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(4.6 billion years ago) As Earth cooled, an atmosphere formed mainly from gases spewed from volcanoes. It included hydrogen sulfide, methane, and ten to 200 times as much carbon dioxide as todays atmosphere.
As Earth cooled, an atmosphere formed mainly from gases spewed from volcanoes. It included hydrogen sulfide, methane, and ten to 200 times as much carbon dioxide as todays atmosphere. After about half a billion years, Earths surface cooled and solidified enough for water to collect on it.
The first atmosphere was formed by outgassing of gases trapped in the interior of the early Earth, which still goes on today in volcanoes. For the Early Earth, extreme volcanism occurred during differentiation, when massive heating and fluid-like motion in the mantle occurred.
An atmosphere is made of the layers of gases surrounding a planet or other celestial body. Earths atmosphere is composed of about 78% nitrogen, 21% oxygen, and one percent other gases.
These layers are the troposphere, stratosphere, mesosphere and thermosphere. A further region at about 500 km above the Earths surface is called the exosphere.
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Earths atmosphere is composed of about 78 percent nitrogen, 21 percent oxygen, 0.9 percent argon, and 0.1 percent other gases. Trace amounts of carbon dioxide, methane, water vapor, and neon are some of the other gases that make up the remaining 0.1 percent.
Erupting volcanoes released hot gases from inside Earth. These gases surrounded Earth, forming an atmosphere. Ancient Earths atmosphere was mainly water vapor with a little carbon dioxide (CO2) and nitrogen.
The air around you has weight, and it presses against everything it touches. That pressure is called atmospheric pressure, or air pressure. It is the force exerted on a surface by the air above it as gravity pulls it to Earth.

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