The History of the Moon
Using samples brought back from the Apollo astronauts, we
can estimate the age of moon rocks through radioactive dating (see your
text for details). So what do we get for the ages of moon rocks?
-
Lunar Highlands: 3.9-4.5
billion years (Gyr) old
-
Lunar Maria: 3.1-3.8
billion years (Gyr) old
Compare this with the oldest Earth
rocks: 3.7 Gyr.
And compare this to the age
of the Sun: ~5 Gyr.
So what have we learned? A sketch
of lunar history:
-
Moon formed 4.5-4.6 Gyr ago
-
Early in the moon's history, its
surface was hot and molten.
-
lack of volatile elements in rock
-
Gabbro rock - slowly cooling magma
-
Meteoric bombardment strong 3.8
- 4.5 Gyr ago
-
Major observed impact basins formed
3.8 - 4.0 Gyr ago
-
Volcanic flooding of basins happened
3.1-3.8 Gyr ago
-
we see evidence of volcanic flows
-
Basaltic rock - rapid cooling
-
Cratering rate much lower since
about 3.8 Gyr ago
What does this tell us about
the solar system?
-
When did the planets coalesce?
-
What were conditions like in the early
solar system?
-
When were the planetesimals largely
"cleaned out" of the solar system?
But what about the formation
of the Moon? How did it get there?