Moon, our fellow wanderer of the night sky, has some strikingly interesting facts and SpaceBoy brings you those “luna”tic info right on your desktop!
>> Indian astronomers of the vedic period as early as 1500 B.C determined the orbit of the Moon precisely based on the phases of the Moon and developed the lunar calendar.

>> Hipparchus, an ancient Greek Astronomer, using only his observations and mathematical formulae measured the distance to the Moon as well as the Sun with surprising accuracies.
>> The mean density of Moon is just 3.35 g/cc whereas that of our Earth is 5.52 g/cc.
>> Moon does not have a substantial molten core like earth and hence no magnetic field.
>> Moon exhibits extremes of temperature. During the daytime mercury soars up to +110 degrees Celcius where as the nights are notoriously cold reaching -180 degrees Celcius.
>> The terrain is basically classified into
- Highlands : rugged ; very ancient.
- Maria : smooth ; younger lowlands.
>> The mountains or highlands in Earth are formed by the crustal deformation or the so called “Plate Tectonics” which is absent in our neighboring wanderer.

>> Maria ( Latin for “Seas” ) are relatively flat areas produced by massive lava flow during earlier Lunar Volcanism, comprising about 16 % of the lunar surface. [Click here to view enlarged image]
>> Maria is associated with gravity anomalies also called as “ Masons ” ( Mass Concentrations )
>> A spacecraft would accelerate as it nears the Maria region and decelerate as it moves away due to Masons.

>> Lunar surface is covered with a gently rolling layer of powdery soil and rock fragments called ‘Regolith’
>> Regolith – is a powdery formation as a result of the debris created by the meteor impacts which cause craters. [Click here to view enlarged image]
>> The juiciest information is: there’s a relative abundance of Helium - 3 isotope (a fusion element) on the moon, compared to earth.
>> This may be due to the fact that over a 4 billion year history of moon tons of He-3 from the solar wind have impacted directly onto the surface of the moon and got trapped in minerals like Ilemenite [ a compound of Iron and titanium oxide : FeTiO3 ]. Though He-3 has high diffusivity and escapes from the lunar soil, Ilemenite has a very high retentivity for the same. [Click here to view enlarged image]
>> The lunar surface where Neil Armstrong set his foot is called – “ The Sea of Tranquility ”
>> Selenography – is the study of the physical features of the Moon.
Hope you enjoyed this nutty compilation of fragments of information about our lovely friend of the night sky !
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