This Map Predicts What the World Will Look Like in 250 Million Years
Imagine standing in a future where the continents we know today no longer exist in their current forms, where new landmasses have fused together, and where the world looks drastically different from anything we can comprehend. This isn't science fiction—it's the future of our planet, as predicted by the slow yet powerful forces of plate tectonics. While this might sound like a topic for geologists, it’s fascinating to think about how our world could change over the next 250 million years.
The Basics of Supercontinents and Plate Tectonics
Before we dive into what the Earth might look like in the distant future, let’s break down the basic science behind it. The Earth’s outer shell, known as the lithosphere, is broken into large, rigid pieces called tectonic plates. These plates are constantly shifting, though at a pace so slow that it’s barely noticeable in our lifetimes. Over millions of years, they collide, drift apart, and rearrange themselves to form new supercontinents.
These supercontinents—large landmasses that unite most or all of Earth’s continents—have been a recurring theme throughout the planet’s history. For instance, Columbia, one of the earliest known supercontinents, existed more than 1.5 billion years ago before breaking apart. Later, another supercontinent, Rodinia, took its place, only to disband around 750 million years ago. But perhaps the most famous of them all is Pangaea, the supercontinent that existed around 300 million years ago and began to break apart around 175 million years ago. The remnants of Pangaea are what make up the continents we know today.
The movement of these plates is not a constant, uniform process. Some plates move very slowly, at a rate of about 20 millimeters per year—the same pace at which fingernails grow, according to Dietmar Muller, a leading expert on tectonics. Despite their slow pace, these movements reshape the planet over vast spans of time.
The Next Supercontinent: What Will It Look Like in 250 Million Years?
Now that we understand how supercontinents form, the next question is: What will the next one look like? While predicting the exact future arrangement of continents is an incredibly complex task, several scientific models have offered projections based on current tectonic movement and data. These models are educated guesses, and although they offer compelling possibilities, they are far from certain.
That said, researchers have proposed several names for the next supercontinent, which is expected to emerge around 250 million years from now. Here are four of the most prominent contenders, each based on different theories about how Earth’s plates will shift over the coming millennia:
- Novopangaea: This theory suggests that all of Earth’s continents will eventually converge around the Pacific Ocean, leading to a supercontinent that closely resembles the ancient Pangaea. The Pacific Ocean will shrink, and the landmasses will come together to form a unified supercontinent.
- Aurica: This model places the Indian subcontinent at the heart of a massive landmass, with other continents surrounding it. The landmasses would gradually move toward India, creating a new configuration of continents.
- Amasia: As the name suggests, Amasia proposes the fusion of Asia and North America, likely via the North Pole. The two landmasses would merge, possibly leading to the formation of a new northern hemisphere supercontinent.
- Pangaea Proxima: Also known as Next Pangaea, this model is often considered the most reliable of the predictions. It envisions a supercontinent that forms through the collision of Africa, Eurasia, and the Americas, with Australia and Antarctica also joining in. This scenario would result in most of the continents fusing together, leaving only isolated areas like New Zealand and Scotland as exceptions.
The Possible Future of Our World
One of the most compelling projections comes from C.R. Scotese, a researcher who has used data from the University of Sydney to model past and future tectonic movements. According to this model, Pangaea Proxima would see most of the Earth’s landmasses fused into a single supercontinent, with the Americas positioned next to Africa. In this new configuration, Europe would sit at the northern edge of the landmass, and countries like France would be far from their current locations, with a shared border with what would be Britain.
While it may sound like a far-off vision, the shifting of tectonic plates is a process that is already happening, just incredibly slowly. As a result, it may take millions of years for the Earth to reach this point. And when it does, the world as we know it will look completely different—perhaps unrecognizable.
The Significance of Plate Tectonics in Earth’s Future
While it’s easy to feel detached from such an immense timeframe, it’s essential to understand that the movement of tectonic plates is not just a geological curiosity; it has profound implications for life on Earth. The constant reshaping of continents affects everything from climate patterns to ocean circulation, and even the evolution of species. For example, the breaking apart of Pangaea contributed to the diversification of life forms as landmasses drifted apart, leading to the species-rich continents we have today.
So, even though we won’t be around to see it, the movement of tectonic plates will continue to shape the Earth for billions of years to come. And who knows? Perhaps in the distant future, life on Earth will adapt in unimaginable ways to the changing geography.
For now, the thought of a world that looks entirely different 250 million years from today serves as a reminder of just how dynamic and ever-changing our planet is. As we move through the rapid advancements of the present, it’s humbling to think about the slow yet unstoppable forces beneath our feet that are constantly reshaping the world on a scale we can barely fathom.