I’m going to try and put the food I eat into context for you, because this is the first time I’ve actually written about a topic this big.
This is, as far as I can tell, the first article I’ve written about the topic.
This first article is actually kind of a spoiler warning because the first thing you’ll see is the very first thing we get to see is this: A map of Earth’s geology.
And it’s really pretty awesome.
It shows a world that’s pretty much the same as the one we see in the movie Interstellar.
But what’s really exciting about this map is that it’s the first map we get of Earth, the only map we’ve got that’s ever been created of Earth.
We’ve only been able to get maps of the planet in our imaginations before.
So the map is amazing and it’s very cool and it does a really great job of capturing the geography of Earth in a way that’s very clear.
But the thing about this is that we can only get that information from the planet.
If you’re a geologist, this is your one opportunity to map Earth.
And so the map shows us that Earth’s geography is really quite simple.
There’s a lot of really shallow, very flat land.
So that’s what we’ve been looking at for the last 200 million years or so.
So this is Earth’s first map.
The next thing we see is a map of the ocean.
And this is actually a map that we got from our own satellites.
So you see, there’s a big hump in the middle of the map that looks like a circle, and it looks like that’s where the ocean meets the land.
And what we’re seeing is the ocean is really big and it has a really steep bottom.
And because of this steep bottom, the water is really, really salty.
So when you think about the water, you think of the salt water in the Gulf of Mexico.
It’s really salty water, but it’s also really cool because it’s a really good comparison.
So, you know, what’s cool about this water is that there’s an area on the surface of the water that’s almost the size of the world.
It looks like the Atlantic Ocean, but because it doesn’t actually look like the Gulf, we can say, Oh my God, we have a little bit of a surprise.
And that surprise is that, as you look at the ocean bottom, there is this large flat spot in the ocean that’s actually about the size and shape of Earth itself.
And the reason that we know that this is really huge is because it has this flat spot.
This flat spot is where the sea meets the ocean, and that’s because there is no water in between.
So it’s actually like an ocean flat spot where water is flat, and the water has a little hole in it.
And we know this because of the magnetic field in the water.
This map shows that the magnetic fields in the sea have changed in the last 2 billion years, and they’ve shifted to an area that is closer to the equator, where the magnetic north pole is.
And there’s one of those spots that looks a little like a triangle with an upside down triangle on one side.
And you can actually see a tiny bit of that spot on this map.
So these magnetic north poles are really close to the surface, so the ocean’s really cool.
But we also know that there are these magnetic south poles that are farther away.
So we can see that these magnetic poles are much closer to where they’re on the Earth.
So in the map, we see that there is a lot more water there.
We see that the ocean isn’t flat, it’s sort of curved like a sphere.
So water’s flowing out, and there’s this big, very thick layer of water underneath.
And now the map lets us see where that water is flowing.
We can see water in these places.
There are places where there’s not water, and we can even see a little chunk of water that looks almost like a hole, and this is where we have an area called the continental shelf.
And here’s where we think that water came from, and where it was there.
The map tells us that water that was deposited by this giant plate of water came up through the ocean and got stuck in this area of the continental ridge, and now it’s there.
Now, this doesn’t mean that this continental shelf is solid, but we know from satellites that we have water there, so that tells us something.
So where is this water coming from?
It’s coming from somewhere.
And where it is coming from is where it’s going to get a lot hotter than it is today.
So as we move through the next 300 million years, the Earth’s crust is going to become hotter and more unstable, and then as the crust gets hotter and hotter, it’ll break apart