A region around a magnetic material or a moving electric charge where the force of magnetism acts. – Earth’s magnetic field is generated by the movement of molten iron in its outer core.
Latitude – The angular distance north or south from the equator, measured in degrees. – The coordinates 40°N indicate a location that is 40 degrees north of the equator.
Longitude – The angular distance east or west from the prime meridian, measured in degrees. – The coordinates 75°W indicate a location that is 75 degrees west of the prime meridian.
Fossil record – The collection of all known fossils, which provides evidence of the history of life on Earth. – The fossil record shows that dinosaurs roamed the Earth millions of years ago.
