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  2. Internal structure of the Moon - Wikipedia

    en.wikipedia.org/wiki/Internal_structure_of_the_Moon

    In 2019, a reanalysis of nearly 50 years of data collected from the Lunar Laser Ranging experiment with lunar gravity field data from the GRAIL mission, shows that for a relaxed lunar fluid core with non-hydrostatic lithospheres, the core flattening is determined as (2.2 ± 0.6) × 10 −4 with the radii of its core-mantle boundary as 381 ± 12 km.

  3. Atmosphere of the Moon - Wikipedia

    en.wikipedia.org/wiki/Atmosphere_of_the_Moon

    be re-implanted into the regolith as a result of the Moon's gravity; escape the Moon entirely if the particle is moving at or above the lunar escape velocity of 2.38 km/s (1.48 mi/s), or 5,328 mph (8,575 km/h); be lost to space either by solar radiation pressure or, if the gases are ionized, by being swept away in the solar wind's magnetic field.

  4. Moon - Wikipedia

    en.wikipedia.org/wiki/Moon

    The Moon has a solid iron-rich inner core with a radius possibly as small as 240 kilometres (150 mi) and a fluid outer core primarily made of liquid iron with a radius of roughly 300 kilometres (190 mi). Around the core is a partially molten boundary layer with a radius of about 500 kilometres (310 mi).

  5. Planetary core - Wikipedia

    en.wikipedia.org/wiki/Planetary_core

    The internal structure of the Moon was characterized in 1974 using seismic data collected by the Apollo missions of moonquakes. [11] The Moon's core has a radius of 300 km. [12] The Moon's iron core has a liquid outer layer that makes up 60% of the volume of the core, with a solid inner core. [13]

  6. Buzz Aldrin reveals the true story behind the most iconic ...

    www.aol.com/article/2016/04/06/buzz-aldrin...

    Source: NASA Armstrong took the photo with a 70mm lunar surface camera while the two explored a region of the moon known as the "Sea of Tranquility.". At an event promoting his new book, No Dream ...

  7. Lunar regolith - Wikipedia

    en.wikipedia.org/wiki/Lunar_regolith

    Surveyor 7 observes levitating dust. There is some evidence that the Moon has a tenuous layer of moving dust particles constantly leaping up from and falling back to the Moon's surface, giving rise to a "dust atmosphere" that looks static but is composed of dust particles in constant motion.

  8. Geology of the Moon - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Moon

    The geology of the Moon (sometimes called selenology, although the latter term can refer more generally to "lunar science") is quite different from that of Earth. The Moon lacks a true atmosphere , and the absence of free oxygen and water eliminates erosion due to weather .

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