As any Christian knows, God created the heavens and the earth and all of things that are therein.
Genesis Chapter 1
verse 14
And God said, Let there be lights in the firmament of the heaven to divide the day from the night; and let them be for signs, and for seasons, and for days, and years:
And let them be for lights in the firmament of the heaven to give light upon the earth: and it was so.
And God made two great lights; the greater light to rule the day, and the lesser light to rule the night: he made the stars also.
And God set them in the firmament of the heaven to give light upon the earth,
And to rule over the day and over the night, and to divide the light from the darkness: and God saw that it was good.
This is what AOL has linked to in order to explain how the moon was created. This is what they are teaching our children.
Was Moon Born From Planet's Crash Into Earth?
National Geographic News
August 20, 2001
The moon is not made of green cheese, as myth suggests. But the real story of the moon's creation may hardly be more probable.
Many scientists have thought for years that the moon was formed
during the early days of the solar system when another planet
collided with Earth, ejecting fragments of rocky material that
condensed into Earth's only satellite.
Full Moon
The Full Moon is one of the four main phases of the moon as seen
from Earth.
For more than two decades, scientists have sought to determine
how large the mysterious intruder planet must have been and exactly
how its cataclysmic crash could have helped form the moon. But
none of their models have offered a completely satisfying explanation.
Now, new research offers a scenario that may work. It suggests
the impact may have come from a much more modestly sized foreign
body than previous research has proposed.
Robin Canup, a researcher at Southwest Research Institute in Boulder,
Colorado, and her colleague have fashioned an improved model using
a sophisticated computer-modeling technique. It explains the size,
composition, and orbital properties of both Earth and the moon.
"We determined that a Mars-sized impactor would work the
best," said Canup. She and co-author Erik Asphaug, a scientist
at the University of California at Santa Cruz, proposed their
scenario in a study that appeared last week in the scientific
journal Nature.
Colossal Impact
"Giant impact" theories explaining the moon's formation
were first proposed in the mid-1970s. A decade later, researchers
ruled out a Mars-sized object as the source of the impact and
began to model larger and larger impacts. The two best models
that emerged, however, both had inherent problems.
In one model, the mass of the Earth was right, as was the composition
of the moon. But the Earth's rotation rate after the collision
was unrealistically fast. An improbable second impact would have
been required to slow the Earth's spin.
A second scenario suggested that the impact occurred when Earth
was only half formed. That idea better explained the Earth's modern
rate of rotation and the moon's orbit, but it required Earth to
continue accumulating matter after the impact. That material would
have been rich in iron, which composes 30 percent of Earth's mass.
But the moon, which contains almost no iron, would have simultaneously
absorbed similarly iron-rich rock. The model offers no way to
explain the moon's confounding dearth of iron.
Canup and Asphaug have proposed that the impact came from an object
that was smaller than in the previous models, but was nonetheless
substantial. At one-tenth the mass of the Earth, it was about
the size of Mars, the two researchers say.
The collision occurred 4.5 billion years ago, only 50 million
years after the solar system formed. The colossal impact must
have nearly rent the young Earth apart.
"It didn't break the Earth up, but it came pretty close,"
Canup said.
"The Earth was distorted into an oblong shape before it gravitationally
rebounded" over the course of several hours or a day, she
said. Some of the material flung into space settled into orbit
and eventually clumped together to form the moon.
Better Modeling
Canup and Asphaug were able to re-test the discredited mid-1980s
hypothesis of impact by a Mars-size object thanks to greater computing
power. They used a technique called smooth particle hydrodynamics
to simulate interactions among the many rocky fragments that would
have been created by the impact.
Using several powerful computers, the two scientists produced
simulations involving 20,000 virtual fragments of the Earth and
of the smaller foreign planet that collided with the Earth. Earlier
simulations of similar impacts had been done with only 3,000 particles,
which limited the realism of the simulations.
The researchers ran many simulations, adjusting the key variables-the
size of the object that caused the impact, the angle of its course,
and the mass of the Earth-to see which combination produced the
best result.
The scenario involving a Mars-size object won out. That was when
the researchers realized "the resolution makes a big difference,"
said Canup, referring to the number of particles that were used
in the simulations. Three thousand particles, it turns out, is
not enough realistically to simulate a collision between planet-sized
objects.
In a companion article in Nature addressing Canup and Asphaug's
study, planetary scientist Jay Melosh of the University of Arizona
in Tucson noted, "Encouraging as these new results are, they
are not the final word."
One major question is the accuracy of the mathematical equation
underlying the new impact model. That equation, developed in 1962,
doesn't distinguish well the behavior of ejected solids, liquids,
and gases in the hours following the impact.
Treating these states of matter differently in the simulation
could explain another peculiar aspect of the moon's composition:
its dearth of easily vaporized "volatile" compounds
such as water.
A newer, more sophisticated modeling equation has been developed, but Canup and Asphaug did not use it because it was known to have some imperfections. Since their study, Melosh has reworked that equation. Now he is teaming with Canup and Asphaug to test their new model with the more sophisticated equation to see if the results are consistent with their present findings.