The troposphere (lower atmosphere) is the densest layer of the atmosphere.

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Above the level of the photosphere is the stellar atmosphere.

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The ionosphere is the inner edge of the magnetosphere and is the part of the atmosphere that is ionized by solar radiation.

And they'll say, OK, it's going to be within this sphere and it actually gets denser as you get into the center of the sphere.

The outer layer, the solid layer is the lithosphere, the more fluid layer right below that is the asthenosphere.

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So it would be this shell.

It's just a red shell.

And we found it in the concrete.

You get the first shell, is 1s2.

It's the fifth shell.

But Mars' atmosphere is about 100 times thinner than Earth's so heat from the sun can easily escape.

Correct coordinates of objects for the effects of the atmosphere

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We also use a lot of the atmosphere for agriculture.

The atmosphere's much more complicated.

Atmospheric physics is the application of physics to the study of the atmosphere.

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We call it atmosphere. This is the icon of our journey.

This that essetnially the lithisphere is kind of riding on top of we call this the asthenosphere. So when we talk about the lithosphere and asthenosphere we're really talking about machanical layers.

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And they changed the atmosphere.

This is your outermost shell right here.

And this is the outermost shell.