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If the giant impact hypothesis is correct, they must be due to some other cause.
Today, the giant impact hypothesis is widely accepted by the scientific community.
There remain several questions concerning the best current models of the giant impact hypothesis.
The leading theory has been the giant impact hypothesis.
A similar process, known as the giant impact hypothesis, has been proposed to explain the formation of the Moon.
The giant impact hypothesis thus explains the Moon's abnormal composition.
However, most of these have a lot of problems which is one reason why giant impact hypothesis has been favored.
The ratios of the Moon's volatile elements are not explained by the giant impact hypothesis.
The work, he added, supports the Giant Impact hypothesis.
The evidence for this giant impact hypothesis is:
The Giant impact hypothesis does not explain well the similar composition of Earth and the Moon.
The giant impact hypothesis is the currently favoured scientific hypothesis for the formation of the Moon.
For example, the giant impact hypothesis implies that a surface magma ocean would have formed following the impact.
Her work is based upon the giant impact hypothesis and has involved intensive modeling testing, simulating how planetary collisions actually unfold.
Rock samples gathered by the astronauts gave us a better understanding of the Moon and provided evidence used to support the so-called "giant impact hypothesis" described above.
SwRI giant impact hypothesis simulation (.
Yet another hypothesis proposes that the Moon and the Earth were created together instead of separately like the Giant Impact hypothesis suggests.
This has led to the giant impact hypothesis: the idea that the Moon was formed during a giant impact of the proto-Earth with another protoplanet.
The giant impact hypothesis is that the Moon was created out of the debris from a collision between the young Earth and a Mars-sized proto planet.
Analysis of composition of the lunar samples supports the giant impact hypothesis, that the Moon was created through impact of a large astronomical body with the Earth.
Despite its accuracy in explaining many lines of evidence, there are still some difficulties that are not fully explained by the giant impact hypothesis, most of them involving the Moon's composition.
The giant impact hypothesis proposes that Earth's Moon formed from a colossal impact of a hypothetical protoplanet, named Theia, with Earth, early in the Solar System's history.
GIH (Giant Impact Hypothesis) suggests a Mars-sized body called Theia impacted Earth, creating a large debris ring around the Earth which then formed the system.
This "giant impact hypothesis", which became popular in 1984, satisfies the orbital conditions of the Earth and Moon and can account for the relatively small metallic core of the Moon.
The Earth's Moon and possibly Charon are exceptions among large bodies in that they are believed to have originated by the collision of two large proto-planetary objects (see the giant impact hypothesis).