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The Moon approx. 9 days after new.
Taken at the Port Macquarie Observatory with the 355 mm reflecting telescope at the prime focus.
The photograph shows the two most conspicuous
craters on the Moon, Tycho & Copernicus.
Tycho, named for Tycho Brahe, the Danish astronomer.and
copernicus for Nicholas Copernicus.
Tycho, top right hand corner, is very bright
and has a tremendous system of rays that extend out from its edge
for hundreds of kilometres in all directions. The crater is approx
90 kilometres in diameter.
Copernicus is approx in the centre of the
photograph, just off the terminator line (day and night).
Copernicus is also about the same diameter as Tycho.
Copernicus also has a ray system, but not as extensive as that of Tycho.
It is very prominent at full moon.
Both craters have mountain peaks.
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PORT
MACQUARIE ASTRONOMICAL ASSOCIATION INC THE
MOON
The
Moons craters tell an interesting story about the history of
our solar system.
Long ago, meteoroids by the millions, hit the Moon with tremendous
force, gouging out most of the craters we see there.
Most of the meteoroids were used up very quickly, and so the
bombardment slowed down dramatically.
When portions of the Moons surface melted, the old craters were
erased. So
we can now tell almost at a glance whether a part of the Moons surface is
young or old.
A young surface has few craters, because there are relatively few
meteoroids left to make fresh craters, but an ancient surface will be
nearly covered with craters.
When astronauts visited the Moon, they brought rock samples back to
the Earth for analysis.
From this it was found that even the youngest rocks on the Moon are
actually extremely old.
This tells us that no new rocks have been produced on the Moon for
a very long time.
On the Earth, however, many geologic processes are still going on,
producing new rocks and fresh surfaces. Although
the Moon was a geological active body once, it is now a nearly dead object
in space. Port Macquarie Astronomical Assoc. Inc. |
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