That's around the height of a golf tee. The width of a cracker. It's also the amount that the Atlantic Ocean is expanding every year.
Now when you're talking about an ocean that is 4,830 kilometres (3,000 miles) wide at its largest point, 4 centimetres (1.6 inches) is not much. But it is happening. So naturally, scientists want to know why.
Thanks to a new study, researchers think that they have the answer why. You could even call it a 'hot take'. As in hot magma, or molten rock, deep under the ocean floor!
The study suggests that the expansion is being caused by magma bubbling up from under an underwater 'mountain range' called the Mid-Atlantic Ridge. Let's start with what that ridge is.
Basically, the Mid-Atlantic Ridge is the seam between some very large tectonic plates. The ridge is also known as a plate boundary. As we've discussed before here, tectonic plates are essentially the platforms that our continents rest on. They are large pieces of the crust that are always moving in slow motion.
This movement is what causes earthquakes, for example. And the areas where the plates meet are where we tend to find things like mountains and volcanos, as well.
Push and pull
In this case, as the magma bubbles up from the mantle below the crust, it is pushing the edges of both plates out of the way. As a result, the ocean is slowly getting wider.
This is a new finding. Before the study, scientists thought that the plates were being pulled apart—they were being dragged away from the ridge by forces occurring on either side of the ocean, not from in the middle.
Scientists still believe that this 'pulling' motion is happening. It is just that now, they feel that the bubbling magma is an important force as well. There is push and pull.
A long look at a small area
The scientists behind this study have been quick to point out that their research is only looking at a small cross-section of the ridge. It's like a slice across it. What is happening right along this slice, may not be happening the same way up and down the entire ridge. But it is still really useful information—and how they got it is pretty cool.
Back in 2016, a research ship traveled to a very quiet spot directly over the ridge. Over five weeks, the crew dropped 39 seismometers on to the ocean floor. These devices allow them to 'listen' to the activity of the tectonic plates and what was beneath it. It's like what a stethoscope does with your heartbeat, but for the planet. A year later, they retreived the devices and looked at the data.
Then it was back to the lab to try and piece together what they learned. In the end, they have added to our understanding of how and why the Earth's surface constantly moves. Even if it is only by about a little bit each year!