The Lunar Disc Flashcards
(10 cards)
Shape of the Moon
Oblate Spheroid
Appearances of Lunar formations (Craters, Maria, Terrae, Mountains, Valleys)
Craters are lighter dots on the surface, best viewed with shadows
Maria (seas) are large dark grey areas best viewed at full moon
Terrae(highlands) are lighter
Mountains are lighter still best viewed with shadow
Valleys are long, narrow depressions
Identify features in the lunar disc
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Describe the orbital periodof the moon
It is synchronous, its rotation and revolution periods are the same, this is caused by Earths gravity and also occurs on moons of other planets
We can see in total about 59% of the moon due to lunar liberation, how?
The moon wobbling slightly in its orbit, so we can see over or under it.
The moons varying speed allows us to ‘peek’ round the corners of the moon
Formation of terrae
Oldest part of the moon, formed from an early solidified crust, heavily cratered and ref.ective
Formation of Maria
Dark flat plains formed after large impacts which caused lava to flood the basins, and so,doofus into dark rock. Younger than the highlands and less cratered
Formation of Mountains
Formed as raised edges of large impact basins.
Formation of valleys
Can be caused by collapsed lava tubes or crust faulting, as well as in between mountain ranges
Differences between the near and far sides of the moon
Near side has many Maria, is less cratered as it is younger. Thinner crust
Far side is mostly terrae, more cratered as it is older Thicker Crust and not visible. First to see was Russian Luna 3