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The Moon Itself

The Moon Itself. Structure and Atmosphere. Basic Lunar Stats. Radius: 1,738 km ( 26 % of Earth’s) Mass: .0123 Earth Masses (7.349 x 10^22 kg) Density: 3.34 g/cm ³ Surface Gravity: 1.6 m/s² (1/6 of Earth’s) Temperature: Low: -173ºC (-280ºF)

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The Moon Itself

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  1. The Moon Itself Structure and Atmosphere

  2. Basic Lunar Stats Radius: 1,738 km ( 26 % of Earth’s) Mass: .0123 Earth Masses (7.349 x 10^22 kg) Density: 3.34 g/cm³ Surface Gravity: 1.6 m/s² (1/6 of Earth’s) Temperature: Low: -173ºC (-280ºF) (Perhaps -240°C ( -400°F) in deep craters) High: 130°C (260°F)

  3. The Lunar Atmosphere For all practical purposes the Moon has no atmosphere. The lack of an atmosphere is why temperatures vary so greatly…no greenhouse effect There is slightly more helium near the Moon’s surface than in space, but not enough to count as an atmosphere. Near the poles there are traces of hydrogen. Source? Frozen Water from comets that has collected in the inside of polar craters that are permanently dark and thus cold.

  4. Water Ice Confirmed on Moon In November 2009 a space probe was delibrately crashed into a crater near the Moon’s South Pole. Another probe flew through the resulting “splash” of debris and confirmed the presence of water ice! This water ice can be used to supply a Lunar colony and make rocket fuel on the Moon making Space exploration easier

  5. The Regolith Collisions of asteroids and meteoroids with the moon have created the Regolith It is a light colored layer of dust and rock It is the “soil” of the Moon.

  6. Regolith: Tens of meters thick. Crust: made of Silicates, rigid 60 km thick on near side. 100 km on far side. Mantle: about 1300km thick. Denser than crust, but rigid Core: Metallic, Iron and Nickel, very small. The core is off center…closer to near side because… Earth’s gravity affects core and crust. Lunar Layers

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